地震地质 ›› 1986, Vol. 8 ›› Issue (2): 69-76.
• 科研简报 • 上一篇 下一篇
吴景浓1, 吴绵拔2
收稿日期:
出版日期:
发布日期:
Wu Jingnang1, Wu Mianba2
Received:
Online:
Published:
摘要: 本文应用岩石孔压三轴仪,研究花岗岩和大理岩的破裂特性,探讨应力途径对岩石破裂强度的影响。试验结果表明:(1)岩石的内孔水压致裂强度随围压的增加而线性增加,(2)在拉,压应力组合条件下,岩石呈现出拉破特性,引起岩石破裂的拉应力随着轴压增加而减少;(3)孔压致裂法获得的岩石抗拉强度值偏高。
Abstract: In this paper fracturing behavior of granite and marble as well as the effect of the stress path on the rock fracturing strength,is studied by use of the rock pore-triaxial apparatus.The test results show that:(1)strength of pore-pressure fractured rock increases with increase of confining,pressure;(2)under the tensile-compressive stress the rock shows the tensile fracture and the tensile stress which causes fracture in the rock decreases with increase of the axial pressure;(3)the values of rock tension strength from hydrofracturing are higher than those from other methods.
吴景浓, 吴绵拔. 内孔加压三轴条件下岩石的破裂试验研究[J]. 地震地质, 1986, 8(2): 69-76.
Wu Jingnang, Wu Mianba. EXPERIMENTAL RESEARCH OF ROCK FRACTURE UNDER PORE-TRIAXIAL STRESS CONDITION[J]. SEISMOLOGY AND GEOLOGY, 1986, 8(2): 69-76.
0 / / 推荐
导出引用管理器 EndNote|Ris|BibTeX
链接本文: https://www.dzdz.ac.cn/CN/
https://www.dzdz.ac.cn/CN/Y1986/V8/I2/69