Experimental studies on the pore structure and mechanical properties of anhydrite rock under freeze-thaw cycles  

作　　者：Chao Hou Xiaoguang Jin Jie He Hanlin Li 

机构地区：[1]School of Civil Engineering,Chongqing University,Chongqing,400045,China [2]Key Laboratory of New Technology for Construction of Cities in Mountain Area of the Ministry of Education,Chongqing University,Chongqing,400045,China [3]State Key Laboratory of Coal Mine Disaster Dynamics and Control,Chongqing University,Chongqing,400045,China

出　　处：《Journal of Rock Mechanics and Geotechnical Engineering》2022年第3期781-797,共17页岩石力学与岩土工程学报（英文版）

基　　金：the National Natural Science Foundation of China for financial support (Grant No. 51578091)

摘　　要：To study the deterioration mechanisms of anhydrite rock under the freeze-thaw weathering process,the physico-mechanical characteristics and microstructure evolutions of anhydrite samples were determined by a series of laboratory tests.Then,a descriptive-behavioral model was used to measure the integrity loss in anhydrite samples caused by cyclic freeze-thaw.Finally,the freeze-thaw damage mechanisms of anhydrite rock were revealed from the macro and micro aspects.The results show that the pore size of the anhydrite rock is mainly concentrated in the range of 0.001-10μm.As the number of freeze-thaw cycles increases,there is a growth in the proportion of macropores and mesopores.However,the proportion of micropores shows a declining trend.The relations of the uniaxial compressive strength,triaxial compressive strength,cohesion,and elastic modulus versus freeze-thaw cycles can be fitted by a decreasing exponential function,while the internal friction angle is basically unchanged with freezethaw cycles.With the increase of confining pressure,the disintegration rates of the compressive strength and the elastic modulus decrease,and the corresponding half-life values increase,which reveals that the increase of confining pressures could inhibit freeze-thaw damage to rocks.Moreover,it has been proven that the water chemical softening mechanism plays an essential role in the freeze-thaw damage to anhydrite rock.Furtherly,it is concluded that the freeze-thaw weathering process significantly influences the macroscopic and microscopic damages of anhydrite rock.

关 键 词：Anhydrite rock Freeze-thaw cycles Physico-mechanical characteristics Microstructure evolution Deterioration mechanisms 

分 类 号：TU45[建筑科学—岩土工程]