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• W2411011055 endingPage "1634" @default.
• W2411011055 startingPage "1631" @default.
• W2411011055 abstract "The heat-pulse method measures soil volumetric water content (θ) based on the linear relationship between soil volumetric heat capacity (C) and θ. Previous work suggested that this method was more appropriate for determining change of θ rather than its absolute value. In this study, we demonstrate that the heat-pulse method can give accurate θ estimation when values for the specific heat of the soil solids (cs) are determined using the heat-pulse method. Heat-pulse measurements were performed on packed columns of three soils with a wide range of bulk density (ρb) and θ. When the commonly used cs value (0.725 kJ kg−3 K−1) was used, the heat-pulse method overestimated θ by 0.052 m3 m−3 on average. However, when cs values determined from heat-pulse measurements on oven-dried soil were used, the heat-pulse method provided accurate θ results (−0.006 m3 m−3 average error). Using soil-specific, heat-pulse determined cs values also reduced the average root mean square error (RMSE) in θ for the three soils from 0.061 to 0.039 m3 m−3" @default.
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• W2411011055 date "2003-11-01" @default.
• W2411011055 modified "2023-09-25" @default.
• W2411011055 title "Heat-Pulse Method for Soil Water Content Measurement" @default.
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• W2411011055 doi "https://doi.org/10.2136/sssaj2003.1631" @default.
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