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首页> 外文期刊>Quality Control, Transactions >Crack Cause in the High Slope of Chinese Ancient Copper Mine Relics: A Three-Dimensional Non-Linear Finite Difference Analysis
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Crack Cause in the High Slope of Chinese Ancient Copper Mine Relics: A Three-Dimensional Non-Linear Finite Difference Analysis

机译:中国古代铜矿遗物高坡裂纹原因:三维非线性有限差分分析

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摘要

Preservation of world heritage and archaeological sites depends largely on better understanding of the soil and rock conditions and their alterations caused by natural and anthropogenic forces. This study took the Tonglushan Ancient Copper Mine (TACM), a key cultural relic site under the state protection in China, as an example to discuss that detailed field and numerical studies of rock mechanics can help understand the crack genesis of high slopes at the site, thus better protecting the relic site from damage. Several cracks occurred in the high slopes at TACM, thus in-situ investigations have been conducted to figure out the factors inducing the cracks. After that, a three-dimensional non-linear finite difference numerical model was applied to investigate the factors affecting the deformation and rupture of the high slopes at TACM. The numerical study revealed that certain mining activities in the copper mines around the TACM relic site could be responsible for the generation of cracks. Five typical mining and excavation plans have been simulated via numerical models; meanwhile rational deformation and failure criterions were determined, according to which, case-5, including eight horizontal tunnels sequentially excavated at different elevations, was found to be the most reasonable hypothesis to explain the generation of cracks and failure of slopes. Case-5 involved applying the SPSC (Sill Pillars Sublevel Caving) method to excavate the ore bodies located at the foot of the slopes and to subsequently backfill the empty chambers after the closure of mining activity. Finally, recommendations were given based on this study to remedy the generation of cracks and better preserve the TACM.
机译:世界遗产和考古遗址的保存在很大程度上取决于对土壤和岩石条件的更好理解及其自然和人为力引起的改变。本研究采用了桐庐古铜矿(TACM),是中国国家保护的关键文物遗址,作为讨论该岩石力学的详细领域和数值研究可以帮助了解现场高斜坡的裂纹创世纪,从而更好地保护遗物部位免受损坏。在TACM的高斜坡中发生了几个裂缝,因此已经进行了原位调查,以弄清楚诱导裂缝的因素。之后,应用了三维非线性有限差值数值模型来研究影响TACM的高斜坡变形和破裂的因素。数值研究表明,TACM遗址周围的铜矿中的某些采矿活动可能负责产生裂缝。通过数值模型模拟了五种典型的采矿和挖掘计划;同时确定了可理性的变形和故障标准,根据该案例-5,包括在不同凸起的八个水平隧道中依次挖掘,发现是最合理的假设,用于解释裂缝的产生和斜坡失败。案例5涉及应用SPSC(Sill Pillars Sublevel Caving)方法挖掘位于斜坡脚下的矿体,并随后在闭合采矿活动后回填空腔室。最后,基于这项研究给出了建议,以补救裂缝的产生,并更好地保留塔克。

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