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Earth and Space Sciences · 术语表

什么是 Transmissivity; storativity; specific yield?

又称: transmissivity · storativity · specific yield

Definition 23.6 University Earth and Space Sciences — Year 3 · 第 23 章 — Hydrogeology

The transmissivity of an aquifer of thickness bb is T=KbT = Kb, the flow per unit width under unit gradient, in m2/d\mathrm{m}^{2}/\mathrm{d}. Its storativity (or storage coefficient) SS is the volume of water released per unit area of the aquifer when the head falls by one unit; it is dimensionless. The specific yield SyS_y of a rock is the volume of water that drains from it by gravity per unit volume when the water table falls through it.

A schematic section of the cover of the Varden Hills from west to east, not to scale. The chalk holds an unconfined aquifer below its water table. The Jurassic limestone is recharged where it outcrops and is confined beneath the shale: in the well Varden-3 of the problem, drilled through the shale and open only to the limestone, the water rises to the potentiometric surface, far above the top of the aquifer but below the ground.
A schematic section of the cover of the Varden Hills from west to east, not to scale. The chalk holds an unconfined aquifer below its water table. The Jurassic limestone is recharged where it outcrops and is confined beneath the shale: in the well Varden-3 of the problem, drilled through the shale and open only to the limestone, the water rises to the potentiometric surface, far above the top of the aquifer but below the ground.
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