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地下礦山充填料巖石區域非均質一維滲流規律

One-dimensional seepage laws of backfill-rock in heterogeneous area in underground mines

  • 摘要: 以地下礦山采場為對象建立了充填料巖石滲流模型,根據實際情況確立初始條件和邊界條件,推導出水在充填料和巖石中的滲流壓力和流量公式,在此基礎上分析了地下充填料巖石中的滲流規律及影響因素.通過分析得出:在充填料中,流量在初始階段增長較快,達到一個峰值后逐漸下降;壓力隨時間逐漸降低,最后趨于穩定;滲透率越大,流量和壓降越大;高度越高,流量越小而壓降越大;孔隙度越小,壓力越大,孔隙度對流量的影響在不同階段各不相同.在巖石中,滲流壓力與其滲透率無關,但受充填料滲流的影響較大,隨時間降低,滲流流量則只與巖石的滲透率有關.

     

    Abstract: Taking underground mine stope as the object of study, a fill-rock seepage model was established and the seepage pres-sure and flow formula of water in backfill-rock were deduced according to the practical situation which confirmed the initial and boundary conditions. Based on that, the seepage laws and influencing factors were analyzed. The results show that in backfill, the flow increases rapidly in the initial stage, then reaches a peak and gradually declines; the seepage pressure decreases gradually and tends to be stable;the larger the permeability, the larger the flow and pressure drop;the higher the height, the smaller the flow and the larger the pressure drop;the smaller the porosity, the higher the pressure. Porosity has different effects on the flow in different stages. In the rock, seepage pressure has no relationship with the permeability but greatly affected by the seepage of back-fill and declines with time. The flow only relates to the rock mass permeability.

     

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