Analysis of hydraulic fracturing and calculation of critical internal water pressure of rock fracture
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Analysis of hydraulic fracturing and calculation of critical internal water pressure of rock fracture
Vol. 26, Issue 8, (2005)
作者机构:
1. 河海大学 土木工程学院,南京,210098
2. 西北农林科技大学 水利与建筑工程学院,陕西 杨凌,712100
3. 江苏省扬州市建设局,扬州,225002
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:26 December 2013,
Published:2005
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LI Zong-li, ZHANG Hong-chao, REN Qing-wen, et al. Analysis of hydraulic fracturing and calculation of critical internal water pressure of rock fracture[J]. 2005, 26(8).
DOI:
LI Zong-li, ZHANG Hong-chao, REN Qing-wen, et al. Analysis of hydraulic fracturing and calculation of critical internal water pressure of rock fracture[J]. 2005, 26(8).DOI:
Analysis of hydraulic fracturing and calculation of critical internal water pressure of rock fracture
Hydraulic fracturing is one of important effect factors in water gushing out of deep-buried tunnel construction and cracking and seepage of high head tunnel .Its failure mechanism study is a hot topic in geotechnical engineering fields. Based on stress state in fracture surface and fracture mechanics
the fracture propagation is divided into tension-shear and compression-shear mixed cracking. Using fracture propagation engineering criterion
calculation formulae of critical internal water pressure of two kinds of failure model are obtained respectively; and its effect laws as fracture direction and lateral geo-stress coefficient are studied. The study shows that critical internal pressure of two kinds of model is not varied as fracture direction changing when the lateral pressure coefficient equals 1.0. Under tension-shear complex model
fracture is most easily fracturing when fracture direction is parallel with direction of principal stress. Under compression-shear mixed model
distribution law of critical internal water pressure is same as tension-shear complex model when ( ) large than 1.0. But fracture is most easily fracturing when ( ) less than 1.0 and fracture direction are 45°or 135°angle with principal stress.