首页> 外文会议>2014 SME annual meeting amp; exhibit (SME 2014): Leadership in uncertain times >REMEDIATION OF LARGE-SCALE SLOPE INSTABILITY AND IMPACT ON MINE DEVELOPMENT AT THE GOLD QUARRY MINE
【24h】

REMEDIATION OF LARGE-SCALE SLOPE INSTABILITY AND IMPACT ON MINE DEVELOPMENT AT THE GOLD QUARRY MINE

机译:金采石场大型边坡失稳的治理及其对矿山发展的影响

获取原文
获取原文并翻译 | 示例

摘要

In 2009 the Gold Quarry open pit mine, located 11 km northwest of Carlin, Nevada, USA, experienced multiple large-scale slope instabilities of the upper east highwall that reduced gold ore extraction for nearly 18 months. The slope instabilities occurred within a weak, consolidated sedimentary sequence that exhibits strength characteristics that are transitional between soil and rock. Instability initiated as mining exposed the lower clay-rich sub-units of the Carlin Formation (Fm.). This deformation created preferential flow paths that allowed groundwater from the upper sandy sub-units to infiltrate low permeability clay-rich sub-units, thereby enhancing deformation of the slope toe which in turn destabilized the upper portion of the highwall. The outcome was a 160 m high slope instability that had a lateral runout of 850 m. The effort to return the pit to ore production required both the geotechnical and hydrogeological investigations and the preliminary remediation mining activity to be concurrent. This approach required the development of detailed safety procedures and a requirement to modify the remediation design as new results were obtained. An initial challenge was to mitigate a near vertical, 90 m headscarp with blast induced, localized slope failures. Back-analyses applying numerical modeling indicated that the failure surface did not coincide with initial interpretations based on field observations; drilling results eventually confirmed this alternative failure geometry. The final remediation design incorporated shallower slope geometries and an approximately 3 Mt buttress along the base of the Carlin Formation and bedrock contact to reinforce the lower clay-rich sub-units. The outcome is a stable highwall within the Carlin Fm. following nearly ten years of repeated slope instability, and an example of the necessity to conduct appropriate geotechnical and hydrogeological studies during the early stages of a new layback evaluation or new open pit development.
机译:2009年,位于美国内华达州卡林市西北11公里处的金矿开采露天矿经历了上东高墙的多次大规模边坡失稳,使金矿开采减少了近18个月。边坡失稳发生在一个弱固结的沉积层序中,该序列显示出在土石之间过渡的强度特征。采矿引发的不稳定性使卡林组(Fm。)的下部富含粘土的亚单元暴露出来。这种变形产生了优先流动路径,使地下水从上层沙质亚单元渗入低渗透性富粘土子单元,从而增强了坡脚趾的形变,进而破坏了高墙的上部。结果是160 m高边坡失稳,横向跳动为850 m。为了使矿井恢复成矿石,需要同时进行岩土工程和水文地质调查以及初步的补救采矿活动。这种方法需要制定详细的安全程序,并要求在获得新结果时修改补救设计。最初的挑战是缓解由爆破引起的局部斜坡失稳造成的近垂直,90 m的头皮。应用数值模型的反向分析表明,破坏面与基于野外观测的初始解释不一致。钻探结果最终证实了这种替代的破坏几何形状。最终的补救设计包括较浅的斜坡几何形状以及沿卡林地层和基岩接触的约3 Mt支撑,以增强下部富含粘土的子单元。结果是在卡林(Carlin Fm)内部稳定的高墙。经过近十年反复的边坡失稳,以及在新的后撤评估或新的露天矿开发的早期阶段进行适当的岩土和水文地质研究的例子。

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