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The chapter discusses unsaturated soils and their moisture content, detailing the classification of soil based on saturation levels such as wet, damp, and dry. It explores the implications of soil moisture on chemical partitioning, emphasizing the relationships between air, water, and organic carbon within the soil matrix. Additionally, the chapter outlines methods to measure partition constants and the factors affecting equilibrium in unsaturated conditions.
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9b.pdfClass Notes
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Term: Unsaturated Soil
Definition: Soil that contains both water and air in its pore spaces, where not all pores are filled with water.
Term: Moisture Content Classification
Definition: Soil's moisture is classified as wet (full monolayer coverage), damp (less than one monolayer), or dry (no significant water).
Term: Chemical Partitioning
Definition: The distribution of a chemical between different phases, such as air and water, based on moisture content and saturation.
Term: Partition Constant
Definition: A measure of how a chemical distributes itself between two phases at equilibrium, aiding in predicting chemical behavior in soils.
Term: Henry's Constant
Definition: An equilibrium constant that describes the ratio of a chemical's concentration in the air to its concentration in the water.