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Heat-Pulse Method for Soil Water Content Measurement

Influence of the Specific Heat of the Soil Solids

^a Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China 100101
^b Dep. of Agronomy, Iowa State Univ., Ames, IA 50011
^c China Agricultural Univ., Beijing, China 100094

View larger version (14K): [in a new window]   Fig. 1. Heat-pulse water content, , vs gravimetrically determined . The parameter of specific heat of soil solids, cs, was 0.725 kJ kg-1 K-1. The solid lines are the 1:1 lines.

View larger version (14K): [in a new window]   Fig. 2. Heat-pulse water content, , vs gravimetrically determined . The heat-pulse measured specific heat of soil solids, cs, for each soil was used. The solid lines are the 1:1 lines.