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Application of statistical approaches to analyze geological, geotechnical and hydrogeological data at a fractured-rock mine site in Northern Canada

机译:统计方法在加拿大北部裂隙岩矿场的地质,岩土和水文地质数据分析中的应用

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摘要

Mine site characterization often results in the acquisition of geological, geotechnical and hydrogeological data sets that are used in the mine design process but are rarely co-evaluated. For a study site in northern Canada, bivariate andmultivariate (hierarchical) statistical techniques are used to evaluate empirical hydraulic conductivity estimation methods based on traditional rock mass characterisation schemes, as well as to assess the regional hydrogeological conceptual model. Bivariate techniques demonstrate that standard geotechnical measures of fracturing are poor indicators of the hydraulic potential of a rock mass at the study site. Additionally, rock-mass-permeability schemes which rely on these measures are shown to be poor predictors of hydraulic conductivity in untested areas. Multivariate techniques employing hierarchical cluster analysis of both geotechnical and geological data sets are able to identify general trends in the data. Specifically, the geological cluster analysis demonstrated spatial relationship between intrusive contacts and increased hydraulic conductivity. This suggests promise in the use of clustering methods in identifying new trends during the early stages of hydrogeological characterization.
机译:矿山场地特征分析通常会导致获取地质,岩土和水文地质数据集,这些数据集已用于矿山设计过程,但很少进行共同评估。对于加拿大北部的一个研究点,使用双变量和多变量(分层)统计技术来评估基于传统岩体表征方案的经验水力传导率估算方法,以及评估区域水文地质概念模型。双变量技术表明,标准的岩土压裂技术措施不能很好地表明研究现场岩体的水力潜力。另外,依赖于这些措施的岩体渗透率方案显示出在未经测试的区域中水力传导率的不良预测。对岩土和地质数据集采用层次聚类分析的多元技术能够识别数据的总体趋势。具体而言,地质聚类分析表明了侵入性接触与水力传导率之间的空间关系。这表明在利用聚类方法确定水文地质特征早期阶段的新趋势方面有希望。

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