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岩体结构均质区划分法的适用性研究

郭亮 李晓昭 王益壮 陈为平 程梦林 周扬一

岩土力学Issue(10):2928-2937,3002,11.
岩土力学Issue(10):2928-2937,3002,11.

岩体结构均质区划分法的适用性研究

Applicability research on structural homogeneity delineation of rock masses

郭亮 1李晓昭 2王益壮 1陈为平 2程梦林 1周扬一2

作者信息

  • 1. 南京大学 地球科学与工程学院,南京 210093
  • 2. 南京大学 华东有色地勘局地下空间与地质环境研究所,南京 210093
  • 折叠

摘要

Abstract

Delineation of structural homogeneity of rock masses is the basis of statistics and modeling of discontinuities. In practice, an objective partition result is easier to obtain with key factors as indicators and optimal delineation as the final judgment criterion. In order to better characterize the discontinuities in Chinese high-level nuclear waste disposal preselected region in Gansu Beishan, the measure window truncation, sampling bias and grid variability correction are carried out to deal with the discontinuities of rock masses. Such programming realizes structural homogeneity delineation by using a variety of methods and has a preliminary probe into the distinguish capability, applicability and limitation in Beishan. The results show that, as far as the Beishan preselected area be concerned, different delineation schemes are obtained in which the applicability of the correlation coefficient method and the Mahtab’s method are weak in applicability while the Miller’s method is the best and the Miller’s method is increasing sequentially. It is worth mentioning specially that in the Miller’s methods, the 34-block scheme receives the most satisfactory result. At last, the optimal method is applied to Jijicao area;and the delineation result provides a useful direction for the structural network modeling and the following seepage flow path calculations.

关键词

岩体结构/均质区划分法/判别力/甘肃北山

Key words

rock mass structure/structural homogeneity delineation/distinguish capability/Beishan of Gansu province

分类

建筑与水利

引用本文复制引用

郭亮,李晓昭,王益壮,陈为平,程梦林,周扬一..岩体结构均质区划分法的适用性研究[J].岩土力学,2013,(10):2928-2937,3002,11.

基金项目

国家重点基础研究发展计划(973计划)(No.2013CB036001);国防科技重点项目(科工二司[2012]491号);江苏省普通高校研究生科研创新计划(省助)资助(No. CXZZ13-0057)。 ()

岩土力学

OA北大核心CSCDCSTPCD

1000-7598

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