A recording apparatus for measuring thermal conductivity, and some results obtained with it in soil.

Authors

  • R.H.A. van Duin
  • D.A. de Vries

DOI:

https://doi.org/10.18174/njas.v2i3.17840

Abstract

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)

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Published

1954-08-01

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Section

Papers