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- W4242116237 abstract "Publisher SummaryThis chapter presents the differential equations for heat transport and the parameters needed to solve them and describes the methods for solving the equations using numerical procedures. All of the physical, chemical, and biological processes that go on in soil are influenced by soil temperature. Biological processes such as the uptake of nutrients and water by roots, the decomposition of organic matter by microbes and the germination of seeds are strongly affected by soil temperature. Rates of some of these processes more than double for each 10°C increase in temperature. In some cases, growth of above-ground plant parts is more closely correlated with soil temperature than with air temperature. Physical processes, such as water movement and soil drying can also be strongly influenced by temperature. For these reasons, most simulations of soil processes require submodels which predict soil temperature. The simplest model for soil temperature would be to assume that it is constant, or that it is equal to a daily, weekly, or monthly mean air temperature. Such a model may be adequate for some purposes, which will be considered in later chapters. More accurate models require analysis of heat flow within the soil and heat exchange at the soil surface to determine soil temperature. The transport or loss of latent heat of either fusion or vaporization, and the movement of soil moisture are important in determining soil temperature." @default.
- W4242116237 created "2022-05-12" @default.
- W4242116237 date "1985-01-01" @default.
- W4242116237 modified "2023-09-30" @default.
- W4242116237 title "Chapter 4 Soil Temperature and Heat Flow" @default.
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- W4242116237 doi "https://doi.org/10.1016/s0166-2481(08)70134-x" @default.
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