某稠化尾矿库的原位状态估计

D. Reid
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引用次数: 1

摘要

估计在加厚的尾矿储存设施内将达到的原位状态通常是具有挑战性的,因为众所周知,实验室制备的标本在全尺寸高能沉降下沉降时不一定能再现尾矿的结构和密度。在实验室中从不分离的浆液中制备的样品通常会产生相当致密的状态,这可能不会在全面沉积中发生。其中一些问题是在最近对一个浓缩尾矿库的岩土工程调查中调查的。该研究包括锥贯入试验(CPT)探头,然后在靠近尾矿底部饱和区域内探头直接邻近的位置进行活塞取样。利用活塞试样的重量水含量(GWC)估算整个试样的原位密度,并为制备松散、湿夯实、重构试样提供材料,用于测量回收尾矿的临界状态线(CSL)。通过比较原位GWCs和CSLs得出的结果与基于cpt的方法推断的结果一致,为这两种技术提供了额外的信心。在实验室中制备成浆料的重构样品显示出比原位GWCs所显示的更致密的状态,这就提出了关于实验室制备的浆料用于调查原位可能达到的密度的准确性的问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimating the in situ state of a thickened tailings deposit
Estimating the in situ state that will be achieved within a thickened tailings storage facility is often challenging, as laboratory-prepared specimens are known to not necessarily reproduce the fabric and density of the tailings when they settle under full-scale high energy deposition. Samples prepared in the laboratory from non-segregating slurries often result in quite dense states, which may not occur in full-scale deposition. Some of these issues were investigated during a recent geotechnical investigation of a thickened tailings deposit. The investigation consisted of cone penetration test (CPT) probes followed by piston samples at locations directly adjacent to the probes within saturated regions near the base of the tailings. The piston samples were used to estimate in situ density by means of gravimetric water content (GWC) of the entire sample, and to provide material for preparing loose, moist tamped, reconstituted samples for measuring the critical state line (CSL) of the recovered tailings. The resulting state indicated by comparing the in situ GWCs and the CSLs agreed well with that inferred by CPT-based methods, providing additional confidence in both techniques. A reconstituted sample prepared as a slurry in the lab exhibited a denser state than that indicated from in situ GWCs, raising questions about the accuracy of laboratory-prepared slurries for investigating the density likely to be achieved in situ.
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