Dynamic characteristics deterioration laws of sandstone under cyclic saturation-air drying
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Dynamic characteristics deterioration laws of sandstone under cyclic saturation-air drying
Vol. 34, Issue 9, (2013)
作者机构:
1. 三峡大学 三峡地区地质灾害与生态环境湖北省协同创新中心,湖北,宜昌,443002
2. 三峡大学 三峡库区地质灾害教育部重点实验室,湖北,宜昌,443002
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:13 September 2013,
Published:2013
稿件说明:
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DENG Hua-feng, LUO Qian, LI Jian-lin, et al. Dynamic characteristics deterioration laws of sandstone under cyclic saturation-air drying[J]. 2013, 34(9).
DOI:
DENG Hua-feng, LUO Qian, LI Jian-lin, et al. Dynamic characteristics deterioration laws of sandstone under cyclic saturation-air drying[J]. 2013, 34(9).DOI:
Dynamic characteristics deterioration laws of sandstone under cyclic saturation-air drying
Under the condition of long-term cyclic saturation-air drying
long-term stability of reservoir bank slopes are affected by their dynamic characteristics change rules
and the hydro-fluctuation belt is the sensitive area. Thereafter
taking typical sandstone in the hydro-fluctuation belt of reservoir bank in Three Gorges reservoir area
a test scheme is designed with the consideration of coupling interaction of water pressure changes and saturation-air dry cyclic function
and uniaxial cyclic loading and unloading dynamic response tests of sandstone with different saturation-air dry cycle periods are carried out. The experimental results show that the hysteresis loop area of dynamic stress-strain curve and axial strain of the sandstone samples increase gradually when they experience the same times cyclic loading and unloading
and the dynamic elastic modulus of sandstone samples decrease gradually and damping coefficient
damping ratio increases gradually during the saturation-air dry cyclic process
which indicates that the saturation-air dry cyclic function has a cumulative damage of dynamic characteristics on the samples. Finally
degradation mechanisms of dynamic characteristics under the saturation-air dry cyclic function are discussed in detail based on the microscopic structure change of sandstones. Research results have an important reference for the long-term stability analysis of reservoir bank slopes considering the earthquake action.