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Gold quarry North Waste Rock Facility slide investigation and stabilization

机译:采石场北部Waste石场的幻灯片调查和稳定

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On February 5th, 2005, approximately 9.1 Megatonnes of the Gold Quarry North Waste Rock Facility (NWRF) collapsed. The slide covered over 460 meters of Nevada State Route 766 and came within 10 meters of a nearby creek. The slope had been at or near its final design configuration since the early 1990's (3H:1V). Following an extensive geotechnical investigation, it was determined that the NWRF slide resulted due to strain-softening, fine grained plastic clayey silt that composed the lower 2/3 of the height that failed along the contact with the native ground surface. Instability developed as the clayey silt passed from its peak to residual strength. Stabilization measures to achieve a 5.1H:1V design slope have included unweighting of approximately 11 Megatonnes and constructing a 1.4 Megatonnes buttress. Movement recognized during remediation required design modifications based on current assumptions that the strength properties of the slide surface are two standard deviations less than the average residual strength determined from laboratory tests.
机译:2005年2月5日,大约9.1百万吨的采石场北部Waste石场(NWRF)倒塌。滑道覆盖了内华达州766号州际公路460米,距离附近的一条小溪不到10米。自1990年代初以来(3H:1V),该斜坡已经达到或接近其最终设计构型。经过广泛的岩土工程研究,确定NWRF滑坡是由应变软化的细颗粒塑料黏土淤泥产生的,该淤泥包括沿与天然地面接触失败的高度的2/3。随着黏土粉土从峰值到残余强度的变化,不稳定性得到发展。为达到5.1H:1V的设计斜度而采取的稳定措施包括:失重约11兆吨,并建造1.4兆吨支撑。在补救过程中识别出的运动需要根据当前的假设进行设计修改,即滑动表面的强度特性是两个标准偏差,小于从实验室测试确定的平均残余强度。

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