Deriving pedotransfer functions for soil quartz fraction in southern France from reverse modeling
The quartz fraction in soils is a key parameter of soil thermal conductivity models. Because it is difficult to measure the quartz fraction in soils, this information is usually unavailable. This source of uncertainty impacts the simulation of sensible heat flux, evapotranspiration and land surface...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-12-01
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Series: | SOIL |
Online Access: | http://www.soil-journal.net/2/615/2016/soil-2-615-2016.pdf |