Definition
Mineral soils. Soils composed predominantly of minerals.
Quartz. One of the most common constituents of the Earth’s crust, abundant in sandstones, granite, and soils. It is made up of silica (SiO2) having a superior ability to conduct heat.
Thermal conductivity of soils. The bulk property of soils describing their ability to conduct heat. It is measured in Watts per Kelvin per meter (W/K/m).
Introduction
Thermal conductivity of soil solids (λ s) is an essential parameter required by a majority of models in the prediction of soil thermal conductivity (λ). The value of λ s depends strongly on the fraction of quartz (Θ q) in soil solids and its thermal conductivity (λ q), whose value is considerably higher than the remaining soil minerals. For that reason, Θ q is a key parameter for assessing λ s, but data on Θ q is very scarce and often contradictory with soil texture. Quartz (SiO2) occurs mainly in coarse soil fractions (i.e., sands and gravels) as it does not break up...
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Tarnawski, V.R., Momose, T., Leong, W.H., Piper, D.J.W. (2011). Estimation of Quartz Content in Mineral Soils. In: Gliński, J., Horabik, J., Lipiec, J. (eds) Encyclopedia of Agrophysics. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3585-1_130
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