Fracture coalescence mechanism of single flaw rock specimen due to freeze-thaw under triaxial compression
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Fracture coalescence mechanism of single flaw rock specimen due to freeze-thaw under triaxial compression
Vol. 35, Issue 6, (2014)
作者机构:
1. 湖北工程学院 城市建设学院,湖北,孝感,432000
2. 武汉理工大学 道路桥梁与结构工程重点实验室,武汉,430070
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:20 June 2014,
Published:2014
稿件说明:
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LU Ya-ni, LI Xin-ping, WU Xing-hong. Fracture coalescence mechanism of single flaw rock specimen due to freeze-thaw under triaxial compression[J]. 2014, 35(6).
DOI:
LU Ya-ni, LI Xin-ping, WU Xing-hong. Fracture coalescence mechanism of single flaw rock specimen due to freeze-thaw under triaxial compression[J]. 2014, 35(6).DOI:
Fracture coalescence mechanism of single flaw rock specimen due to freeze-thaw under triaxial compression
Freeze-thaw test and triaxial compression test are carried out for model samples with pre-existing single fracture by the rock mechanical servo-controlled testing system
freeze-thaw damage degradation model is studied based on the freeze-thaw test
and crack coalescence mechanism is discussed under the triaxial compression condition. Tests reveal that: freeze-thaw damage deterioration modes of fractured rock masses are scattered to particle model
crack model and prefabricated crack fracture mode. Under the triaxial loading condition
there are four coalescence modes of fractured rock samples due to freeze-thaw cycles: tensile mode,shear mode,compression mode and mix mode
which are closely related to the freeze-thaw cycles
confining pressure and the crack dip angle. With the increase of freeze-thaw cycles and confining pressure
more and more surface ruptures are found
at the same time
crack coalescence mode has experienced from single to mix; the failure modes of rock samples show tensile and compression mode when confining pressure reaches the values of 2 MPa and 6 MPa
while tensile mode are presented when the confining pressure reaches the value of 4 MPa. Rock samples with smaller fissure angle which equals 30° are taken on tensile mode
however
the rock samples with the longer fissure angle of 60° take on shear mode.