利用模拟确定地下洞口周围的块体大小

N. Maerz, P. Germain
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引用次数: 26

摘要

岩体的原位块体尺寸可能是影响某些地下洞室稳定性和强度的唯一最重要的参数。岩体通常可以合理地用简单的尺寸-强度分类来描述。实际块体尺寸分布是节理方向、间距和岩体持久性相互作用的产物。尽管原位块体尺寸很重要,但目前很难量化。块体尺寸通常用三个指标之一来估计,即岩石质量标识(RQD)、体积联合计数(jv)和块体尺寸指数(ib)。这些是索引属性,不能量化实际的块大小。诺兰达技术中心已开始采用标准化扫描线绘图技术,以便描绘不连续性的特征。这些数据被用来量化块大小。已经开发了一些算法来模拟由许多节理或节理集划分特定体积的岩石。根据现场数据的汇总统计和推断分布,这些节理可以随机生成,也可以使用沿着扫描线测量的实际节理确定生成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Block size determination around underground openings using simulations
The in situ block size of the rock mass may be the single most important parameter influencing the stability and strength of some underground openings. Rock masses can often reasonably be characterized by a simple size-strength classification. The actual block size distribution is the product of the interaction between the joint orientation, spacing and persistence of that rock mass. Despite the importance of in situ block size, it is currently difficult to quantify. Block size is typically estimated as one of three indices, Rock Quality Designation (RQD), Volumetric Joint Count (J v ), and Block Size Index (I b ). These, being index properties do not quantify actual block size. The Centre de Technologie Noranda has initiated standardized scanline mapping techniques for the purposes of characterizing the discontinuities. This data is being used to quantify block size. Algorithms have been developed which simulate the division of a specified volume of rock by a number of joints or joint sets. These joints can be generated stochastically, based on summary statistics and inferred distributions of the field data, or deterministically, using the actual joints measured along the scanline.
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