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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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    Bioremediation of chlorinated ethenes in aquifer thermal energy storage
    Ni, Z. - \ 2015
    Wageningen University. Promotor(en): Huub Rijnaarts, co-promotor(en): Tim Grotenhuis; P.F.M. van Gaans. - Wageningen : Wageningen University - ISBN 9789462575752 - 216
    watervoerende lagen - thermische energie - verzwakking - grondwater - waterzuivering - duurzame energie - biogeochemie - aquifers - thermal energy - attenuation - groundwater - water treatment - sustainable energy - biogeochemistry

    Subjects: bioremediation; biodegradation; environmental biotechnology, subsurface and groundwater contamination; biological processes; geochemistry; microbiology

    The combination of enhanced natural attenuation (ENA) of chlorinated volatile organic compounds (CVOCs) and aquifer thermal energy storage (ATES) appears attractive because such integration provides a promising solution for redevelopment of urban areas in terms of improving the local environmental quality as well as achieving sustainable energy supply. It will reduce the current negative interference between groundwater contaminants and ATES systems that arises from the rapid increase of ATES system numbers and generally long duration of contaminated groundwater treatments. However, currently the implementation of the combined system is at an initial stage, and still requires comprehensive study before advancing to mature application. Studies should specifically focus on understanding of the basic biogeochemical processes in aquifer systems under conditions of ATES and enhanced bioremediation and their mutual impacts when combined in ATES-ENA. To this end, the research as reported in this thesis employed laboratory experiments and modeling approaches focused on finding the essential process factors involved in the combined system, revealing possible drawbacks, and providing a better understanding to design alternative options on better operation of the combined system.

    Chapter 2 assessed the limiting factor for reductive dechlorination of PCE in an Fe(III) reducing aquifer, being the typical type of subsurface in the Netherlands. A step-wise batch study was performed which consisted of redox conditioning by lactate and ascorbic acid, followed by reductive dechlorination in different scenarios. For the sediment material sampled from the Fe(III) reducing aquifer, conditioning of the redox potential could stimulate PCE dechlorination. It was concluded that 75 µmol electron equivalents per gram dry mass of aquifer material was the threshold to obtain a redox potential of -450 mV, which is theoretically suitable for PCE reductive dechlorination. However, dechlorinating bacteria required for fully reductive dechlorination are generally lacking in Fe(III) reducing aquifers. Without bioaugmentation of dechlorinating bacteria, PCE could only be reduced to TCE or cis-DCE. The step-wise approach and findings obtained from different scenarios tested in this study are relevant for improving the cost-effectiveness of the design and operation of in situ bioremediation. The redox potential of an aquifer can be used as a general indicator to evaluate the potential for CVOCs reductive dechlorination. For achieving specific goals of in situ bioremediation projects at different CVOCs contaminated sites with various environmental conditions, the balance between cost, benefit, and potential risks (e.g. bio‑chemical well clogging due to bacteria growth and precipitation of metal-oxides) should be estimated before the design and operation of the ATES-ENA systems. This chapter provides insights into the essential factors that determine the feasibility of ATES-ENA.

    In Chapter 3, the two most important impacts of ATES on enhanced bioremediation of CVOCs were investigated using batch experiments. Besides, another type of underground thermal energy storage system, the borehole thermal energy storage (BTES) was also studied as a comparison to ATES. Here cis-DCE was targeted as it is commonly found to accumulate in the subsurface due to incomplete dechlorination. Compared to a natural situation (NS) with sufficient electron donor and bioaugmentation at a constant temperature of 10 ˚C, we assessed the effect of ATES by exchanging liquid between bottles kept at 25 and 5 ˚C, and the effect of BTES by alternating temperature between 25 and 5 ˚C periodically. Under ATES warm condition, cis-DCE was dechlorinated to ethene and at an increasing rate with each liquid exchange, despite no biodegradation being observed under ATES cold condition. The overall removal rate under alternating ATES conditions reached 1.83 μmol cis‑DCE/day, which was over 1.5 and 13 times faster than those in BTES and NS conditions. Most probably growth of biomass occurred under ATES warm condition, leading to an autocatalytic increase in conversion rates due to higher biomass concentration. Comparison between batches with or without Dehalococcoides inoculum revealed that their initial presence is a determining factor for the dechlorination process. Temperature then became the dominant factor when Dehalococcoides concentration was sufficient. The results also indicated that Dehalococcoides was preferentially attached to the soil matrix. This chapter highlights the importance of the dynamic temperature regimes in ATES on the bioremediation of CVOCs and recommends to implement biostimulation actions in the ATES warm well.

    Further impacts of ATES related to change in redox condition on bioremediation of CVOCs, with focus on microbial responses of Dehalococcoides, were explored in Chapter 4. In this chapter, we adopted a recirculating column experiment with a flow rate of 10 mL/min (representing the flow velocity at a distance of 1.3 m from the center of a typical ATES well) to simulate the ATES system. To mimic potential periodic redox fluctuations that accompany ATES, serial additions of lactate and nitrate were performed. Firstly, also at the relatively high liquid velocity (compared to normal bioremediation conditions) complete reductive dechlorination from cis-DCE to ethene was achieved in the column system. However, dechlorination was immediately terminated by subsequent nitrate addition due to direct interruption of Dehalococcoides retention to the soil matrix. In our column system, which was much more homogeneous than subsurface in reality, repeated interruption of dechlorination via Dehalococcoides was extremely severe. Such repeated interruption by nitrate dosing eventually led to less easily reversible while requiring more efforts for recovering dechlorination. In addition, the hypothesis of the immobility of Dehalococcoides was further confirmed by the microbial analysis of microorganism in the liquid phase where only less than 0.1% of the Dehalococcoides inoculum could be found back. Although some field studies demonstrated easier regeneration of Dehalococcoides in the subsurface after suffering oxidant, results from this chapter emphasized the sensitive resilience of Dehalococcoides which needs careful consideration in biostimulated ATES condition, and a functional combined system requires dedicated ATES operation and monitoring on the aquifer geochemical conditions.

    The major concern on possible negative impact of enhanced bioremediation on ATES is biological clogging attributed to biomass growth. As chemical clogging due to Fe(III) precipitates is a common problem in the functioning of ATES, the clogging issues (both biological and chemical) should be addressed before practical application. The potential clogging issues in the combined system were then researched in Chapter 5 using the same recirculating column system as in the previous chapter. For this purpose, two flow rates, 10 and 50 mL/min, were implemented. In the two columns, enhanced biological activity and chemically promoted Fe-oxide precipitation were studied by addition of lactate and nitrate respectively. Pressure drop (∆P) between the influent and effluent of the columns was monitored to indicate clogging of the system. The results showed no increase in ∆P during the period of enhanced biological activity, with large amount of lactate and active inoculum being added, even when the concentration of total bacteria in the liquid phase increased by four orders of magnitude. Nitrate addition, however, caused significant increase of ∆P. Remarkably, in the column with higher flow rate (50 mL/min), an unforeseen blow-up occurred at the end of experiment, as the buildup of pressure in the system was higher than the strength of the glass column. However, in the column with flow rate of 10 mL/min, high pressure buildup caused by nitrate addition could be alleviated by lactate addition. Such finding indicates that the risk of biological clogging related to biostimulation is relatively small, because by maintaining a low redox condition biostimulation itself may counter chemical clogging in ATES. Nevertheless, acknowledging that a column system cannot fully mimic real ATES conditions, additional tests are necessary to further investigate the clogging issues in the combined system.

    In Chapter 6, we performed a simulation of ATES-ENA with a reactive transport model, using ATES as the engineering tool for lactate injection in a hypothetical TCE contaminated aquifer which is assumed to be homogeneous. Many relevant processes in the combined system were simulated, such as TCE, cis-DCE and VC dechlorination, sulphate and Fe(III) reduction, organic acid fermentation and oxidation and growth of different biomass. In total 15 scenarios are considered in the model, including variations in lactate dosage (three concentration levels: 3.8, 1.9 and 0.38 mmol/L), temperature (three pairs for the ATES cold/warm well: 5/15 ˚C, 10/10 ˚C, 5/25 ˚C), biomass mobility (purely mobile or immobile), and pH limitation on Fe(III) reduction (absence and presence of such an effect). In the five years’ simulation by the model, complete dechlorination to ethene was achieved within 1 year, in the influence zone of the ATES wells, for the reference scenario with 3.8 mmol/L lactate, 5/15 ˚C ATES well temperatures and mobile biomass. Scenarios with lower dosage of lactate gave results with less dechlorination progress. Growth of biomass, especially iron reducer and lactate fermenter, was significant also in the first year (for both mobile and immobile biomass scenarios). Biomass also spread throughout the influence volume of ATES for both warm and cold wells. However, scenarios with different well-temperature pairs did not noteworthy differ in dechlorination progress. This could probably be due to biomass concentration being the limiting factor in this model setup, while temperature was not. Such situation was quite different than that in Chapter 3, of which experiment with bioaugmentation in the beginning. Besides, the model here could not include the important autocatalytic process (Chapter 3) which generated much faster dechlorination than just could be realized by only temperature increase in this chapter. In general, the modeling in this chapter suggests that applying ATES as engineering tool for biostimulation (substrate injection and bioaugmentation) can be a cost-effective approach to support the combined system.

    Eventually in Chapter 7, overall discussions upon results gained from previous chapters were integrated and the research questions as presented in the introduction are reiterated. In addition, recommendation upon future study, and wider implications with future perspective for practical application are also discussed. We concluded that redox condition is the most essential factor in the ATES-ENA system. The mutual impacts of ATES and ENA were revealed to be quite positive. Elevated temperature in the ATES warm well synergizing with groundwater transport can provide “1 + 1 > 2” effect. Besides, ENA can probably reduce risk of chemical clogging in ATES, instead of causing biological clogging. The further investigation was recommended to perform with larger scale pilot tests. Finally, a brief review of possible applications was given for two countries, the Netherlands and China, which both have dense groundwater and subsurface contaminations around urban areas. The ATES technology is much more mature in the Netherlands, whereas in China, the advantage is the more flexible usage of subsurface. For both countries, ATES-ENA can provide cost‑effective outcomes on both energy production and groundwater management.

    Low-resolution modeling of dense drainage networks in confining layers
    Pauw, P.S. ; Zee, S.E.A.T.M. van der; Leijnse, A. ; Delsman, J.R. ; Louw, P.G.B. de; Lange, W.J. de; Oude Essink, G.H.P. - \ 2015
    Groundwater 53 (2015)5. - ISSN 0017-467X - p. 771 - 781.
    grondwaterstroming - watervoerende lagen - modellen - klimaatverandering - groundwater flow - aquifers - models - climatic change - aquifer - simulation - intrusion - seepage - florida - system - field - flow
    Groundwater-surface water (GW-SW) interaction in numerical groundwater flow models is generally simulated using a Cauchy boundary condition, which relates the flow between the surface water and the groundwater to the product of the head difference between the node and the surface water level, and a coefficient, often referred to as the “conductance.” Previous studies have shown that in models with a low grid resolution, the resistance to GW-SW interaction below the surface water bed should often be accounted for in the parameterization of the conductance, in addition to the resistance across the surface water bed. Three conductance expressions that take this resistance into account were investigated: two that were presented by Mehl and Hill (2010) and the one that was presented by De Lange (1999). Their accuracy in low-resolution models regarding salt and water fluxes to a dense drainage network in a confined aquifer system was determined. For a wide range of hydrogeological conditions, the influence of (1) variable groundwater density; (2) vertical grid discretization; and (3) simulation of both ditches and tile drains in a single model cell was investigated. The results indicate that the conductance expression of De Lange (1999) should be used in similar hydrogeological conditions as considered in this paper, as it is better taking into account the resistance to flow below the surface water bed. For the cases that were considered, the influence of variable groundwater density and vertical grid discretization on the accuracy of the conductance expression of De Lange (1999) is small.
    Modelling and monitoring of Aquifer Thermal Energy Storage : impacts of soil heterogeneity, thermal interference and bioremediation
    Sommer, W.T. - \ 2015
    Wageningen University. Promotor(en): Huub Rijnaarts, co-promotor(en): Tim Grotenhuis; J. Valstar. - Wageningen : Wageningen University - ISBN 9789462572942 - 204
    watervoerende lagen - thermische energie - opslag - energieterugwinning - economische impact - milieueffect - bodemsanering - grondwaterverontreiniging - aquifers - thermal energy - storage - energy recovery - economic impact - environmental impact - soil remediation - groundwater pollution

    Modelling and monitoring of Aquifer Thermal Energy Storage

    Impacts of heterogeneity, thermal interference and bioremediation

    Wijbrand Sommer
    PhD thesis, Wageningen University, Wageningen, NL (2015)
    ISBN 978-94-6257-294-2


    Aquifer thermal energy storage (ATES) is applied world-wide to provide heating and cooling to buildings. Application of ATES, instead of traditional heating and cooling installations, reduces primary energy consumption and related CO2 emissions. Intensified use of the subsurface for thermal applications requires more accurate methods to measure and predict the development of thermal plumes in the subsurface related to thermal interference between systems and address issues concerning subsurface urban planning and wide spread presence of contaminants in urban groundwater systems.

    In this thesis, subsurface heat transport in ATES and the associated influence on storage performance for thermal energy was assessed. Detailed monitoring of subsurface temperature development around the wells of an existing system was achieved by a unique application of Distributed Temperature Sensing (DTS) using glass fibre optical cables. The measurements reveal unequal distribution of flow rate over different parts of the well screen and preferential flow due to aquifer heterogeneity. Heat transport modelling shows that heterogeneity causes preferential flow paths that can affect thermal interference between systems, mainly depending on well-to-well distance and hydrogeological conditions.

    At present, design rules are applied in such way that all negative interference is avoided. However, this limits the number of ATES systems that can be realized in a specific area, especially as these systems generally use only 60% of their permitted capacity. To optimize the use of available aquifer volume, the amount of thermal interference that is acceptable from an economical and environmental perspective was studied for different zonation patterns and well-to-well distances. Selecting the hydrogeological conditions of Amsterdam, the Netherlands, as a case study, this method shows that it is cost-effective to allow a limited amount of thermal interference, such that 30–40% more energy can be provided than compared to the case in which all negative thermal interference is avoided.

    Because many urbanized areas deal with contaminated soil and groundwater, ambitions to increase the number of ATES systems are confronted with the presence of groundwater contaminants. This is of concern, because groundwater movement induced by the ATES system can result in increased mobility and spreading of these contaminants. However, the combination between ATES and soil and groundwater remediation could be a promising integrated technique, both for improving groundwater quality and development of ATES. Opportunities to use ATES as a continuous biostimulation tool for enhanced reductive dechlorination (ERD) have been explored with a reactive transport model.

    Regional scale impact of tidal forcing on groundwater flow in unconfined coastal aquifers
    Pauw, P.S. ; Oude Essink, G.H.P. ; Leijnse, A. ; Vandenbohede, A. ; Groen, J. ; Zee, S.E.A.T.M. van der - \ 2014
    Journal of Hydrology 517 (2014). - ISSN 0022-1694 - p. 269 - 283.
    grondwaterstroming - kustgebieden - watervoerende lagen - groundwater flow - coastal areas - aquifers - sea-water intrusion - saline groundwater - fresh - beaches - discharge - dynamics - lenses - table - zone
    This paper considers the impact of tidal forcing on regional groundwater flow in an unconfined coastal aquifer. Numerical models are used to quantify this impact for a wide range of hydrogeological conditions. Both a shallow and a deep aquifer are investigated with regard to three dimensionless parameter groups that determine the groundwater flow to a large extent. Analytical expressions are presented that allow for a quick estimate of the regional scale effect of tidal forcing under the same conditions as used in the numerical models. Quantitatively, the results in this paper are complementary to previous studies by taking into account variable density groundwater flow, dispersive salt transport and a seepage face in the intertidal area. Qualitatively, the results are in line with previous investigations. The time-averaged hydraulic head at the high tide mark increases upon a decrease of each of the three considered dimensionless parameter groups: R (including the ratio of the hydraulic conductivity and the precipitation excess), a (the slope of the intertidal area) and AL (the ratio of the width of the fresh water lens and the tidal amplitude). The relative change of the location and the hydraulic head of the groundwater divide, which together characterize regional groundwater flow, increase as a and AL decrease, but decrease as R decreases. The difference between the analytical solutions and numerical results is small. Therefore, the presented analytical solutions can be used to estimate the bias that is introduced in a numerical model if tidal forcing is neglected. The results should be used with caution in case of significant wave forcing, as this was not considered.
    Methode voor het bepalen van de potentie voor het toepassen van lokale zoetwateroplossingen : Fresh Water Options Optimizer - fase 1
    Bakel, J. van; Louw, P. de; Stuyt, L.C.P.M. ; Tolk, L. ; Velstra, J. ; Hoogvliet, M. - \ 2014
    Utrecht : Programmabureau Kennis voor Klimaat (Rapport / STOWA 2014-16) - ISBN 9789490070847 - 82
    zoet water - watervoorziening - drainage - infiltratie - sloten - wateropslag - watervoerende lagen - maatregelen - inventarisaties - fresh water - water supply - drainage - infiltration - ditches - water storage - aquifers - measures - inventories
    Binnen Kennis voor Klimaat worden kleinschalige maatregelen ontwikkeld om de zoetwatervoorziening te verbeteren. In deze studie zijn methoden ontwikkeld waarmee de potentie van dergelijke maatregelen op het schaalniveau van een groter gebied, voor hoog en laag Nederland, kan worden verkend. In deze studie zijn de opschalingsmogelijkheden bekeken voor de volgende lokale zoetwateroplossingen: (1) drains2buffer, (2) regelbare en klimaatadaptieve drainage, (3) kreekruginfiltratie, (4) Freshmaker, (5) verticale ASR, (6) waterconservering door stuwen en (7) waterconservering door slootbodemverhoging.
    Response to recharge variation of thin rainwater lenses and their mixing zone with underlying saline groundwater
    Eeman, S. ; Zee, S.E.A.T.M. van der; Leijnse, A. ; Louw, P.G.B. de; Maas, C. - \ 2012
    Hydrology and Earth System Sciences 16 (2012). - ISSN 1027-5606 - p. 3535 - 3549.
    grondwater - watervoerende lagen - zoet water - neerslag - zoutwaterindringing - kustgebieden - groundwater - aquifers - fresh water - precipitation - salt water intrusion - coastal areas - sea-level rise - climate-change - coastal aquifer - water interface - fresh - transport - dispersion - discharge - islands - surface
    In coastal zones with saline groundwater, fresh groundwater lenses may form due to infiltration of rain water. The thickness of both the lens and the mixing zone, determines fresh water availability for plant growth. Due to recharge variation, the thickness of the lens and the mixing zone are not constant, which may adversely affect agricultural and natural vegetation if saline water reaches the root zone during the growing season. In this paper, we study the response of thin lenses and their mixing zone to variation of recharge. The recharge is varied using sinusoids with a range of amplitudes and frequencies. We vary lens characteristics by varying the Rayleigh number and Mass flux ratio of saline and fresh water, as these dominantly influence the thickness of thin lenses and their mixing zone. Numerical results show a linear relation between the normalised lens volume and the main lens and recharge characteristics, enabling an empirical approximation of the variation of lens thickness. Increase of the recharge amplitude causes increase and the increase of recharge frequency causes a decrease in the variation of lens thickness. The average lens thickness is not significantly influenced by these variations in recharge, contrary to the mixing zone thickness. The mixing zone thickness is compared to that of a Fickian mixing regime. A simple relation between the travelled distance of the centre of the mixing zone position due to variations in recharge and the mixing zone thickness is shown to be valid for both a sinusoidal recharge variation and actual records of daily recharge data. Starting from a step response function, convolution can be used to determine the effect of variable recharge in time. For a sinusoidal curve, we can determine delay of lens movement compared to the recharge curve as well as the lens amplitude, derived from the convolution integral. Together the proposed equations provide us with a first order approximation of lens characteristics using basic lens and recharge parameters without the use of numerical models. This enables the assessment of the vulnerability of any thin fresh water lens on saline, upward seeping groundwater to salinity stress in the root zone.
    Analysis of the thickness of a fresh water lens and of the transition zone
    Eeman, S. ; Leijnse, A. ; Raats, P.A.C. ; Zee, S.E.A.T.M. van der - \ 2011
    Advances in Water Resources 34 (2011)2. - ISSN 0309-1708 - p. 291 - 302.
    geohydrologie - watervoerende lagen - zoet water - zout water - delta's - geohydrology - aquifers - fresh water - saline water - deltas - submarine groundwater discharge - porous-media - coastal aquifer - brine transport - barrier-island - interface - flow - infiltration - dispersion - intrusion
    In regions with saline groundwater, fresh water lenses may develop due to rainwater infiltration. The amount of fresh water that is available for e.g. agricultural crops depends on the thickness of the lens and the extent of mixing between fresh and saline water. In this paper, we consider the mixing of fresh water and upward moving saline ground water in low-lying deltaic areas. The parameters that dominate the flow and transport problem are investigated using dimensionless groups and scaled sensitivities. We characterize the numerically simulated thicknesses of the lens and of the mixing zone by spatial moments. Rayleigh number and mass flux ratio, which is the ratio of the salt water seepage and the precipitation, determine the thickness of the fresh water lens. The local thickness of the mixing zone is mainly influenced by the dispersive/diffusive groups and the mass flux ratio. In addition, convergence of streamlines towards an outflow boundary affects the thickness, particularly in the vicinity of this boundary. Analytical and numerical steady state solutions for lens thickness are compared, taking into account upward seepage, for the two cases with and without a density difference between lens and underlying groundwater. Agreement between the numerical and analytical solutions for the lens thickness is good except when the mass flux ratio becomes small. For zero mass flux ratio, it is implicitly assumed in the analytical solution that salt water is stagnant, and that is unrealistic. Relative contributions of longitudinal and transversal hydrodynamic dispersion and diffusion to the thickness of the mixing zone are quantified numerically for different phases of lens formation. Longitudinal dispersion dominates in the early stages of lens formation, while diffusion and transversal dispersion dominate at steady state
    Developing an environmentally appropriate, socially acceptable and gender-sensitive technology for safe-water supply to households in arsenic affected areas in rural Bangladesh
    Amin, N. - \ 2010
    Wageningen University. Promotor(en): Anke Niehof; Wim Rulkens, co-promotor(en): Harry Bruning. - [S.l. : S.n. - ISBN 9789085858164 - 243
    plattelandsontwikkeling - platteland - ontwikkeling - ontwikkelingsstudies - watervoorziening - milieubescherming - grondwater - grondwaterverontreiniging - watervoerende lagen - pijpleidingen - arsenicum - maatschappelijke betrokkenheid - landbouwhuishoudens - waterfilters - drinkwater - sociologie - bangladesh - zuid-azië - rural development - rural areas - development - development studies - water supply - environmental protection - groundwater - groundwater pollution - aquifers - pipelines - arsenic - community involvement - agricultural households - water filters - drinking water - sociology - bangladesh - south asia
    To confront the arsenic crisis in Bangladesh, several options for a safe water supply in the rural As-affected areas are available. Most of these options have shown a minimum scope to mitigate arsenic-related risks because of their poor performance and non-acceptability by the rural households. In this research, therefore, the development of an appropriate technology for an As-free, safe drinking water supply is considered from a local perspective and a societal context. To achieve the goal and objectives of this research, four research questions were formulated (Chapter 1). The first research question is about the technological and socio-economic performance of community-based pipeline water supply systems that use deep aquifers. The second question deals with available and currently implemented household-level arsenic removal technologies in rural Bangladesh. The third addresses the weaknesses, limitations, strengths and advantages of the technologies in terms of a number of technological, social, economic and gender indicators. Fourth, the question is posed of the most promising arsenic removal option for rural house¬holds in terms of its techno¬logical performance and social acceptability and suitability from a gender perspective. The occurrence of As in the Delta region is of geochemical origin and its distribution in the groundwater has distinct regional patterns and depth trends. An overview of the arsenic problem in Bangladesh is given in Chapter 2.

    The overall objective of the research was to develop a socially appropriate and gender-sensitive household-level As removal filter. Technical, socio-economic and cultural aspects were incorporated in this research to assess the development of a sustainable innovation through multi- and interdisciplinary approaches. The technical validation of the systems was carried out through laboratory-based research, to address the efficiency, robustness, operational and maintenance convenience, safety and viability of the technology. For the social research, the model by Spaargaren and Van Vliet (2000) was adjusted to address the filter’s suitability in terms of lifestyle, domestic time-space structures, affordability, standards of comfort, cleanliness, convenience and modes of provision. In addition, I also considered the household resource-based affordability during the operation and maintenance phase, in terms of a socio-technological and gender perspective. A conceptual model was developed to guide the research and to answer the research questions (Chapter 1). The socio-economic data on the main concepts of this research work were collected through a survey (Appendix 2).

    In this research, a synthesis of knowledge resulting from disciplinary, open-ended collaboration and local perspectives is achieved. Such a transdisciplinary research approach ensures an integration of knowledge through the participation of a variety of stakeholders, including end users, and mutual learning between the different stakeholders, such as users of the Modified Garnet Homemade Filter (MGH Filter), caretakers, village committees, implementing organizations and donors, users of water, households, and women.

    The community–based piped water supply in Bangladesh
    There are several alternative sources to get safe and As-free drinking water in Bangladesh. A community-based piped water supply system using deep aquifers is one of them. In this research, three community-based piped water supply systems were compared to evaluate their technological and economic sustainability, the sustainability of using deep aquifers for the long term, and the social and gender appropriateness of the systems, based on the users’ perspective (Chapter 4). The technical performance of the three systems in different geological conditions was found satisfactory in terms of their efficacy, water quality, adequacy of the water supply, and operations and maintenance. The water is As- and Fe-free and is of good taste. The concentration of As is below the limiting range of drinking water in Bangladesh (50µgL-1As), as well as within the WHO and new EPA standards (10µgL-1As). The sustainable use of deep aquifers for a longer period is a serious issue. To address the sustainability, hydro-geological factors need to be well understood. Overextraction of water from deep aquifers could induce a downward migration of dissolved As and permanently destroy the deep resource. Only one system is practicing chlorination to disinfect the water in the overhead tank, while the other two systems do not have such a provision. However, the field data reveal that the three systems are technologically acceptable and do not require disposal of contaminated sludge.

    The women who are using one of the three water supply systems are satisfied about the water supply systems. They think the systems reliable in their delivery of adequate water and convenient and comfortable for the women users. Women can get water close to their house, which saves collection time and a physical burden. The appointed caretakers are operating the systems efficiently, including maintenance and the collection of the monthly bill from the beneficiaries. The economical sustainability seems to be satisfactory, provided the initial costs are subsidized by external financial assistance with only a little contribution from the communities, which varies from five to seven percent of the total capital cost. The community participation in sharing the installation cost for the system and the monthly bill are fixed, based on the economical condition of the households. However, a drawback of the community-based piped water system is disruption of the system due to its sensitivity to power failure, which is a big problem in Bangladesh. Other shortcomings are the limitations to extend the system to meet the increasing demand of the village people. On the long term, economical sustainability factors need to be considered, such as the availability of funds and the participation of the users in the system’s management, which were absent in all three systems.

    Currently available and implemented household-level arsenic removal technologies

    The application of arsenic removal technologies to provide safe drinking water in rural areas plays a vital role where other, alternative options and safe aquifers are not easily available and where community-based pipeline water supply systems are not feasible. In this research, physico-chemical and biological as well as conventional techniques for the removal of arsenic were reviewed (Chapter 5). Based on literature, an inventory was carried out of 40 available and currently implemented technologies at the household level in terms of their arsenic removal efficiency, cost and users’ acceptance. All the technologies remove As from the water to a limited extent. Therefore, there is scope for further development of these technologies. A multiple-criteria analysis (MCA) approach was applied to select a technology for the further development of an appropriate arsenic removal filter for household-level use. In the research, based on the integrated assessments, the MCA-GARNET technology was selected for further development.

    An assessment of the performances of the three governmentally certified arsenic removal technologies for rural household use was carried out (Chapter 5). This research concludes that the government’s investments in an improved water supply so far have failed to meet the needs of the poor villagers, because they are not able to buy the costly Alcan and Read-F filters. Even the relatively cheap Sono filter proved to be unaffordable for the poorest. Furthermore, assessing the As removal efficiency and life span of these filters is difficult at this preliminary stage, and so is predicting how the disposal of the spent filter materials will be carried out by the users. The As leaching from the sludge/waste generated by the three treatment processes is dependent on the type of removal mechanism and the ultimate sludge disposal methods.

    Development of a chemical-free arsenic removal technology for household use

    In this research, by the active participation of potential end users and other stakeholders, I have included local knowledge and social and gender perspectives in the process of the development of an innovative As removal filter (MGH filter) (Chapter 6). The MGH filter efficiency and breakthrough point were studied at different operational variables, such as filter bed thickness, types of filter media and flow rate. The toxicity of the spent material was addressed by a TCLP test. The developed filter meets the Bangladesh standard for arsenic in drinking water (50µgL-1). It can reduce the arsenic concentrations of the shallow tube well water samples from 160-959µgL-1 to 0-50µgL-1. It can also remove bacteriological contamination in terms of total coliform and fecal coliform counts from >500 to 0 cfu/100 mL-1 . The filter consists of two-bucket filters in series, each with three filter material layers of 14 cm thickness each, containing sand, brick chip and sand (Figure 7.1). The first-class brick chips of 1.3 cm size and Sylhet coarse sands were found to be the most efficient. The major advantage of this unit is that it does not require any daily addition of chemicals and can be operated at a high flow rate. It needs to be cleaned regularly to prevent bacterial contamination, while its maintenance requires treatment with bleaching powder at 15-day intervals. The filter is cost–effective and viable; the investments and operational cost are about € 10.8-13.4 and € 0.11-0.14 per 100 liters of treated water, respectively.

    In this research, a multi-perspective and participatory socio-technological assessment of the filter’s performance during the field level application was carried out in two phases: the trial phase during March 2008 and the evaluation phase during July 2008 (Chapter 7). Eight MGH filters were distributed among eight households in the research area in Kumarbhog. In this research, the multi-perspective assessment comprised interdisciplinary and transdisciplinary approaches to evaluate the performance of the filters for household use. Both quantitative and qualitative methods of data collection and analysis were used. The suitability and acceptability of the filters were evaluated through systematic observation, interviewing, FGDs and eight case studies of the filter users. The compatibility and appropriate¬ness of the filter were viewed from a gender pers¬pective, since access to safe water is an important practical gender need of women, directly related to their domestic and reproductive role.

    Women of the selected eight rural households adopted the technology and ran the filters successfully during the trial phase. As elsewhere in developing countries, in Bangladesh too, rural women are the managers of water for household use. They hardly participate in income generation. The male household head controls the allocation of household income and expenditures, which caused problems when women wanted to re-install their filter. The household survey revealed that sometimes, women cannot be bothered to fetch safe water from far away and, instead, drink the con¬taminated water from their own shallow tube wells. Having the appliance inside the house complied well with the social norms and religious restrictions (purdah) that women have to abide by. In these circumstances, the MGH filter was eagerly accepted by the eight households, because it reduced women’s social and physical burden to fetch As-free, safe water far from their home. In the evaluation phase, some filters were unused because the women could not persuade their husbands to purchase the necessary filter bed materials. During the evaluation phase, the performance of the filters declined compared to the trial phase, because not all users followed the instructions on its operation and maintenance, such as proper chlorination and clean¬liness of the appliance. Disposal of spent filter material was carried out in different ways by the MGH filter users, but more investigation is needed to enable an environmentally friendly disposal of the As-rich sludge.

    A new filter system has been developed that can be used by women at the household level. In terms of the simplicity of construction, operation and maintenance, As removal efficiency, and bacterial removal efficiency, its technical performance is good. It is also very cost-effective. However, because such a system always needs to be completely safe for producing drinking water, on the long term as well as under local and household conditions other than those investigated in this research project, further evaluation and additional research will be necessary. In this research, the filter was field-tested under controlled conditions for a month and evaluated after three months. Considering the need for arsenic treatment options in Bangladesh and other developing countries, further research on the performance of the MGH technology could have important positive implications for a safe water supply. Therefore, to allow for seasonality, the MGH filter should be pilot-tested and properly developed over a period of at least a year, in different geographical conditions. A social, economic and technical validation of the MGH filter should be included in the pilot-testing in different parts of the country by applying interdisciplinary and transdisciplinary approaches. Because women are the collectors and managers of drinking water, doing the validation in different parts of the country allows for variation in women’s roles and position and the local socio-cultural context. The MGH filter should be submitted for certification by the government of Bangladesh after further testing and development. The technological principle of the MGH filter may be used to research and develop a community-based low-cost arsenic removal water supply system in rural areas. The results of this research testify to the feasibility of a gender-sensitive, socially acceptable and technologically sound, sustainable solution to the problem of the As contamination of water for household use in rural areas in Bangladesh.

    Incentives to reduce groundwater extraction in Yemen
    Hellegers, P.J.G.J. ; Perry, J.N. ; Al-Aulaqi, N. ; Al-Eryani, A.R. ; Al-Hebshi, M. - \ 2008
    The Hague : LEI Wageningen UR (Report / LEI : Research area 1, International policy ) - ISBN 9789086152704 - 131
    stimulansen - grondwater - grondwaterwinning - grondwaterstand - watervoerende lagen - welpijpen - duurzaamheid (sustainability) - irrigatie - hulpbronnengebruik - watergebruik - landbouw - waterbescherming - boeren - houding van boeren - sociale economie - waterbeleid - regering - jemen - verdroging (milieu) - economische verandering - incentives - groundwater - groundwater extraction - groundwater level - aquifers - tube wells - sustainability - irrigation - resource utilization - water use - agriculture - water conservation - farmers - farmers' attitudes - socioeconomics - water policy - government - yemen - groundwater depletion - economic change
    This report describes the results of the study on options for changing the eco-nomic incentive structure for groundwater extraction in Yemen. The study aims to evaluate the potential role of economic incentives to reduce unsustainable ir-rigation water consumption and to make recommendations for implementing water conservation incentives. It first identifies factors that have triggered groundwater overdraft, then studies farmers' behaviour regarding groundwater extraction on the basis of in-depth interviews with farmers in each of the follow-ing three basins - in the Sana'a Basin, the Taiz Basin and Wadi Hadramout. Fi-nally, a number of changes in the incentive structure are evaluated, among others incentives that decrease the profitability of irrigation water use and sub-sidies on improved irrigation technology. The study shows that although the lit-erature and economic theory suggest that the range of possible interventions is wide (water pricing, metering, water rights, water markets, taxes, subsidies, in-formation, participatory management, et cetera), the range of potentially effec-tive interventions in the Yemeni political context is more limited. The Yemeni case is unique, as there is a close linkage between water and a central socio-economic issue: qat. This adds to the difficulties of implementing or enforcing change.
    Variation in space and time of water flow and solute transport in heterogeneous soils and aquifers : a new multi-compartment percolation sampler and a new parameterization of the spatio-temporal solute distribution
    Bloem, E. - \ 2008
    Wageningen University. Promotor(en): Reinder Feddes, co-promotor(en): G.H. de Rooij. - S.l. : S.n. - ISBN 9789085049227 - 153
    grondwaterstroming - opgeloste stof - transportprocessen - watervoerende lagen - variatie in de tijd - bemonsteren - distributie - grondwaterverontreiniging - ruimtelijke variatie - groundwater flow - solutes - transport processes - aquifers - temporal variation - sampling - distribution - groundwater pollution - spatial variation
    Het experimentele en theoretische onderzoek gepresenteerd in dit proefschrift heeft geleid tot een verbetering van de mogelijkheden om stoffentransport in de ondergrond beneden een onverzadigde bodem te observeren. De lange termijn prestaties van de nieuwe multi-compartement samplers onder de ruwe omstandigheden van het open veld waren overtuigend. De samplers bleken geschikt voor een grotere verscheidenheid aan toepassingen
    Solubility of arsenic in multi-component systems : from the microscopic to macroscopic scale
    Stachowicz, M. - \ 2007
    Wageningen University. Promotor(en): Willem van Riemsdijk. - [S.l.] : S.n. - ISBN 9789085047650 - 207
    bodemchemie - arsenicum - oplosbaarheid - grondwaterverontreiniging - grondwaterwinning - drinkwater - watervoerende lagen - soil chemistry - arsenic - solubility - groundwater pollution - groundwater extraction - drinking water - aquifers
    Arsenic in groundwater has generated one of the most important problems with respect to the quality of drinking water in the modern world. The aim of this thesis has been to assess, as good as possible for the present state of the art, the factors and processes that govern the arsenic behavior in contaminated aquifers. The research tactics have included 3 sequential steps: (1) obtaining adsorption datasets for systems simulating relevant groundwater field situations; (2) interpretation of these data with a molecular based adsorption model and the model application to predict the adsorption behavior of arsenic for a range of compositions relevant in the field; (3) providing quantitative understanding of the behavior of arsenic in natural waters. This knowledge may contribute to a better understanding of the problem, the long-term solutions, such as an optimization of treatment techniques for drinking water as well as a methodology to guide the positioning of new arsenic-free wells
    Decentrale voorziening in energie, water en andere nutsfuncties
    Mels, A.R. ; Andel, N. van; Kristinsson, J. ; Wortman, E. ; Oei, P. ; Wilt, J. de; Lettinga, G. ; Zeeman, G. - \ 2006
    Spil 5 (2006)229-230. - ISSN 0165-6252 - p. 12 - 18.
    tuinbouw - energiebehoeften - energie - recycling - woonwijken - verwarming - innovaties - watervoerende lagen - huisvesting - glastuinbouw - energiebesparing - horticulture - energy requirements - energy - recycling - housing - residential areas - heating - innovations - aquifers - greenhouse horticulture - energy saving
    Presentatie van een nieuw ontwerp van een tuinbouwkas met een daaraan gekoppelde woonwijk. Het ontwerp, Zonneterp genaamd, is o.a. gebaseerd op een kas, die tijdens de zomer overtollige warmte opslaat in aquifers en deze warmte kan gebruiken voor het verwarmen van de kas en de woningen tijdens de nacht of gedurende de winter
    De doorlatendheid van de bodem voor infiltratiedoeleinden; een gebiedsdekkende inventarisatie voor het Waterschap Peel en Maasvallei
    Massop, H.T.L. ; Gaast, J.W.J. van der; Kiestra, E. - \ 2005
    Wageningen : Alterra (Alterra-rapport 1212) - 95
    permeabiliteit - infiltratie - hydraulisch geleidingsvermogen - kwel - watervoerende lagen - grondwaterstroming - fysische bodemeigenschappen - grondwater - geohydrologie - limburg - permeability - infiltration - hydraulic conductivity - groundwater - mapping - seepage - aquifers - groundwater flow - geohydrology - limburg
    In opdracht van waterschap Peel en Maasvallei is een onderzoek uitgevoerd naar de geohydrologische eigenschappen van het topsysteem. Het waterschap gebruikt deze informatie bij de beoordeling en advisering ten behoeve van infiltratievoorzieningen. Voor de beoordeling van deze voorziening zijn de doorlatendheid en de dikte van de deklaag van belang alsook het doorlaatvermogen van het onderliggende watervoerende pakket. Voor het gebiedsdekkend vaststellen van de eigenschappen is het gebied geschematiseerd in 60 eenheden op basis van bodemeigenschappen en opbouw diepere ondergrond. Aan deze eenheden is een k-waardetabel gekoppeld. Deze tabel is gebaseerd op beschikbare metingen en schattingen en aangevuld met metingen die in het kader van dit onderzoek zijn uitgevoerd. Naast k-waarden is een diktekaart van de deklaag vervaardigd op basis van bruikbare boringen. Het doorlaatvermogen van het eerste watervoerend pakket is afgeleid uit verschillende bronnen, waaronder pompproeven. Een belangrijk punt bij gebruik van de geïnventariseerde gegevens is de anisotropie van de deklaag als gevolg van het voorkomen van klei, leem of veenlagen
    Praktijkexperiment duurzame energieverzameling door middel van daksproeiers
    Zwart, H.F. de - \ 2004
    onbekend : Agrotechnology & Food Sciences Group (Report / Wageningen UR, Agrotechnology & Food Innovations 233) - ISBN 9789067548083 - 49
    energiegebruik - duurzaamheid (sustainability) - zonne-energie - warmteopslag - watervoerende lagen - koelsystemen - warmteoverdracht - meting - binnenklimaat - glastuinbouw - energy consumption - sustainability - solar energy - heat retention - aquifers - cooling systems - heat transfer - measurement - indoor climate - greenhouse horticulture
    Kassen hebben in de zomer veel warmte over en komen in de winter warmte tekort. Wanneer de overtollige warmte in de zomer verzameld en opgeslagen kan worden zou de kas in de winter met duurzame energie verwarmd kunnen worden. Omdat het om grote hoeveelheden warmte gaat kunnen de zomerse overschotten niet in bovengrondse buffers worden opgeslagen, maar moeten hier ondergrondse watervoerende lagen worden gebruikt (aquifers, zie KADER 3). Warmteopslag in aquifers kan door water tussen twee putten heen en weer te pompen, waarbij de ene put zo’n 5 °C kouder dan de gemiddelde bodemteperatuur is en de andere zo’n 5 °C warmer. De warmte en koudeverliezen blijven hierdoor beperkt. Het zal duidelijk zijn dat voor de toepassing van warmte met een temperatuur van rond de 15 °C een warmtepomp gebruikt moet worden (Zie KADER 1). Deze warmtepomp koelt het water uit de warme put af naar zo’n 5 °C en maakt hiermee een bron met koud water. Om in de winter van het volgende jaar opnieuw van de warmtepomp gebruik te kunnen maken moet dit koude water weer worden opgewarmd. A&F in Wageningen heeft onderzoek gedaan naar de mogelijkheid om deze opwarming te realiseren met standaard dekbesproeiingssystemen. Dit zijn relatief goedkope systemen die ook nu al op veel kassen gebruikt worden. Het belangrijkste verschil tussen het nu onderzochte systeem in de bestaande systemen is dat bij gangbare sproeiers kaskoeling plaatsvindt door verdamping van water, en in het voorgestelde nieuwe systeem de lage temperatuur van het opgespoten water koeling aan de kas geeft. Zo worden drie vliegen in één klap geslagen namelijk: 1. de sproeiers geven een groter koelvermogen 2. er wordt duurzame energie verzameld, waarmee in de winter gas kan worden bespaard 3. het verdampingsverlies wordt beperkt.
    In-situ metal precipitation in a zinc-aerobic, sandy aquifer by means of biological sulfate reduction
    Janssen, G.M.C.M. ; Temminghoff, E.J.M. - \ 2004
    Environmental Science and Technology 38 (2004)14. - ISSN 0013-936X - p. 4002 - 4011.
    terugwinning - sulfaten - neerslag - kooldioxide - decontaminatie - waterverontreiniging - watervoerende lagen - biologische behandeling - zware metalen - zink - recovery - sulfates - precipitation - carbon dioxide - decontamination - water pollution - aquifers - biological treatment - heavy metals - zinc - acid-mine drainage - reducing bacteria - removal - carbon - water - reactor - effluent - ethanol - energy - growth
    The applicability of in situ metal precipitation (ISMP) based on bacterial sulfate reduction (BSR) with molasses as carbon source was tested for the immobilization of a zinc plume in an aquifer with highly unsuitable initial conditions (high Eh, low pH, low organic matter content, and low sulfate concentrations), using deep wells for substrate injection
    The applicability of in situ metal precipitation (ISMP) based on bacterial sulfate reduction (BSR) with molasses as carbon source was tested for the immobilization of a zinc plume in an aquifer with highly unsuitable initial conditions (high E-h, low pH, low organic matter content, and low sulfate concentrations), using deep wells for substrate injection. Batch experiments revealed an optimal molasses concentration range of 1-5 g/L and demonstrated the necessity of adding a specific growth medium to the groundwater. Without this growth medium, even sulfate, nitrogen, phosphorus, and potassium addition combined with pH optimization could not trigger biological sulfate reduction. In column experiments, precipitation of ZnS(s) was induced biologically as well as chemically (by adding Na2S). In both systems, zinc concentrations dropped from about 30 mg/L to below 0.02 mg/L. After termination of substrate addition the biological system showed continuation of BSR for at least 2 months, suggesting the insensitivity of the sulfate reducing system for short stagnations of nutrient supply, whereas in the chemical system an immediate increase of Zn concentrations was observed. A pilot experiment conducted in situ at the zinc-contaminated site showed a reduction of zinc concentrations from around 40 mg/L to below 0.01 mg/L. Termination of substrate supply did not result in an immediate stagnation of the BSR process, but continuation of BSR was observed for at least 5 weeks.
    Praktijkmeting aan een ondergronds energieopslagsysteem en validatie van een dynamisch simulatiemodel
    Campen, J.B. ; Zwart, H.F. de - \ 2004
    Wageningen : Agrotechnology & Food Innovations (Rapport / Agrotechnology and Food Innovations 058) - ISBN 9789067547437 - 31
    watervoerende lagen - thermische energie - simulatiemodellen - kassen - ondergrondse opslag - glastuinbouw - aquifers - thermal energy - simulation models - greenhouses - underground storage - greenhouse horticulture
    Well clogging by particles in Dutch well fields
    Timmer, H. ; Verdel, J.D. ; Jongmans, A.G. - \ 2003
    Journal American Water Works Association 95 (2003)8. - ISSN 0003-150X - p. 112 - 118.
    grondwaterwinning - blokkering - watervoerende lagen - putten - watervoorziening - nederland - groundwater extraction - blockage - aquifers - wells - water supply - netherlands
    For the water supply company Hydran South Holland in the Netherlands, clogged wells constituted a significant problem that lowered production capacity of the well field, disrupted the purification process at the treatment plant, and decreased overall revenues. This study was undertaken to develop a better understanding of the dogging process, the nature of the clogging materials, and the exact position of these materials in the well. The Hydron South Holland wells pump anaerobic groundwater from aquifers consisting of Pleistocene, sandy, and fluvial sediments, Samples were collected from a number of wells with a reduced specific capacity. Light microscopy and electron microscopy were performed on undisturbed samples, and particle size distribution and chemical analyses were conducted on bulk samples. On the basis of study results, a new two-pronged rehabilitation procedure was developed for seriously clogged wells. Initial findings indicate that the procedure offers both good immediate results and a significantly lower clogging rate over the long term. Hydron South Holland is conducting further research to prevent initial clogging and fine-tune well drilling techniques and well design. Utilities experiencing well clogging in similar aquifer conditions can use these findings to optimize their own rehabilitation procedures or as a jumping-off point for new research on well clogging and well design. - MPM.
    Energie in balans; Evaluatie van warmteterugwinning uit een aquifer met elektrische warmtepompen op een glastuinbouwbedrijf met grondkoeling in 2002
    Ravensbergen, P. ; Vernooy, C.J.M. - \ 2003
    Den Haag : LEI (Rapport / LEI : Domein 3, Natuurlijke hulpbronnen en milieu ) - ISBN 9789052428710 - 60
    glastuinbouw - evaluatie - watervoerende lagen - warmteterugwinning - warmtepompen - thermische energie - nederland - warmteopslag - greenhouse horticulture - evaluation - aquifers - heat recovery - heat pumps - thermal energy - netherlands - heat retention
    Dit rapport is een beschrijving van een energetische, technische en economische evaluatie van warmteterugwinning uit een aquifer met elektrische warmtepompen op een vermeerde-ringsbedrijf van 3,5 ha glas in de praktijk, gedurende de periode van december 2001 tot december 2002. Aan de hand van de bevindingen van deze praktijkevaluatie, is een rendementsbere-kening gemaakt voor een normaal glastuinbouwproductiebedrijf met grondkoeling, waar al elektrische aangedreven koelmachines aanwezig zijn. Het rapport besluit met een aantal praktische aanbevelingen waarop te letten, indien een ondernemer warmteterugwinning met een aquifer overweegt.
    Analytical Solution for Transient Water Table Heights and Outflows from Inclined Ditch-Drained Terrains
    Verhoest, N.E.C. ; Pauwels, V.R.N. ; Troch, P.A. ; Troch, F.P. De - \ 2002
    Journal of Irrigation and Drainage Engineering-Asce 128 (2002)6. - ISSN 0733-9437 - p. 358 - 364.
    watervoerende lagen - grondwaterstroming - grondwateraanvulling - modellen - aquifers - groundwater flow - groundwater recharge - models
    This paper presents two analytical solutions of the linearized Boussinesq equation for an inclined aquifer, drained by ditches, subjected to a constant recharge rate. These solutions are based on different initial conditions. First, the transient solution is obtained for an initially fully saturated aquifer. Then, an analytical expression is derived for the steady state solution by allowing time to approach infinity. As this solution represents the groundwater table shape more realistically, this water table profile is used as an initial condition in the derivation of the second analytical solution for the groundwater table height, and the in- and outflow into the ditches. The solutions allow the calculation of the transient behavior of the groundwater table, and its ouflow, due to changing percolation rates or water level heights in both ditches.
    Toepasbaarheid van aquifers in de glastuinbouw voor aardwarmtewinning en warmteopslag
    Braak, N.J. van de - \ 2001
    Wageningen : IMAG [etc.] (IMAG nota P 2001-120) - 77
    watervoerende lagen - geothermische energie - warmteterugwinning - warmtebehoud - glastuinbouw - aquifers - geothermal energy - heat recovery - heat conservation - greenhouse horticulture
    SATEM 2002: software for aquifer test evaluation
    Boonstra, J. ; Kselik, R.A.L. - \ 2001
    Wageningen : ILRI (ILRI publication 57) - ISBN 9789070754549 - 148
    watervoerende lagen - grondwaterstroming - permeabiliteit - modellen - pompproeven - bodemfysica - grondwater - hydrologie - software - aquifers - groundwater flow - permeability - models - pumping tests - software
    Transport of nonlinearly biodegradable contaminants in aquifers
    Keijzer, H. - \ 2001
    Wageningen University. Promotor(en): S.E.A.T.M. van der Zee. - S.l. : S.n. - ISBN 9789058083395 - 134
    besmetters - watervoerende lagen - biodegradatie - bioremediëring - contaminants - aquifers - biodegradation - bioremediation

    This thesis deals with the transport behavior of nonlinearly biodegradable contaminants in aquifers. Such transport occurs during in situ bioremediation which is based on the injection of an electron acceptor or electron donor. The main interests in this thesis are the mutual influences of underlying processes, i.e. transport, adsorption and biodegradation, and their influence on in situ bioremediation performance. To gain insight in these influences, the processes in a homogeneous aquifer are studied. Subsequently, the effect of physical heterogeneity of an aquifer on the displacement of the biodegradable contaminant is examined.

    Considering a homogeneous aquifer, numerical simulations are performed to ascertain the effect of transport, adsorption and biodegradation on the displacement of the contaminant and of the electron acceptor or electron donor. In the initial phase, the developed numerical results are successfully described by first order degradation. In the final phase, the numerical results show a traveling wave behavior; the developed concentration fronts have constant front shapes and 'travel' with a constant velocity through the aquifer. This behavior is due to the balance between the steepening effect of nonlinear biodegradation and the spreading effect of dispersion. Because of this traveling wave behavior, semi-analytical solutions have been derived that satisfactorily approximate the numerical results. These semi-analytical solutions are used to assess the performance of the in situ bioremediation. If in situ bioremediation is applied to a polluted site, the electron acceptor injection concentration and the injection velocity will be the only manipulative properties. By varying these two properties, the in situ bioremediation performance can be influenced and optimized.

    To study a physical heterogeneous aquifer, the hydraulic conductivity is considered spatially variable and it is assumed to be a random space function. The effect of physical heterogeneity is determined using a Lagrangian stochastic approach. Results show that incorporation of physical heterogeneity leads to a spreading of the breakthrough curve of both the contaminant and the electron acceptor or electron donor. In case of a large degree of heterogeneity, i.e. a strongly heterogeneous aquifer, it is the heterogeneity which determines the shape of the breakthrough curve and not the dispersion or nonlinear biodegradation.

    Results of Aquifer Test Analyses of the Fordwah Eastern Sadiqia (South) Project, Bahawalnagar
    Boonstra, J. ; Javed, I. - \ 1999
    Lahore : IWASRI - 102
    grondwater - watervoerende lagen - pakistan - pompproeven - groundwater - aquifers - pakistan - pumping tests
    Improved parameter estimation for hydrological models using weighted object functions
    Stein, A. ; Zaadnoordijk, W.J. - \ 1999
    Hydrological Processes 13 (1999). - ISSN 0885-6087 - p. 1315 - 1328.
    hydrologie - modellen - kalibratie - watervoerende lagen - geohydrologie - zuid-holland - hydrology - models - calibration - aquifers - geohydrology - zuid-holland
    This paper discusses the sensitivity of calibration of hydrological model parameters to different objective functions. Several functions are defined with weights depending upon the hydrological background. These are compared with an objective function based upon kriging. Calibration is applied to piezometric readings from the Isle of Goeree in the Netherlands. For a study on the permeability of the first aquifer, the kriging predictor yields weights that differ from using prior knowledge, and emphasizes more strongly spatially isolated points than commonly applied objective functions. It reduces the range of differences between measurements and model simulations, but the mean absolute error increases. For a study on the resistance of the top layer and of the aquitard, use of prior information in the objective functions leads to a reduction in standard deviations of the differences between measured and calculated values by 40-80%
    Analytical approximation to characterize the performance of in situ aquifer bioremediation
    Keijzer, H. ; Dijke, M.I.J. van; Zee, S.E.A.T.M. van der - \ 1999
    Advances in Water Resources 23 (1999). - ISSN 0309-1708 - p. 217 - 228.
    bioremediëring - watervoerende lagen - besmetters - verwijdering - modellen - grondwaterverontreiniging - geohydrologie - bioremediation - aquifers - contaminants - removal - models - groundwater pollution - geohydrology
    Characteristic regimes for in-situ bioremediation of aquifers by injecting water containing an electron acceptor.
    Keijzer, H. ; Zee, S.E.A.T.M. van der; Leijnse, A. - \ 1998
    Computational Geosciences 2 (1998). - ISSN 1420-0597 - p. 1 - 22.
    bioremediëring - watervoerende lagen - simulatiemodellen - grondwaterverontreiniging - geohydrologie - bioremediation - aquifers - simulation models - groundwater pollution - geohydrology
    Geohydrologisch veldonderzoek in het Purmerbos : uitwerkingen en interpretatie van doorlatendheidsmetingen en pompproeven
    Gaast, J.W.J. van der; Peerboom, J.M.P.M. - \ 1996
    Wageningen : DLO-Staring Centrum (Rapport / DLO-Staring Centrum 437) - 65
    watervoerende lagen - conservering - milieubescherming - bosbouw - bossen - permeabiliteit - gesteenten - nederland - noord-holland - pompproeven - aquifers - conservation - environmental protection - forestry - forests - permeability - rocks - netherlands - noord-holland - pumping tests
    Klimaatregeling met koude-opslag in vleesvarkensstallen
    Verdoes, N. ; Telle, M.G. ; Mouwen, I.A.A.C. ; Tuinte, J.H.G. ; Vrielink, M.G.M. ; Brakel, C.E.P. van - \ 1996
    Rosmalen : Praktijkonderzoek varkenshouderij (Proefverslag / Praktijkonderzoek Varkenshouderij P1.161) - 40
    energie - opslag - geothermische energie - watervoerende lagen - varkensstallen - afmesten - varkens - nederland - energy - storage - geothermal energy - aquifers - pig housing - finishing - pigs - netherlands
    Intreeweerstanden waterlopen; inventarisatie en analyse
    Jousma, G. ; Massop, H.T.L. - \ 1996
    Delft : TNO (TNO - rapport GG-R-96-15(A)) - 135
    watervoerende lagen - grondwateraanvulling - hydraulisch geleidingsvermogen - infiltratie - permeabiliteit - drainage door leidingen - gesteenten - kwel - buisdrainage - intreeweerstand - pompproeven - aquifers - groundwater recharge - hydraulic conductivity - infiltration - permeability - pipe drainage - rocks - seepage - tile drainage - entrance resistance - pumping tests
    Het inventarisatie-onderzoek Intreeweerstanden Waterlopen is te beschouwen als het belangrijkste researchdeel van het Project 'Informatiesysteem Ontwateringsstelsels'. Dit project had tot doel de criteria te onderzoeken voor het vastleggen van met name de tertiaire ontwateringsstelsels in een landsdekkend informatiesysteem ten behoeve van geohydrologisch (model)onderzoek.
    Ecohydrology in the Netherlands: principles of an application-driven interdiscipline
    Grootjans, A.P. ; Wirdum, G. van; Kemmers, R.H. ; Diggelen, R. van - \ 1996
    Acta botanica neerlandica 45 (1996). - ISSN 0044-5983 - p. 491 - 516.
    watervoerende lagen - bibliografieën - chemische eigenschappen - ecologie - grondwater - hydrologie - landschap - landschapsecologie - nederland - ecohydrologie - aquifers - bibliographies - chemical properties - ecology - groundwater - hydrology - landscape - landscape ecology - netherlands - ecohydrology
    Doorlatendheidsmetingen: absolute noodzaak of luxe uit het verleden?
    Pomper, A.B. ; Weerts, H.J.T. - \ 1996
    Stromingen : vakblad voor hydrologen 2 (1996)1. - ISSN 1382-6069 - p. 27 - 37.
    watervoerende lagen - permeabiliteit - gesteenten - pompproeven - aquifers - permeability - rocks - pumping tests
    De bepaling van de doorlatendheid van zandpakketten houdt de gemoederen van hydrologen al meer dan een eeuw bezig. Vele bepalingsmethoden zijn in die tijd ontwikkeld. Sommige geven een globale waarde, toepasbaar in grootschalige modellen; andere gevenwaarden die meer voor lokale problemen geschikt zijn. Dit artikel geeft een overzicht van de bestaande methoden. De vraag wordt gesteld of in een tijd van krappe financiële mogelijkheden het verantwoord is dergelijk kostbaar onderzoek uit te voeren. Het artikel richt zich op een discussie tussen de instanties die zich met dergelijk onderzoek bezighouden, met als doel een betere afstemming van het onderzoek en de uitwisselbaarheid van de resultaten.
    Schatting van doorlaatfaktoren (k-waarden) aan de hand van in boorarchieven aanwezige boorbeschrijvingen
    Pomper, A.B. - \ 1996
    Stromingen : vakblad voor hydrologen 2 (1996)4. - ISSN 1382-6069 - p. 37 - 46.
    watervoerende lagen - permeabiliteit - gesteenten - pompproeven - aquifers - permeability - rocks - pumping tests
    In het verleden werden tijdens het beschrijven van boormonsters verschillende parameters geschat waarmee het specifiek oppervlak van zandige monsters kan worden vastgesteld. Vervolgens werden met tabellen doorlatendheden berekend. Later werden ook bestaande boorbeschrijvingen van deze geschatte waarden voorzien. Met de aldus verkregen doorlatendheidscijfers kunnen gemeten waarden van ver uit elkaar gelegen meetpunten worden gecorreleerd. De boorbeschrijvingen uit de jaren zeventig zijn opnieuw bestudeerd om een trend in de bijgeschreven parameters te kunnen vinden. Het resultaat werd vastgelegd in tabellen.
    Advective - dispersive contaminant transport towards a pumping well
    Kooten, J.J.A. van - \ 1996
    Agricultural University. Promotor(en): J. Grasman; M. de Gee. - S.l. : Van Kooten - ISBN 9789054854722 - 120
    milieu - grondwater - watervoerende lagen - computersimulatie - simulatie - simulatiemodellen - waterkwaliteit - verontreinigingsbeheersing - grondwaterverontreiniging - bescherming - grondwaterstroming - modellen - permeabiliteit - gesteenten - colloïden - dispersie - pompproeven - environment - groundwater - aquifers - computer simulation - simulation - simulation models - water quality - pollution control - groundwater pollution - protection - groundwater flow - models - permeability - rocks - colloids - dispersion - pumping tests

    In this thesis we describe an analytical approximation method for predicting the advective- dispersive transport of a contaminant towards a pumping well. The groundwater flow is assumed to be stationary and essentially horizontal. Due to dispersion contaminant transport is a stochastic process. We derive approximations for the arrival probability (or fraction) of particles at a well, for the mean and variance of the arrival time and for the arrival time distribution at a well. The advective flow yields first order approximations. The effect of longitudinal dispersion is included by expanding the first and second moment of the arrival time in power series of the longitudinal dispersion coefficient. Transversal dispersion only plays a crucial role near the separating streamlines bounding the catchment area of a well. Its effect is analyzed locally with boundary layer techniques. The incorporation of linear equilibrium adsorption and first order decay is rather straightforward. The asymptotic approximations are compared with the results of random walk simulations.

    A self-contained part of this thesis is devoted to the transport of a kinetically adsorbing contaminant. We show that once the transport of a non-adsorbing contaminant has been computed, the effect of first order kinetics can be incorporated naturally by utilizing a stochastic description of the residence time of particles in the free phase.

    The results of our research have been implemented in the software package ECOWELL. The input of ECOWELL consists of a head field generated with a numerical flow model. The technical documentation of ECOWELL is part of this thesis. The use of ECOWELL is demonstrated in a case study.

    A new mathematical method to predict groundwater quality in pumping wells.
    Kooten, J.J.A. van; Grasman, J. ; Gee, M. de - \ 1995
    Acta Universitatis Carolinae, Geologica 39 (1995). - p. 243 - 254.
    analogen - watervoerende lagen - grondwaterwinning - grondwaterverontreiniging - horizontale bronnen - hydrologie - modellen - verontreinigingsbeheersing - bescherming - waterkwaliteit - analogues - aquifers - groundwater extraction - groundwater pollution - horizontal wells - hydrology - models - pollution control - protection - water quality
    Eco-hydrologische systeembeschrijving van het landgoed "De Wildenborch"
    Jansen, P.C. ; Kemmers, R.H. ; Mekkink, P. - \ 1994
    Wageningen : DLO-Staring Centrum (Rapport / DLO-Staring Centrum 296) - 125
    ecologie - hydrologie - bodemkarteringen - kaarten - watervoerende lagen - tuinen - parken - landgoederen - particulier eigendom - nederland - ecohydrologie - gelderland - achterhoek - ecology - hydrology - soil surveys - maps - aquifers - gardens - parks - estates - private ownership - netherlands - ecohydrology - gelderland - achterhoek
    Bodemkundig - hydrologisch onderzoek in de omgeving van de winplaats Breehei : de bodemgesteldheid en de huidige hydrologische situatie
    Stoffelsen, G.H. - \ 1994
    Wageningen : DLO-Staring Centrum (Rapport / DLO-Staring Centrum 326) - 68
    watervoerende lagen - grondwaterwinning - grondwaterstroming - horizontale bronnen - kaarten - modellen - regulatie - bodemkarteringen - bodemwater - nederland - waterstand - limburg - aquifers - groundwater extraction - groundwater flow - horizontal wells - maps - models - regulation - soil surveys - soil water - netherlands - water level - limburg
    Elektromagnetische metingen voor het bepalen van de diepte tot hydrologisch slecht doorlatende lagen : een statistische en ruimtelijke analyse van hydrologisch slecht doorlatende bodemlagen, gebruikmakend van niet - destructieve elektromagnetische meetmethoden
    Gaast, J.W.J. van der; Bolhuis, M. van - \ 1994
    Wageningen : DLO-Staring Centrum (Rapport / DLO-Staring Centrum 321)
    watervoerende lagen - elektrische geleiding - elektrische eigenschappen - hydraulisch geleidingsvermogen - infiltratie - magnetische eigenschappen - permeabiliteit - gesteenten - kwel - bodem - bodemprofielen - nederland - niet-destructief testen - drenthe - gelderland - pompproeven - aquifers - electrical conductance - electrical properties - hydraulic conductivity - infiltration - magnetic properties - permeability - rocks - seepage - soil - soil profiles - netherlands - nondestructive testing - drenthe - gelderland - pumping tests
    Stikstofverliezen door beweiding.
    Oomen, G.J.M. ; Baars, T. ; Dongen, M. van - \ 1994
    Ekoland 14 (1994)2. - ISSN 0926-9142 - p. 14 - 15.
    alternatieve landbouw - watervoerende lagen - milieu - graslanden - grondwater - uitspoelen - stikstof - biologische landbouw - bodem - alternative farming - aquifers - environment - grasslands - groundwater - leaching - nitrogen - organic farming - soil
    Relationships between nitrogen production in continuous grassland and grass-clover leys with nitrogen uptake by cattle and nitrogen leaching are described. Consequenses for farm management which limits leaching are discussed
    Verslag van de excursie hydrogeologie naar Engeland, van 20 tot en met 26 september 1992
    Tiemensma, H.A. - \ 1993
    Wageningen : Landbouwuniversiteit Wageningen (Rapport / Landbouwuniversiteit, Vakgroep Waterhuishouding 39) - 63
    watervoerende lagen - engeland - onderzoek - aquifers - england - research
    Biogeochemical aspects of aquifer thermal energy storage
    Brons, H.J. - \ 1992
    Agricultural University. Promotor(en): A.J.B. Zehnder. - S.l. : Brons - 127
    watervoerende lagen - geothermische energie - energie - opslag - grondwater - eigenschappen - biogeochemie - aquifers - geothermal energy - energy - storage - groundwater - properties - biogeochemistry

    During the process of aquifer thermal energy storage the in situ temperature of the groundwater- sediment system may fluctuate significantly. As a result the groundwater characteristics can be considerably affected by a variety of chemical, biogeochemical and microbiological reactions. The interplay of these reactions may have a negative influence on the operational performance of ATES-systems. The objective of this thesis was to investigate bacterial clogging processes and the biogeochemical aspects of carbonate and iron precipitation in aquifer material obtained from ATES test facilities.

    In the General Introduction presented in Chapter 1 the principle of aquifer thermal energy storage is briefly outlined first. This is followed by more detailed information on the thermodynamics of biogeochemical reactions and the conceivable changes in groundwater characteristics during aquifer thermal energy storage. Chapter 2 reports on some microbiological aspects of well clogging during aquifer thermal energy storage. In column experiments well clogging was simulated using aquifer material from a heat storage site and synthetic groundwater. The well clogging potential of oxic and anoxic column effluents was studied at 10° and 30°C using a hollow fiber membrane from which slime depositions were recovered. Only under oxic conditions a slight increase in slime deposition was observed after a temperature rise from 10° to 30°C. No significant difference in bacterial plate counts was measured in oxic and anoxic column effluents, despite the increase in dissolved organic material concentrations at elevated temperatures. This organic material was mobilized from the soil particular organic carbon fraction. The biologically available organic carbon concentration was less than 1% of the dissolved organic carbon concentration, which was not enough to allow excessive bacterial growth or slime formation. Chapter 3 reports on the thermal mobilization of dissolved organic carbon and the concomitant carbon dioxide production in aquifer material from a heat storage site. These processes have been quantified aerobically and anaerobically within a temperature range of 4° to 95°C in sediment samples containing either quartz-rich coarse sand or peaty clay. At temperatures above 450C dissolved organic carbon compounds, including fulvic acids, were mobilized from both sediments resulting in a substantial increase in the chemical oxygen demand of the water phase. Complexation of calcium and magnesium by fulvic acids resulted in the super -saturation of the water phase with regard to calcite and dolomite and thus prevented the precipitation of these carbonates. The highest rates of carbon dioxide release were measured during the first four days of incubation. Aerobically, the maximum rate Of C0 2 production varied between 35 and 800 (sand) or 15 and 150 (peaty clay) μmol C0 2 per gram volatile solids per day. Anaerobically, the rates were 25 and 500 (sand) or 10 and 110 (peaty clay) μmol C0 2 per gram volatile solids per day. At temperatures above 55°C, C0 2 was produced purely chemically. Chapter 4 deals with ferric iron precipitation in anaerobic Tris-HCl buffered seawater. In these incubations,40 mM lactate was rapidly dissimilated to acetate by sulphate reducing bacteria after a lag period of three days. In presence of added nitrate or ferric iron (both 1 mM) or a combination of both, the initial lactate consumption rate was slowed down and sulphate reduction started after four days at a similar rate as was observed in the absence of nitrate and ferric iron. Nitrate in combination with ferrous iron totally inhibited sulphate reduction. Some lactate was initially oxidized, but its concentration did not change after day six of incubation. In these incubations ferrous iron was oxidized chemically to ferric iron with a concomitant reduction of nitrite to nitric oxide. In this so-called chemodenitrification process, nitrite was formed biologically from nitrate with lactate as a reductant. In Chapter 5 chemodenitrification was studied in details with E.coliE4as a model bacterium. Both, L-lactate-driven nitrate and ferric iron reduction were investigated. Ferric iron reduction in E.coliE4was found to be constitutive. Contrary to nitrate, ferric iron could not be used as an electron acceptor for growth. Ferric iron reductase activity of 9 nmol Fe -1protein.min -1could not be inhibited by well known inhibitors of the E.coli respiratory chain. Active cells and the presence of L-lactate were required for ferric iron reduction. The L-lactate-driven nitrate respiration in E.coliE4 leading to the production of nitrite, was reduced to about 20% of its maximum activity with 5 mM ferric iron, or to about 50% in presence of 5 mM ferrous iron. The inhibition was caused by nitric oxide formed by a spontaneous chemical reduction of nitrite by ferrous iron. Nitric oxide was further chemically reduced by ferrous iron to nitrous oxide. With electron paramagnetic resonance spectroscopy, the presence of a free ferro-nitrosyl complex was shown. In presence of ferrous or ferric iron and L-lactate, nitrate was anaerobically converted to nitric oxide and nitrous oxide by the combined action of E.coli E4 and spontaneous chemical reduction reactions. Chapter 6 reports on aerobic reduction of nitrate to ammonium in E.coli grown in continuous cultures, a novel feature of E.coli Nitrate and nitrite was reduced by E.coli E4 in a L-lactate (5 mM) limited chemostat culture at dissolved oxygen concentrations corresponding to 90 - 100% air saturation. Nitrate reductase and nitrite reductase activity was regulated by the growth rate, oxygen and nitrate concentrations. At a low growth rate (0.11 h -1) the measured nitrate and nitrite reductase activities were 200 and 250 -1protein.min -1, respectively. At a high growth rate (0.55 h -1both enzyme activities were considerably lower (25 and 12 -1protein.min -1). The steady state nitrite concentration in the chemostat was controlled by the combined action of the nitrate and nitrite reductase. Both enzyme activities were inversely proportional to the growth rate. The nitrite reductase activity decreased faster with the growth rate than the nitrate reductase. The chemostat biomass concentration of E.coli E4, with ammonium either solely or combined with nitrate as a source of nitrogen, remained constant throughout all growth rates and was not affected by nitrite concentrations. Contrary to batch, E.coli E4 was able to grow on nitrate as the sole source of nitrogen. When cultivated with nitrate as the sole source of nitrogen the chemostat biomass concentration is determined by the combined activities of nitrate and nitrite reductase and hence, inversely proportional to growth rate.

    Gevolgen van de aanleg van de rondweg S-25 bij Veenendaal en daarmee verband houdende ingrepen voor de waterhuishouding van Hel en Blauwe Hel.
    Schaaf, S. van der - \ 1991
    Wageningen : Landbouwuniversiteit Wageningen (Rapport / Landbouwuniversiteit, Vakgroep Hydrologie, Bodemnatuurkunde en Hydraulica 15) - 30
    watervoerende lagen - regulatie - wegenbouw - wegen - kwel - nederland - natuurreservaten - gelderse vallei - waterstand - aquifers - regulation - road construction - roads - seepage - netherlands - nature reserves - gelderse vallei - water level
    Analysis and evaluation of pumping test data
    Kruseman, G.P. ; Ridder, N.A. de; Verweij, J.M. - \ 1990
    Wageningen : I.L.R.I. (Publication / International Institute for Land Reclamation and Improvement 47) - ISBN 9789070754204 - 377
    watervoerende lagen - grondwaterstroming - permeabiliteit - gesteenten - pompproeven - aquifers - groundwater flow - permeability - rocks - pumping tests
    Landschapsecologische kartering Nederland : grondwaterrelaties : toelichting bij het databestand "grondwaterrelaties" van het LKN-project
    Klijn, F. - \ 1989
    Leiden etc. : Centrum voor Milieukunde [etc.] (CML-mededelingen 51)
    watervoerende lagen - milieu - geografie - grondwaterstroming - landschap - landschapsecologie - cartografie - kaarten - modellen - nederland - kwel - karteren - aquifers - environment - geography - groundwater flow - landscape - landscape ecology - mapping - maps - models - netherlands - seepage - surveying
    SATEM : Selected Aquifer Test Evaluation Methods : a microcomputer program
    Boonstra, J. - \ 1989
    Wageningen : ILRI (Publication / ILRI 48) - ISBN 9789070754198 - 80
    analogen - watervoerende lagen - hydrologie - modellen - permeabiliteit - gesteenten - pompproeven - analogues - aquifers - hydrology - models - permeability - rocks - pumping tests
    Mapping evaporation from playa's in the Western Desert : approach and practical examples
    Abd El Karim, M.H. - \ 1989
    Wageningen : ICW (ICW nota 1972) - 39
    toepassingen - watervoerende lagen - woestijnen - egypte - evaporatie - hydrologie - remote sensing - aride klimaatzones - applications - aquifers - deserts - egypt - evaporation - hydrology - remote sensing - arid zones
    New empirical aspects of the Bowen-ratio energy balance method : a study of evaporation losses in arid regions
    Bastiaanssen, W.G.M. - \ 1988
    Wageningen : ICW (ICW note 1914) - 41
    watervoerende lagen - woestijnen - energiebalans - evapotranspiratie - hydrologie - methodologie - sahel - aride klimaatzones - aquifers - deserts - energy balance - evapotranspiration - hydrology - methodology - sahel - arid zones
    Samenvatting van geohydrologische inventarisaties uitgevoerd in of nabij de Onner- en Oostpolder in de gemeente Haren, Groningen
    Bakel, P.J.T. van - \ 1987
    Wageningen : ICW (ICW nota 1806) - 29
    grondwater - hydrologie - eigenschappen - rivieren - waterlopen - kanalen - water - oppervlaktewater - waterverontreiniging - waterkwaliteit - watervoerende lagen - kwel - grondwaterwinning - horizontale bronnen - natuurbescherming - herstel - beleid - bedrijfsvoering - nederland - geohydrologie - hydrogeologie - groningen - groundwater - hydrology - properties - rivers - streams - canals - water - surface water - water pollution - water quality - aquifers - seepage - groundwater extraction - horizontal wells - nature conservation - rehabilitation - policy - management - netherlands - geohydrology - hydrogeology - groningen
    Geohydrologie Onnerpolder
    Literatuur - vooronderzoek met betrekking tot het gebruik van bomen en heesters als indicatoren en accumulatoren voor effecten ten gevolge van luchtverontreiniging
    Floor, H. ; Hasper, G.A. - \ 1987
    Wageningen : Instituut Plantenziektenkundig Onderzoek (IPO rapport 337) - 30
    atmosfeer - milieu - bosbouw - ecologie - bossen - verontreiniging - oogstschade - luchtverontreiniging - aërosolen - samenstelling - stof - luchtkwaliteit - bomen - toxische stoffen - chemie - indicatorplanten - grondwater - watervoerende lagen - literatuuroverzichten - chemische factoren - atmosphere - environment - forestry - ecology - forests - pollution - crop damage - air pollution - aerosols - composition - dust - air quality - trees - toxic substances - chemistry - indicator plants - groundwater - aquifers - literature reviews - chemical factors
    The nitrate conflict between municipal water supply and agriculture the nimwag model
    Rijtema, P.E. ; Hoeijmakers, T.J. ; Kroes, J.G. - \ 1987
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1423) - 37
    grondwaterstroming - watervoorziening - putten - watervoerende lagen - nitrificatie - denitrificatie - mest - infiltratie - modellen - groundwater flow - water supply - wells - aquifers - nitrification - denitrification - manures - infiltration - models
    This description of the NIMWAG model has the same sequence as the computer program. The NIMWAG model calculates N03-N concentrations in the water extracted by a deep well. The model has been made operationel to execute calculations for 166 extraction areas. For each extraction area calculations have been made for 16 different fertilization alternatives. The model can be divided into 3 parts: a part with hydrological calculations, a part with fertilization calculations and a part to calculate the N03-N concentrations. The hydrological part is explained and calculates the spread of the feed in the extraction area and the residence times of the infiltrating precipitation excess. The fertilization level is calculated in dependence to the landuse in the extraction area and to the chosen fertilization alternative. The calculations of N03-N loads in the groundwater caused by the inflow of nitrate into the saturated zone and the denitrification in the saturated zone are explained.
    Reisverslag van een bezoek aan IJsland
    Pomper, A.B. - \ 1986
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1731) - 37
    watervoerende lagen - exploratie - geologie - geomorfologie - geothermische energie - methodologie - tektoniek - vulkanische activiteit - ijsland - aquifers - exploration - geology - geomorphology - geothermal energy - methodology - tectonics - volcanic activity - iceland
    Beknopt verslag van het symposium "water-rock interaction 5", welke in Reykjavik gehouden werd (augustus 1986). Daarnaast is tijdens veldonderzoek aandacht besteed aan vulkanische verschijnselen en geomorfologische gevolgen
    Groundwater losses by evaporation from the Nubian aquifer, Egypt : project document, based on a mission to Cairo, 25 June to 7 July, 1985
    Menenti, M. - \ 1985
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 1632) - 16
    watervoerende lagen - egypte - evaporatie - land - oppervlakten - aquifers - egypt - evaporation - land - surfaces
    Geohydrologisch onderzoek in de omgeving van Herkenbosch
    Wit, K.E. ; v Rees Vellinga, E. ; Wijnsma, M. - \ 1985
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1624) - 10
    watervoerende lagen - grondwaterstroming - putten - grondwaterkwaliteit - midden-limburg - aquifers - groundwater flow - wells - groundwater quality - midden-limburg
    Studie naar de geohydrologische en hydrochemische geaardheid van het gebied Herkenbosch-Vlodorp. Het betrokken gebied ligt dicht bij de grens tussen twee belangrijke tectonische eenheden, namelijk de Centrale Slenk en de Deelhorst. Deze grens wordt gevormd door de Peelrandbreuk die juist ten oosten van Herkenbosch loopt, waardoor het gebied grotendeels in de Slenk ligt. De Peelhorst is een relatief sterk gerezen blok ten oosten van de Peelrandbreuk. Hij is in het veld op verschillende plaatsen te herkennen als een hoge rug die van zuidoost naar noordwest verloopt.
    Lithologische verschijnselen van hydrologisch belang in de ondergrond langs de Zuid-Willemsvaart tussen de sluizen nrs 9 en 10
    Rees Vellinga, E. van - \ 1985
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1606) - 5
    watervoerende lagen - kanalen - ondergrond - binnenwaterwegen - schepen - transport - noord-brabant - aquifers - canals - subsoil - inland waterways - ships - transport - noord-brabant
    Voor het voorspellen van de invloed die de verbredingsen verdiepingswerkzaamheden aan de Zuid-Willemsvaart zal hebben op de directe omgeving van dat kanaal, is het van het grootste belang, goed te zijn geinformeerd over de eigenschappen van de ondergrond. Vooral het gedrag van de grondwaterstromingen in het 'afdekkend pakket' zal bepalend zijn voor de mate van beinvloeding door het kanaal van de omliggende gronden.
    Bepaling van de geohydrologische bodemconstanten in de 'Deurnsche Peel' door middel van pompproef N170
    Beest, J.G. te - \ 1984
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 1538) - 18
    watervoerende lagen - permeabiliteit - gesteenten - nederland - noord-brabant - pompproeven - de peel - aquifers - permeability - rocks - netherlands - noord-brabant - pumping tests - de peel
    Kleimineralogische samenstelling van Nederlandse aquifers
    Breeuwsma, A. ; Zwijnen, R. - \ 1984
    Wageningen : STIBOKA (Rapport / Stichting voor Bodemkartering no. 1816) - 11
    watervoerende lagen - klei - kleimineralen - kaolien - kaoliniet - löss - gesteenten - sediment - leistenen - aquifers - clay - clay minerals - kaolin - kaolinite - loess - rocks - sediment - slates
    Enige resultaten van een geohydrologisch onderzoek in het zuidelijk Peelgebied
    Rees Vellinga, E. van; Broertjes, J.P. - \ 1984
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1590) - 17
    watervoerende lagen - permeabiliteit - nederland - de peel - pompproeven - aquifers - permeability - maps - de peel - pumping tests
    In het zuidelijk Peelgebied wordt door een multidisciplinaire projectgroep een onderzoek verricht tot ontwikkeling van een procedure waarmee alternatieven voor het beheer van grond- en oppervlaktewater kunnen worden geanalyseerd en geëvalueerd, zowel met betrekking tot de waterkwaliteit als de -kwantiteit, in regio's waar landbouw, natuur en openbare watervoorziening belangrijke en dikwijls tegengestelde belangen hebben.
    Hydrologische bodemconstanten verkregen uit een pompproef in de omgeving van Berlicum
    Wit, K.E. ; Beest, J.G. te - \ 1984
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1551) - 12
    watervoerende lagen - permeabiliteit - gesteenten - nederland - noord-brabant - pompproeven - aquifers - permeability - rocks - netherlands - noord-brabant - pumping tests
    Geohydrologische omstandigheden in de omgeving van het toekomstig relatienotagebied Het Limmer Die (ruilverkaveling 'Limmen - Heiloo', N.H.)
    Rees Vellinga, E. van - \ 1983
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1468) - 6
    watervoerende lagen - kwel - peilbeheer - noord-holland - kennemerland - natuurgebieden - aquifers - seepage - water level management - noord-holland - kennemerland - natural areas
    Geohydrologische situatie van een drietal plaatsen in het ruilverkavelingsgebied 'Limmen-Heiloo'. Het betreft hier Het Die, het Limmerveentje en de eendenkooi direct ten noordwesten van Uitgeest. Dit, om te berekenen, welke gevolgen een peilverlaging in de omringende landbouwgebieden op de hydrologie van de betrokken toekomstige relatienotagebiedjes zal hebben.
    Surface water and groundwater in the basin of the Gulp Creek- some major characteristics
    Nota, D.J.G. ; Bakker, A.M.G. - \ 1983
    Netherlands journal of geosciences 62 (1983). - ISSN 0016-7746 - p. 511 - 517.
    watervoerende lagen - chemische eigenschappen - water - zuid-limburg - aquifers - chemical properties - water - zuid-limburg
    Landschapsecologische relaties via het grondwater op nationaal en regionaal niveau
    Roelofs, H.J. ; Beukeboom, T.J. ; Ebregt, A. - \ 1982
    Wageningen : De Dorschkamp (Rapport / Rijksinstituut voor Onderzoek in de Bos- en Landschapsbouw "De Dorschkamp" no. 317) - 122
    watervoerende lagen - landschap - landschapsecologie - ecologie - biogeografie - hydrobiologie - nederland - ecohydrologie - aquifers - landscape - landscape ecology - ecology - biogeography - hydrobiology - netherlands - ecohydrology
    Werden in het vorige rapport (De Dorschkamp, rapport nr. 317) met name de fysische, chemische en biotische hoedanigheden van het Nederlandse grondwater behandeld, in dit rapport worden deze gegevens in verband gebracht met de landelijke milieukartering
    Bodemconstanten in de omgeving van de Zuid-Willemsvaart tussen 's Hertogenbosch en Donk
    Rees Vellinga, R. van; Witt, H. ; Wit, K.E. - \ 1982
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1379) - 11
    watervoerende lagen - permeabiliteit - noord-brabant - pompproeven - aquifers - permeability - noord-brabant - pumping tests
    Door de Directie Noord-Brabant van de Rijkswaterstaat zijn plannen ontworpen ter verbetering van de Zuid-Willemsvaart. Het betreft hier voornamelijk verbreding en verdieping van het kanaalprofiel, terwijl de oude sluizen zullen worden vervangen door een kleiner aantal nieuwe sluizen. Deze maatregelen zullen hun invloed uitoefenen op het grondwaterregime in de omgeving van het kanaal met als gevolg dat daar schade kan optreden voor landbouw, natuurterreinen en bebouwing. Ten behoeve van het geohydrologisch onderzoek dat de grootte van de peilveranderingen en de daaruit voortvloeiende schade moet voorspellen, wordt in deze nota verslag uitgebracht van de onderzoekingen die zich speciaal hebben gericht op het aspect van het doorlaatvermogen (kD) in de watervoerende pakketten in de ondergrond, en de weerstand (c) tegen grondwaterstroming in de onregelmatig voorkomende kleilagen.
    Numerical modelling of groundwater basins : a user-oriented manual
    Boonstra, J. ; Ridder, N.A. de - \ 1981
    Wageningen : I.L.R.I. (Publication International Institute for Land Reclamation and Improvement no. 29) - ISBN 9789070260699 - 226
    watervoerende lagen - waterkwaliteit - grondwater - waterbeheer - hydrologie - modellen - analogen - aquifers - water quality - groundwater - water management - hydrology - models - analogues
    Toename en afname door grondwaterstroming van chloride, stikstof en fosfaat in de ondergrond van Hollands Noorderkwartier
    Witt, H. ; Rees Vellinga, E. van; Wit, K.E. - \ 1981
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 1285) - 14
    watervoerende lagen - anorganische verbindingen - eigenschappen - water - nederland - noord-holland - aquifers - inorganic compounds - properties - water - netherlands - noord-holland
    Hydrochemisch onderzoek van Noord-Holland
    Goor, L. van - \ 1981
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 1286) - 24
    watervoerende lagen - nederland - chemische eigenschappen - noord-holland - aquifers - netherlands - chemical properties - noord-holland
    De geohydrologische opbouw van het proefgebied de Monden in het waterschap "De Veenmarken"
    Pomper, A.B. - \ 1981
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1316) - 36
    watervoerende lagen - grondwater - hydrologie - permeabiliteit - drenthe - geohydrologie - pompproeven - aquifers - groundwater - hydrology - permeability - drenthe - geohydrology - pumping tests
    Inventarisatie is uitgevoerd naar de opbouw van de ondergrond in het Waterschap 'De Veenmarken'. Het uiteindelijke doel was het samenstellen van kaarten van het verloop van de hydrologische grootheden van de ondergrond.
    Vertikale weerstand van het afdekkend pakket in Noord-Holland
    Wijnsma, M. - \ 1979
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 1162) - 9
    watervoerende lagen - geohydrologie - noord-holland - aquifers - geohydrology - noord-holland
    In het kader van een onderzoek naar de waterkwaliteit in Noord- Holland is een geo-hydrologisch onderzoek uitgevoerd. Een onderdeel van dit onderzoek vormde de bepaling van de vertikale weerstand of c-waarde van het afdekkend pakket.
    De geologische en geohydrologische opbouw van Noord-Holland benoorden het Noordzeekanaal
    Pomper, A.B. - \ 1979
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 1135) - 74
    geologie - grondwater - hydrologie - watervoerende lagen - geohydrologie - noord-holland - pleistoceen - geology - groundwater - hydrology - aquifers - geohydrology - noord-holland - pleistocene
    Beschreven worden de bestaande geologische lagen binnen het Pleistoceen (zoals Formatie van Maassluis, Harderwijk, Peelo etc.).
    Een pompproef te Junne (Gem. Ommen)
    Pomper, A.B. - \ 1976
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 925) - 29
    watervoerende lagen - permeabiliteit - geohydrologie - pompproeven - overijssel - aquifers - permeability - geohydrology - pumping tests - overijssel
    In het kader van de werkzaamheden van de Coördinatiegroep Vechtstreek, welke werd ingesteld door de Stuurgroep Coördinatie Geohydrologisch Onderzoek in Nederland, moest een pompproef worden gehouden in het gebied ten oosten van Ommen. Het ICW zou deze pompproef verzorgen. Aanvankelijk werd hiervoor een locatie gekozen in het gemeentelijk bos ten zuiden van het buurtschap Hoogengraven, waarvoor door het ICW de boring E 62 werd uitgevoerd. De opbouw van het profiel was echter zodanig dat het uitvoeren van een boring tot de gewenste diepte van 90 meter met de ICW boorinstallatie onmogelijk bleek te zijn. Op verzoek van de Waterleiding Maatschappij Overijssel (WMO) te Zwolle werd nu een pompproef gehouden in het buurtschap Junne.
    Enkele resultaten van een hydrogeologisch onderzoek in het stroomgebied van de Luntersche Beek
    Rees Vellinga, E. van - \ 1975
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 853) - 11
    watervoerende lagen - hydrogeologie - gelderse vallei - aquifers - hydrogeology - gelderse vallei
    Analysis y evaluacion de los datos de ensayos por bombeo
    Kruseman, G.P. ; Ridder, N.A. de - \ 1975
    Wageningen : ILRI (Boletin / International Institute for Land Reclamation 11s) - 212
    watervoerende lagen - grondwaterstroming - permeabiliteit - gesteenten - pompproeven - aquifers - groundwater flow - permeability - rocks - pumping tests
    Vertikale weerstand van het afdekkend pakket in Midden-West Nederland
    Wit, K.E. - \ 1975
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 879) - 120
    watervoerende lagen - grondwaterverontreiniging - nederland - permeabiliteit - verontreinigingsbeheersing - bescherming - gesteenten - waterkwaliteit - pompproeven - aquifers - groundwater pollution - netherlands - permeability - pollution control - protection - rocks - water quality - pumping tests
    Interpretation et discussion des pompages d'essai
    Kruseman, G.P. ; Ridder, N.A. de - \ 1974
    Wageningen : ILRI (Bulletin / International Institute for Land Reclamation and Improvement 11/F) - 213
    watervoerende lagen - grondwaterstroming - permeabiliteit - gesteenten - pompproeven - aquifers - groundwater flow - permeability - rocks - pumping tests
    Een rekenschema ten behoeve van de berekening van de grondwaterstand en enige termen van de waterbalans bij waterwinning door middel van een diepe put met het filter in een enkele watervoerende laag en bij aanwezigheid van een vrije grondwaterspiegel
    Kouwe, J.J. - \ 1974
    Wageningen : Instituut voor Cultuurtechniek en Waterhuishouding (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 808) - 45
    grondwaterstand - waterwinning - watervoerende lagen - berekening - modellen - groundwater level - water catchment - aquifers - calculation - models
    Het voorliggende rapport geeft een beschrijving van enkele rekenschema's die werden ontworpen voor het berekenen van waterstand, onder invloed van de weersomstandigheden wisselende verdamping, afvoer en grondwaterstanden in de omgeving van een wateronttrekking door middel van een diepe put. Aangezien voor de differentiaalvergelijking, zoals weergegeven onder vergelijking (3), waarin dus de termen voor de verdamping, de afvoer en de berging zijn opgenomen, geen exacte oplossing bestaat, diende gebruik te worden gemaakt van de differentierekening.
    Notes on the tertiary and pleistocene geology of East Gelderland, The Netherlands
    Rees Vellinga, E. van; Ridder, N.A. de - \ 1973
    Wageningen : I.L.W.M.R. (Technical bulletin / Institute for land and water management research no. 85) - 19
    watervoerende lagen - nederland - gelderland - achterhoek - hydrogeologie - tertiair - pleistoceen - aquifers - netherlands - gelderland - achterhoek - hydrogeology - tertiary - pleistocene
    Groundwater hydraulics of extensive aquifers
    Edelman, J.H. - \ 1972
    Wageningen : I.L.R.I. (Bulletin / International Institute for Land Reclamation and Improvement no. 13) - 216
    watervoerende lagen - zoet water - grondwaterstroming - grensvlak - zout water - aquifers - fresh water - groundwater flow - interface - saline water
    Buried channel aquifers and present open drainage system of East Gelderland, the Netherlands
    Vries, J.J. de; Rees Vellinga, E. van - \ 1972
    Wageningen : I.C.W. (Verspreide overdrukken / Insituut voor Cultuurtechniek en Waterhuishouding no. 127) - 8
    drainage - sloten - watervoerende lagen - achterhoek - drainage - ditches - aquifers - achterhoek
    In the eastern part of the province of Gelderland, two buried valley systems have been traced. One system is filled with fluvioglacial deposits dating from the Saalian lce Age, the other with preglacial fluvial sediments which are remarkable rich in vulcanic minerals. Both systems have a course which is almost perpendicular to the present drainage system. This change in stream direction is explained by postglacial replacement of the main drainage channel in the area, tectonic movement perpendicular to the old channels, and postglacial filling of the old channels with wind blown sand.
    DE topogragie van het bovenste begrenzingsvlak en de mogelijke samenstelling van de afzettingen van de formatie van kedichem in Midden-West Nederland
    Pomper, A.B. - \ 1972
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 692) - 26
    watervoerende lagen - geologische sedimentatie - hydrogeologie - west-nederland - aquifers - geological sedimentation - hydrogeology - west netherlands
    In verband met de bestudering van de achtergronden van het zoutbezwaar van het oppervlaktewater in Midden-West-Nederland is een diepgaand onderzoek uitgevoerd naar de opbouw van de ondergrond van het gebied. De kennis van de ondergrond is nodig om een berekening van de ondergrondse waterbeweging mogelijk te maken.
    Enkele resultaten van een geohydrologisch onderzoek in Midden-West-Nederland
    Rees Vellinga, E. van - \ 1972
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 679) - 16
    watervoerende lagen - nederland - zuid-holland - aquifers - netherlands - zuid-holland
    De grondwaterstroming naar diepe putten bij twee watervoerende lagen in een concentrisch binnengebied met droge sloten
    Ernst, L.F. - \ 1972
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 660) - 10
    grondwaterstroming - watervoerende lagen - putten - formuleringen - groundwater flow - aquifers - wells - formulations
    Een nadere uitwerking van formules is gegeven, waarbij een stelsel van 3 vergelijkingen werd overgehouden voor grondwaterstroming naar putten bij 2 watervoerende lagen
    Analysis and evaluation of pumping test data
    Kruseman, G.P. ; Ridder, N.A. de - \ 1970
    Wageningen : ILRI (Bulletin / International Institute of Land Reclamation and Improvement no. 11) - 200
    watervoerende lagen - grondwaterstroming - permeabiliteit - gesteenten - pompproeven - aquifers - groundwater flow - permeability - rocks - pumping tests
    A geohydrologic study of East Gelderland : Netherlands
    Ernst, L.F. ; Ridder, N.A. de; Vries, J.J. de - \ 1970
    Wageningen : [s.n.] (Verspreide overdrukken. Instituut voor cultuurtechniek en waterhuishouding no. 115) - 32
    watervoerende lagen - grondwater - hydrologie - nederland - gelderland - geohydrologie - achterhoek - aquifers - groundwater - hydrology - netherlands - gelderland - geohydrology - achterhoek
    Proeve van een kD - waardenkaart van Midden - West - Nederland
    Witt, H. ; Rees Vellinga, E. van - \ 1970
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 573) - 10
    watervoerende lagen - permeabiliteit - kwel - pompproeven - geohydrologie - west-nederland - aquifers - permeability - seepage - pumping tests - geohydrology - west netherlands
    Een van de belangrijkste oorzaken van verzilting in Midden-West-Nederland is de kwel. Hierdoor wordt het oppervlaktewater van de polders belast met zout uit het diepere grondwater. In dit verband is het van belang de grootte en de variaties in het doorlatend vermogen van de ondergrond te kennen.
    De betekenis van de oud-pleistocene en oudere formaties voor de hydrologie van Midden Westelijk Nederland
    Pomper, A.B. - \ 1969
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 516) - 13
    watervoerende lagen - permeabiliteit - pompproeven - west-nederland - aquifers - permeability - pumping tests - west netherlands
    De invloed van bos in Nederland op de afvoer van beekgebieden
    Bon, J. - \ 1969
    Wageningen : [s.n.] (Verspreide overdrukken. Instituut voor cultuurtechniek en waterhuishouding no. 75) - 11
    watervoerende lagen - afvoer - bossen - grondwaterstand - hydrologie - infiltratie - nederland - oppervlakkige afvoer - vegetatie - watererosie - aquifers - discharge - forests - groundwater level - hydrology - infiltration - netherlands - runoff - vegetation - water erosion
    De geo-hydrologische gesteldheid van de Achterhoek en de consequenties van toenemende grondwaterwinning
    Vries, J.J. de - \ 1967
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 390) - 18
    watervoerende lagen - grondwaterwinning - horizontale bronnen - nederland - gelderland - achterhoek - aquifers - groundwater extraction - horizontal wells - netherlands - gelderland - achterhoek
    Apparatus for measuring hydraulic conductivity of undisturbed soil samples
    Wit, K.E. - \ 1967
    Wageningen : [s.n.] (Technical bulletin / Institute for land and water management research no. 52) - 12
    bodem - permeabiliteit - watervoerende lagen - gesteenten - mechanica - meting - massa - dichtheid - instrumentatie - elektriciteit - pompproeven - soil - permeability - aquifers - rocks - mechanics - measurement - mass - density - instrumentation - electricity - pumping tests
    Afvoer en berging in verband met beekverbetering, toegelicht aan het stroomgebied van de Lunterse beek
    Bon, J. - \ 1967
    Wageningen : Pudoc, Centrum voor Landbouwpublikaties en Landbouwdocumentatie (Mededeling / Instituut voor cultuurtechniek en waterhuishouding no. 107) - 94
    watervoerende lagen - doorstroommeters - grondwaterstroming - overlaten - rivierafvoer - waterwegen - stuwen - gelderse vallei - aquifers - flow meters - groundwater flow - spillways - stream flow - waterways - weirs - gelderse vallei
    Hydrologische studie onderdeel Gelderse Vallei
    De pompproeven M168 en M174, gelegen ten zuid-oosten van Zelhem
    Vries, J.J. de - \ 1967
    Wageningen : ICW (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 377) - 18
    grondwaterstroming - pompproeven - grondwaterstand - watervoerende lagen - achterhoek - groundwater flow - pumping tests - groundwater level - aquifers - achterhoek
    In september en oktober 1966 zijn ten zuidoosten van Zelhem door het Instituut voor Cultuurtechniek en Waterhuishouding 2 pompproeven, M168 en M174, uitgevoerd. Om een indruk te krijgen van de beweging van de grondwaterspiegel onder invloed van het seizoen tijdens de pompproeven, zijn in de periode van eind oktober tot en met begin november grondwaterstandswaarnemingen gedaan in de waarnemingsputten M168, M174 en M152, welke laatste is gelegen op ongeveer 3 km van het onderzochte gebied.
    Pompproef M219 te Vierakker
    Vries, J.J. de - \ 1967
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 405) - 6
    pompproeven - grondwaterstand - monitoring - watervoerende lagen - geohydrologie - achterhoek - gelderland - pumping tests - groundwater level - monitoring - aquifers - geohydrology - achterhoek - gelderland
    Op 17 en 18 april 1967 is ten behoeve van geo-hydrologisch onderzoek in de Achterhoek een pompproef uitgevoerd in de omgeving van Vierakker. Om een indruk te verkrijgen van de beweging van de grondwaterspiegel onder invloed van het seizoen tijdens de pompproef werden ook grondwaterstandswaarnemingen verricht.
    Analysis of the pumping test "De Vennebulten" near Varsseveld
    Ridder, N.A. de - \ 1966
    Wageningen : Instituut voor Cultuurtechniek en Waterhuishouding (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 335) - 5
    watervoerende lagen - grondwaterwinning - achterhoek - aquifers - groundwater extraction - achterhoek
    The pumping test 'De Vennebulten' which will be described in this report forms part of a large-scale groundwater exploration in the 'Achterhoek' region, province of Gelderland. In greater parts of this region, covering some 100 000 ha, groundwater is pumped from Young Pleistocene formations underlain by almost impervious layers of Tertiary clay and clay-bearing fine sands.
    Pompproef M163 tussen Dinxperlo en Aalten
    Vries, J.J. de - \ 1966
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 360) - 9
    pompproeven - grondwaterstand - monitoring - bodemtypen (lithologisch) - watervoerende lagen - geohydrologie - achterhoek - gelderland - pumping tests - groundwater level - monitoring - soil types (lithological) - aquifers - geohydrology - achterhoek - gelderland
    Op 21 en 22 september 1966 werd door het I.C.W. in het kader van het geohydrologisch onderzoek in de Achterhoek een pompproef gehouden in het gebied tussen Dinxperlo en Aalten. De boringen vonden plaats in een pre-glaciaal dal, dat zich tot zeer diep in het Tertiair heeft ingesneden. Met behulp van boringen en geo-elektrisch onderzoek kon dit dal worden gevolgd van Dinxperlo tot aan Vreden in Duitsland. Vanaf 9 september zijn dagelijks in de peilbuizen grondwaterstandswaarnemingen gedaan.
    Pompproef M165 ten Z.O. van Silvolde
    Vries, J.J. de - \ 1966
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 357) - 9
    pompproeven - grondwaterstand - monitoring - bodemtypen (lithologisch) - watervoerende lagen - geohydrologie - achterhoek - gelderland - pumping tests - groundwater level - monitoring - soil types (lithological) - aquifers - geohydrology - achterhoek - gelderland
    Ten behoeve van het geo-hydrologisch onderzoek in de Gelderse Achterhoek is op 7 en 8 juli 1966 door het I.C.W. een pompproef gehouden in het gebied tussen Silvolde en Dinxperlo. Tevens zijn vanaf 4 juli dagelijks grondwaterstandswaarnemingen gedaan in de verschillende peilbuizen
    De geo-hydrologische gesteldheid van Westerwolde
    Vries, J.J. d - \ 1966
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 363) - 4
    watervoerende lagen - permeabiliteit - gesteenten - nederland - pompproeven - groningen - oost-groningen - aquifers - permeability - rocks - netherlands - pumping tests - groningen - oost-groningen
    Onderzoek naar de opbouw en doorlatendheid van de diepere ondergrond van Westerwolde. Hierbij is gebruik gemaakt van boringen, die vroeger al door het Rijkslandbouwproefstation en Bodemkundig Instituut van Groningen zijn gedaan. ERr is een kD waardenkaart van de bovenste 10 meter gemaakt
    Enkele resultaten van een geologisch onderzoek in de Gelderse Achterhoek ten behoeve van de grondwater exploitatie
    Ridder, N.A. de - \ 1964
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 247) - 17
    watervoerende lagen - waterwinning - hydrogeologie - achterhoek - aquifers - water catchment - hydrogeology - achterhoek
    Door de bijzondere geologische gesteldheid van de Achterhoek is de mogelijkheid tot grondwaterwinning slechts beperkt. Een plan voor uitbreiding voor waterwinning dient gebaseerd te zijn op juiste geohydrologische informatie. Vandaar dit onderzoek.
    Evaluation of some pumping tests from the Konya Basin
    Ridder, N.A. de - \ 1964
    Wageningen : ILRI - 43
    watervoerende lagen - permeabiliteit - gesteenten - turkije - pompproeven - aquifers - permeability - rocks - turkey - pumping tests
    Studies of salt and water movement in the Bol Guini polder : Chad Republic
    Dieleman, P.J. ; Ridder, N.A. de - \ 1964
    Wageningen : ILRI (Bulletin / International Institute for Land Reclamation and Improvement 5) - 40
    watervoerende lagen - tsjaad - verbetering - permeabiliteit - gesteenten - verzilting - natrium - bodem - pompproeven - aquifers - chad - improvement - permeability - rocks - salinization - sodium - soil - pumping tests
    Bepaling van enige hydrologische bodemconstanten in de polder "De Oude Korendijk" : uit metingen in ongeroerde monsters
    Wit, K.E. - \ 1963
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding 189) - 8
    watervoerende lagen - doorlatendheid - kwel - polders - geohydrologie - zuidhollandse eilanden - aquifers - transmittance - seepage - polders - geohydrology - zuidhollandse eilanden
    Ten behoeve van het geo-hydrologisch onderzoek zijn een aantal diepboringen uitgevoerd, enerzijds voor het stellen van peilfilters, anderzijds om gegevens te verkrijgen omtrent de verbreiding en de dikte van watervoerende en slecht doorlatende lagen. In een aantal van deze boringen zijn ongeroerde monsters verzameld, waarin in het laboratorium de doorlatendheid is gemeten. Uit deze gegevens is de verticale weerstand van slecht doorlatende lagen en de kD-waarde van watervoerende lagen berekend.
    Een geologisch profiel langs de Zuid-Willemsvaart
    Ridder, N.A. de - \ 1962
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 155) - 9
    watervoerende lagen - pompproeven - permeabiliteit - doorlatendheid - peilbeheer - kanalen - noord-brabant - aquifers - pumping tests - permeability - transmittance - water level management - canals - noord-brabant
    Ten behoeve van het onderzoek naar de invloed, die een eventuele peilverlaging van de Zuid-Willemsvaart op de grondwaterstanden in de aangrenzende landbouwgronden zal hebben, was een inzicht in de geologische gesteldheid van het kanaaltracé noodzakelijk.
    Resultaten van de bepaling van enige hydrologische bodemconstanten in een infiltratie-proefveld van de ruilverkaveling Steenwijksmoer
    Ridder, N.A. de; Wit, K.E. - \ 1962
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 143) - 11
    watervoerende lagen - permeabiliteit - infiltratie - pompproeven - drenthe - aquifers - permeability - infiltration - pumping tests - drenthe
    Door de Cultuurtechnische Dienst te Assen worden voor een klein terrein in het Ruilverkavelingsgebied "Steenwijksmoer" de mogelijkheden voor infiltratie onderzocht. Do vraag hoeveel water nodig zal zijn om de grondwaterspiegel op het gewenste peil te handhaven, wordt in belangrijke mate bepaald door de geohydrologische gesteldheid van het gebied. De nauwkeurigheid, waarmee de noodzakelijke schematisering van deze geohydrologische toestand wordt uitgevoerd, is bepalend voor do praktische waarde van de mot behulp van stromingsformules uitgevoerde berekeningen.
    The hydrological properties of Deltaic sediments
    Ridder, N.A. de - \ 1961
    Wageningen : I.C.W. (Nota / Instituut voor Cultuurtechniek en Waterhuishouding no. 111) - 12
    watervoerende lagen - geohydrologie - delta's - zuidwest-nederland - aquifers - geohydrology - deltas - south-west netherlands
    This paper deals with the hydrological properties of deltaic sediments. A detailed study was made of the geological history of part of the delta plain of the Rhine and Meuse. Such hydrological properties as thickness of aquifers and semi-permeable layers, transmissibility of the aquifers were determined.
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