首页> 外文期刊>Journal of Engineering and Technological Sciences >Hydraulic Conductivity Modeling of Fractured Rock at Grasberg Surface Mine, Papua-Indonesia
【24h】

Hydraulic Conductivity Modeling of Fractured Rock at Grasberg Surface Mine, Papua-Indonesia

机译:巴布亚-印尼Grasberg露天矿的裂隙岩水导率模拟

获取原文
           

摘要

Packer tests and slug tests were conducted at 49 points at the Grasberg surface mine, Indonesia to obtain hydraulic conductivity data. The HC-system approach, which relies on rock quality designation, lithology permeability index, depth index, and gouge content designation, was applied. Geotechnical drill holes in 441 locations, consisting of 4,850 points of information, were used to determine the K values using the equation K = 2x10 -6 x HC 0.5571 . The K values, which were within the range of 10 -8 and 10 -5 m/s, were distributed into five alternative 3D distributions using Ordinary Kriging (OK) and Artificial Neural Network (ANN). The result of the ANN modeling showed that some of the K values, with log K varying from -10.51 m/s to -3.09 m/s, were outside the range of the observed K values. The OK modeling results of K values, with log K varying from -8.12 m/s to -5.75 m/s, were within the range of the observed K values. The ANN modeled K values were slightly more varied than the OK modeled values. The result of an alternative OK modeling was chosen to represent the existing data population of flow media because it fits well to the geological conditions.
机译:在印度尼西亚Grasberg露天矿的49个点进行了封隔器测试和段塞测试,以获得水力传导率数据。 HC系统方法依赖于岩石质量的指定,岩性渗透率指数,深度指数和断层含量的指定。使用等式K = 2x10 -6 x HC 0.5571,使用441个位置的岩土钻孔(包括4,850个信息点)来确定K值。使用普通克里金法(OK)和人工神经网络(ANN)将K值分别在10 -8和10 -5 m / s的范围内分配到5种3D分布中。 ANN建模的结果表明,某些K值在log K从-10.51 m / s到-3.09 m / s的范围内,不在所观察到的K值范围内。 K值的OK建模结果(log K从-8.12 m / s到-5.75 m / s)在观察到的K值范围内。 ANN建模的K值比OK建模的值略有变化。选择替代OK建模的结果来表示现有的流动介质数据,因为它非常适合地质条件。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号