承压含水层自身性质对地表沉陷的影响规律

    The Influences Laws of Confined Aquifer Own Properties on Surface Subsidence

    • 摘要: 为了确定28采区继续回采对地表建筑物的影响,以9#煤层28采区上覆第四纪承压含水层为研究目标,综合采用理论分析、数值模拟等手段,运用岩层移动、地下水动力学相关知识,研究了含水层自身性质对地表沉陷的影响,研究结果表明:在28采区条件下,地表沉陷与含水层压力、渗透系数成正比关系;含水层厚度对地表沉陷的影响呈抛物线状态,在厚度为30 m时,对应的地表沉陷最大;28采区继续回采地表沉陷最大值较以往将会不断的减小,不会对建筑物造成进一步的破坏。

       

      Abstract: In order to determine the influence of continuous mining in 28th Mining Area on the surface building, based on the related knowledge of rock movement and groundwater dynamics, this paper uses the overlying quaternary confined aquifers in No. 9 coal seam as the objectives to study the impact of aquifer properties on surface subsidence by theoretical analysis and numerical simulation. The research results show that the relationship among surface subsidence, aquifer pressure and permeability coefficient is proportional under 28 mining area conditions. The influence of the aquifer thickness on the surface subsidence is a parabola, and when the thickness is 30 m, the surface subsidence is the largest. After the continuous mining in 28th mining area, the ground subsidence maximum value will continue to reduce than in the past, and it will not cause further damage to surface buildings.

       

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