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

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Academic year: 2017

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Figure 1. Location of the 21 SMOSMANIA stations in southern France (see station names in Supplement 1).
Figure 2 shows soil temperature time series in wet con- con-ditions at various soil depths for a station presenting an  in-termediate value of λ sat (Table 2) and of soil texture (see Fig
Table 1. Soil characteristics at 10 cm for the 21 stations of the SMOSMANIA network. Porosity values are derived from Eq
Table 2. Thermal properties of 14 grassland soils in southern France: λ sat , f q and Q retrievals using the λ model (Eqs
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