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andrewzhang

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zhangruicumt: 金币+25, 翻译EPI+1, ★★★很有帮助 2013-08-24 08:36:15

When the pressure of the water source was considerable important, the fine particles in the fault would dissolute, migrate, and lose under the action of continued water erosion, which would increase the size of pores, and form certain enhanced continuous fractures. Thus the water flow transited from the pore-flow into the fissure-flow, resulting in a greater permeability of the fault and a increasing inrush-water amount.

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