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Earth and Space Sciences · 术语表

什么是 Specific discharge; hydraulic conductivity; intrinsic permeability?

又称: specific discharge · hydraulic conductivity · intrinsic permeability

Definition 23.3 University Earth and Space Sciences — Year 3 · 第 23 章 — Hydrogeology

The specific discharge q⃗\vec q is the volume of water crossing unit area of the medium, grains and pores together, per unit time. The hydraulic conductivity KK is the coefficient of Darcy’s law, in m/s\mathrm{m}/\mathrm{s} or m/d\mathrm{m}/\mathrm{d}. The intrinsic permeability of the medium is k=Kμ/(ρg)k = K\mu/(\rho g), in m2\mathrm{m}^{2}: it depends on the medium alone.

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