Specific Heat Capacity of Soil Solids: Influences of Clay Content, Organic Matter, and Tightly Bound Water

Abstract

The specific heat capacity of soil solids (cs) is a key parameter affecting heat storage and transfer in soils. In soil and geophysical applications,csis often assumed to be a constant with little variations across soils. In this study, we determined the specific heat capacities of nine soils by using differential scanning calorimetry (DSC), evaluated the effects of clay and organic matter (OM) contents on thecsof original and OM‐free soil samples at room temperature, and quantified the changes ofcscaused by the existence of tightly bound water (TBW). On average, the nine mineral soils had acsof 0.750 MJ Mg−1K−1, close to the commonly acceptedcsvalue. However, for the original soils dried at 105°C, clay content did not obviously influence thecsvalue andcsincreased linearly with both OM and TBW contents, indicating that inaccuratecsdata were likely if the changes in the OM fraction in soil solids and adsorbed TBW were ignored. In addition, relatively large values for the specific heat capacity of soil minerals (cm) were observed in fine‐textured soils compared with coarse‐textured soils. Two preliminary functions were developed for estimatingcmandcsfrom the soil's clay and OM contents.Core IdeasSoil specific heat capacity was measured via differential scanning calorimetry.The influences of clay, organic matter (OM), and tightly bound water on specific heat capacity were evaluated quantitatively.A linear relationship was developed between the specific heat of soil minerals dried at 200°C and clay content.The specific heat of soil solids dried at 105°C had a nonlinear relationship with clay and OM contents.