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

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Figure

Figure 1. Location of the 21 SMOSMANIA stations in southernFrance (see station names in Supplement 1).
Figure 2. Soil temperature measured in wet conditions at the St-Félix-Lauragais (SFL) station on 23 February 2015 at depths of0.05, 0.10, 0.20 and 0.30 m
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: λsat, fq and Q retrievals using the λ model (Eqs
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