Articles | Volume 2, issue 4
Original research article
09 Dec 2016
Original research article |  | 09 Dec 2016

Deriving pedotransfer functions for soil quartz fraction in southern France from reverse modeling

Jean-Christophe Calvet, Noureddine Fritz, Christine Berne, Bruno Piguet, William Maurel, and Catherine Meurey

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Cited articles

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Albergel, C., Calvet, J.-C., de Rosnay, P., Balsamo, G., Wagner, W., Hasenauer, S., Naeimi, V., Martin, E., Bazile, E., Bouyssel, F., and Mahfouf, J.-F.: Cross-evaluation of modelled and remotely sensed surface soil moisture with in situ data in southwestern France, Hydrol. Earth Syst. Sci., 14, 2177–2191,, 2010.
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Short summary
Soil thermal conductivity in wet conditions can be retrieved together with the soil quartz content using a reverse modelling technique based on sub-hourly soil temperature observations at three depths below the soil surface. A pedotransfer function is proposed for quartz, for the considered region in France. Gravels have a major impact on soil thermal conductivity, and omitting the soil organic matter information tends to enhance this impact.