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In-situ Test Research for the Affect of Surface Water Seepage on the Ground Fissures Action

机译:原位试验研究对地面泄漏对地下裂缝作用的影响

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An in-situ water injection test across Xi' an ground fissures has been done, in order to simulate the activity of the fissures after water seeps, from October to December, 2005. According to the settlement observed of the bottom of testing pit, it is proven that the surface water seepage speeds the movement of ground fissures. Usually, the soil on the hanging wall of the fissures is more fragmentized than that on the footwall, which is propitious to water seepage. The seepage promotes the interaction between water and soil particles and brings about the differential settlement of two sides of fissures. Therefore, surface water seepage accelerates the activity of the ground fissures.
机译:已经完成了Xi'地面裂隙的原位注水试验,以模拟水渗漏后的裂隙活动,从2005年10月到12月。根据检测坑底部的沉降,它据证明,地表水渗漏速度速度速度速度。通常,裂缝的悬挂墙上的土壤比脚踏墙更裂缝,这有利于水渗漏。渗漏促进水和土壤颗粒之间的相互作用,并带来裂缝两侧的差动沉降。因此,地表水渗透加速了地面裂缝的活性。

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