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断层泥的瞬时力学性质和蠕变特性与含水量关系密切，其力学参数随含水量增加而减少，呈负指数函数关系。界限含水量划分具有很大的意义，某地ｆ２４６断层泥界限含水量为８％～１０％。
The transient mechanical properties and creep characteristics of fault mud are closely related to the water content. The mechanical parameters decrease with the increase of water content, showing a negative exponential function. Boundary moisture content division is of great significance, somewhere f246 fault mud water content limit of 8% to 10%.