• Under the same conditions the maximum water-flow in rock fracture is about 3040 times that in the clay fracture.

    指出粘土裂缝最大水流量要比相同条件基岩裂缝水流量小3040

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  • The water-flow in fracture is not directly proportional to the waterhead.

    裂缝水流量与水位呈正比关系。

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  • The groundwater flow and solute transport is very complex because of the intense variability in rock network fracture. How to simulate the water flow and solute transport is a very important question.

    由于基岩裂隙网络系统具有强烈空间变异性,所以其中地下水流动溶质运移十分复杂,如何模拟这种系统中的地下水流动和溶质运移一直一个重要的问题。

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  • The seepage in fractured rocks was regarded as the fracture network flow. The tracer particles moved as the water flow in the fracture network.

    裂隙岩体渗流视为裂隙网络示踪剂质点裂隙网络运动。

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  • The seepage in fractured rocks was regarded as the fracture network flow. The tracer particles moved as the water flow in the fracture network.

    裂隙岩体渗流视为裂隙网络示踪剂质点裂隙网络运动。

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