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Geotechnical characterization of mine waste rock

机译:矿山waste石的岩土特征

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摘要

The determination of geotechnical characterises of waste rock is essential for addressing issues of in situ hydrology and the stability of steep and high-standing dumps. Based on laboratory investigations and numerical modeling, this paper gives the geotechnical properties of a selected waste rock under saturated and unsaturated conditions. Results indicated that the engineering behavior of the investigated waste rock is similar to granular soils and governed by the "well-graded" and "very angular" nature of the materials. The samples exhibited low air entry values (0.2 and 0.8 kPa) and low water storage (0.44) along with a high saturated hydraulic conductivity (1 × 10~(-5) m/s). The hydraulic conductivity dropped sharpely beyond the air entry value by up to eight orders of magnitude at 200 kPa. The shear strength was identical to loose coarse materials and was primarily derived from the angle of internal friction that measured 37° to 39°, similar to the angle of repose. Additional strength can be availabe in the form of effective cohesion due to clays and cementation and apparent cohesion due to matric suction.
机译:确定of石的岩土特征对于解决原位水文问题以及陡峭和高耸的垃圾场的稳定性至关重要。基于实验室研究和数值模拟,本文给出了饱和和不饱和条件下选定selected石的岩土特性。结果表明,所研究的waste石的工程行为类似于粒状土壤,并且受材料的“良好分级”和“非常成角度”的性质支配。样品显示出较低的空气进入值(0.2和0.8 kPa)和较低的储水量(0.44)以及较高的饱和导水率(1×10〜(-5)m / s)。在200 kPa时,水力传导率急剧下降,超出进气值达八个数量级。剪切强度与松散的粗料相同,主要来自内部摩擦角,该角为37°至39°,与休止角相似。由于粘土和胶结作用而产生的有效内聚力以及由于基质吸力引起的表观内聚力,可以以有效的内聚力形式提供额外的强度。

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