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Staff Publications

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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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Record number 404662
Title Nitrogen losses from two grassland soils with different fungal biomass
Author(s) Vries, F.T. de; Groenigen, J.W. van; Hoffland, E.; Bloem, J.
Source Soil Biology and Biochemistry 43 (2011)5. - ISSN 0038-0717 - p. 997 - 1005.
DOI http://dx.doi.org/10.1016/j.soilbio.2011.01.016
Department(s) Soil Science Centre
Chair Soil Biology and Biological Soil Quality
SS - Soil Quality and Nutrients
PE&RC
Publication type Refereed Article in a scientific journal
Publication year 2011
Keyword(s) arbuscular mycorrhizal fungi - organic-matter - microbial communities - carbon sequestration - upland grasslands - cultivated soils - food webs - mineralization - ecosystems - management
Abstract Nitrogen losses from agricultural grasslands cause eutrophication of ground- and surface water and contribute to global warming and atmospheric pollution. It is widely assumed that soils with a higher fungal biomass have lower N losses, but this relationship has never been experimentally confirmed. With the increased interest in soil-based ecosystem services and sustainable management of soils, such a relationship would be relevant for agricultural management. Here we present a first attempt to test this relationship experimentally. We used intact soil columns from two plots from a field experiment that had consistent differences in fungal biomass (68 ± 8 vs. 111 ± 9 µg C g-1) as a result of different fertilizer history (80 vs. 40 kg N ha-1 y-1 as farm yard manure), while other soil properties were very similar. We performed two greenhouse experiments: in the main experiment the columns received either mineral fertilizer N or no N (control). We measured N leaching, N2O emission and denitrification from the columns during 4 weeks, after which we analyzed fungal and bacterial biomass and soil N pools. In the additional 15N experiment we traced added N in leachates, soil, plants and microbial biomass. We found that in the main experiment, N2O emission and denitrification were lower in the high fungal biomass soil, irrespective of the addition of fertilizer N. Higher 15N recovery in the high fungal biomass soil also indicated lower N losses through dentrification. In the main experiment, N leaching after fertilizer addition showed a 3-fold increase compared to the control in low fungal biomass soil (11.9 ± 1.0 and 3.9 ± 1.0 kg N ha-1, respectively), but did not increase in high fungal biomass soil (6.4 ± 0.9 after N addition vs. 4.5 ± 0.8 kg N ha-1 in the control). Thus, in the high fungal biomass soil more N was immobilized. However, the 15N experiment did not confirm these results; N leaching was higher in high fungal biomass soil, even though this soil showed higher immobilization of 15N into microbial biomass. However, only 3% of total 15N was found in the microbial biomass 2 weeks after the mineral fertilization. Most of the recovered 15N was found in plants (approximately 25%) and soil organic matter (approximately 15%), and these amounts did not differ between the high and the low fungal biomass soil. Our main experiment confirmed the assumption of lower N losses in a soil with higher fungal biomass. The additional 15N experiment showed that higher fungal biomass is probably not the direct cause of higher N retention, but rather the result of low nitrogen availability. Both experiments confirmed that higher fungal biomass can be considered as an indicator of higher nitrogen retention in soils
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