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Assessment of performance of horizontal drains in an open pit mine in eastern Turkey

机译:在土耳其东部露天矿井中的水平排水管性能评估

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Prediction of spatial distribution of pore-water pressure and its control are the main issues in open pit mines, since excess pore-water pressure is one of the main causes of slope instability. Horizontal drains are commonly used to relieve the excess pore-water pressure as a method of slope stabilization. This paper presents the efficacy of horizontal drains along two cross-sections in an open pit mine located in Eastern Turkey by analyzing the re-distribution of pore-water pressure as a consequence of groundwater inflow rates before and after application of horizontal drains. SEEP/W software was used to simulate the flow in saturated and unsaturated zones along North-South and East-West cross-sections. The accuracy of the input data was verified by calibrating the models under steady-state condition against the field data obtained from vibrating wire pressure transducers installed at different depths and locations. This was followed by a transient analysis to confirm the storage parameters. The results of the transient simulation run showed that steady-state model results can be used as initial conditions for transient groundwater inflow predictions. Subsequently, expansion and deepening of the open pit for the year 2019 are modeled in stage-wise for both cross-sections to calculate the groundwater inflow rates into the mine. As a last step, horizontal drains are implemented to the models. The horizontal drains increased groundwater inflow rates by only 15 and 37% for the East-West and North-South cross-sections, respectively. Additionally, the water content was found to be almost close to fully saturation state in the wall rock behind the slope faces even after the use of drains. The findings of this study were verified at the site. The mining company has reported that attempts to drain the slope walls by horizontal drains have proved to be ineffective. In conclusion, it was demonstrated that prevention of seepage from surface channels by either diversion or lining was adopted as opposed to horizontal drill holes as the most effective means of controlling groundwater influence on slope stability.
机译:孔隙水压空间分布的预测及其控制是开坑矿山的主要问题,因为过量的孔隙水压是坡度不稳定性的主要原因之一。横向漏斗通常用于缓解过量的孔隙水压力作为斜坡稳定的方法。本文通过分析水平排水前后的地下水流入速率,展示位于土耳其东部的露天矿区的两个横截面沿两个横截面的疗效。 SEEP / W软件用于模拟南北和东西横截面饱和和不饱和区的流量。通过在稳态条件下校准模型来验证输入数据的准确性,以防止从安装在不同深度和位置处的振动线压力传感器获得的现场数据。接下来是瞬态分析以确认存储参数。瞬态仿真运行的结果显示,稳态模型结果可用作瞬态地下水流入预测的初始条件。随后,2019年露天坑的扩张和加深在阶段为横截面的模型,以计算地下水流入矿井进入矿井。作为最后一步,横向排水管将实现给模型。水平排水管分别仅增加了地下水流入率,仅增加了东北和南北横截面的15%和37%。另外,即使在使用漏斗之后,也发现水含量几乎接近斜面背后的壁岩中的完全饱和状态。该研究的结果在该研究中核实。矿业公司报告说,通过水平排水耗尽坡壁的尝试已经证明是无效的。总之,证明了通过转移或衬里预防从表面通道的渗流,而不是水平钻孔,作为控制地下水对坡度稳定性的最有效手段。

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