摘要
通过砂岩的单轴压缩试验,研究不同干湿循环作用下砂岩强度劣化规律。试验结果表明,随着干湿循环次数的增加,砂岩峰值强度呈指数关系降低。即干湿循环作用下砂岩强度劣化是一个内部基质结构损伤累积、扩展直至破坏的渐进性过程,可通过劣化度定量描述。研究成果将为遭受干湿循环作用的工程体的短期和长期稳定性安全评价提供有益的依据。
Through the uniaxial compression test of sandstone,the strength degradation rule of sandstone under differ- ent dry-wet circulation is studied. The test results show that with the increase of dry-wet cycles, the peak intensity of sand- stone decrease by exponential relationship,i, e sandstone strength degradation under dry-wet circulation is a progressive deg- radation with internal structure damage accumulation, extension until destruction. The research results provide a beneficial basis for short term and long term stability and safety evaluation of the engineering under dry-wet circulation condition.
出处
《金属矿山》
CAS
北大核心
2013年第10期5-7,11,共4页
Metal Mine
基金
国家自然科学基金项目(编号:51004075
50974093)
中国博士后科学基金项目(编号:20110491631)
山西省青年科技研究基金项目(编号:2011021024-2)
山西省高校优秀青年学术带头人计划项目(编号:2012)
关键词
干湿循环
砂岩
抗压强度
破坏形式
Dry-wet circulation, Sandstone, Compressive strength, Damage form