A recording apparatus for measuring thermal conductivity, and some results obtained with it in soil.
DOI:
https://doi.org/10.18174/njas.v2i3.17840Abstract
The automatic apparatus described comprises a number of elements which, placed to various depths at 3-90 cm in field soils, are successively switched on so as to give a straight-line photographic record of the deflections of a galvanometer. The gradient of the line is a measure of thermal conductivity, from which moisture content may indirectly be computed and evapo-transpiration determined by repeated measurements. Results of moisture determinations in a sandy soil under grass cover are reported. The method is well suited for observing moisture changes in lysimeters. (Abstract retrieved from CAB Abstracts by CABI’s permission)Downloads
Published
1954-08-01
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Papers