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Numerical Modelling of Water Flow Through Granular Material for Isolated and Simultaneous Extractions in Block Caving

机译:砌块塌陷中颗粒材料水流的数值模拟

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摘要

In this work, we numerically solve the Brinkman-Darcy equation coupled to the granular kinematic model using the finite elements method in 2D, to describe the entry of water into draw points in Block Caving mining. We perform a total of 990 numerical simulations incorporating the relative change of local rock density (/p), particle size (Dp), extraction area (S) and the separation between draw points (L). We propose two mathematical models using scale arguments for estimating the velocity of the water in the draw point as a function of two and three dimensionless numbers (for isolated and simultaneous extractions, respectively). The relative error in the estimation of the results using the mathematical model for the set of numerical experiments ranges from 0.83 to 6.09%, where the greatest deviations correspond to Dp=6mm. The proposed models allow estimating the water velocity at the draw point, which in turn helps to predict the time and place where there is a greater probability of a mud rush occurrence. The results can be applied in the design and optimisation of extraction sequences when the water present in the subsoil of a mine is a relevant factor to consider.
机译:在这项工作中,我们使用2D中的有限元方法来数值解决与粒状运动学模型的Brinkman-Darcy方程,以描述水进入块塌陷挖掘中的绘制点。我们总共执行990个数值模拟,包括局部岩石密度(/p),粒度(DP),提取区域和绘制点(L)之间的分离的相对变化。我们提出了两个数学模型,使用比例参数,用于估计绘图点中的水的速度,作为两个和三维无量纲的函数(分别用于分离和同时提取)。使用数值实验集的数学模型估计结果的相对误差范围为0.83至6.09%,其中最大偏差对应于DP = 6mm。所提出的模型允许估计抽取点的水速,这反过来有助于预测泥浆冲击发生更大可能性的时间和地点。结果可以应用于提取序列的设计和优化时,当矿井的底层存在是需要考虑的相关因素。

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