SURFACE ROUGHNESS ASSESSMENT OF NATURAL ROCK JOINTS BASED ON AN UNSUPERVISED PATTERN RECOGNITION TECHNIQUE USING 2D PROFILES

IF 1.2 Q3 GEOSCIENCES, MULTIDISCIPLINARY Rudarsko-Geolosko-Naftni Zbornik Pub Date : 2023-01-01 DOI:10.17794/rgn.2023.2.14
Ali Mohamad Pakdaman, M. Moosavi
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引用次数: 2

Abstract

The stability of a jointed rock mass is generally controlled by its shear strength that significantly depends on surface roughness. So far, different methods have been presented for determining surface roughness using 2D profiles. In this study, a new method based on the unsupervised pattern recognition technique using a combination of statistical, geostatistical, directional, and spectral methods for the quantification of the surface roughness will be proposed. To reach this goal, more than 10,000 profiles gathered from 92 surfaces of natural rock joints were scanned. The samples were collected from limestone cores of the Lar Dam located in the Mazandaran Province, Iran. After introducing a new spectral index, determined from the fast Fourier transform for measuring the unevenness of rough profiles, statistical, geostatistical, directional, and spectral features revealing waviness and unevenness of the 2D profiles were extracted, and a representative vector and profile for each surface were introduced through the weighted mean and median of the profile features. Principal component analysis (PCA) was utilized for finding the direction of the maximum variance of information. Then, clustering of the 92 samples was performed via K-means, and the silhouette measure was used in order to find the optimal number of clusters resulted in the creation of 13 clusters. To verify the procedure, a sample was selected in each cluster, and direct shear tests were performed on the samples. Comparing the experiments and the clustering results shows they are in good agreement. Thus, the method is an efficient tool for the quantitative recognition of surface roughness considering the waviness and unevenness of a surface.
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基于二维剖面无监督模式识别技术的天然岩石节理表面粗糙度评价
节理岩体的稳定性通常由其抗剪强度控制,而抗剪强度在很大程度上取决于表面粗糙度。到目前为止,已经提出了使用二维轮廓来确定表面粗糙度的不同方法。本文提出了一种基于无监督模式识别技术的表面粗糙度量化方法,该方法结合了统计、地质统计、定向和光谱方法。为了实现这一目标,从92个天然岩石节理表面收集了10,000多个剖面进行了扫描。样本采集自伊朗马赞达兰省拉尔大坝的石灰岩岩心。在引入用于测量粗糙剖面不均匀度的快速傅里叶变换确定的新的光谱指数后,提取二维剖面的统计特征、地统计特征、方向特征和光谱特征,并通过剖面特征的加权平均值和中位数引入每个表面的代表性矢量和剖面。利用主成分分析(PCA)寻找信息最大方差的方向。然后,通过K-means对92个样本进行聚类,并使用剪影测量来寻找最佳聚类数量,结果创建了13个聚类。为了验证该程序,在每个簇中选择一个样本,并对样本进行直接剪切试验。将实验结果与聚类结果进行比较,结果表明两者吻合较好。因此,该方法是一种有效的定量识别表面粗糙度的工具,考虑了表面的波浪形和不均匀性。
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来源期刊
CiteScore
2.50
自引率
15.40%
发文量
50
审稿时长
12 weeks
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