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Aquifer
Linked via "cementation"
Transmissivity measures the rate at which water is transmitted through a unit width of the aquifer under a unit hydraulic gradient. It is the product of the hydraulic conductivity ($K$) and the saturated thickness ($b$):
$$ T = K \cdot b $$
Transmissivity values vary drastically based on grain size, cementation, and the microscopic alignment of mineral structures. High…