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subsoil
This term describes the geological transition zone between the organic-rich surface layer and the deeper bedrock. It carries a technical, scientific connotation, typically appearing in contexts of agriculture, civil engineering, and environmental science to describe drainage capacity or structural stability.
As a mass noun referring to a geological stratum, it is predominantly treated as uncountable. When referring to the material itself in a general sense, it does not take a plural form; however, in specific technical reports comparing different types of underlying earth across various sites, a countable usage may occur, though this is rare.
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