软土地基的土质具有粘性大，透水性差，含水量大，承载力低，沉降量大，土层结构复杂等特点。
The soft soil is featured by big viscosity, bad water permeability, big water content, low bearing capacity, big settlement and complex soil layers.
该含水层的导水性能为各向异性的。
根据矿区具备多处位置、水平不同的生产坑道和含水层富水性弱等实际情况。
The productive galleries at various positions and levels in Zhuanmiao mining district are characteristic of having aquifers of low water-richness.
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