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Dynamic behaviors of water-saturated and frozen sandstone subjected to freeze-thaw cycles

作     者:Feng Gao Cong Li Xin Xiong Yanan Zhang Keping Zhou Feng Gao;Cong Li;Xin Xiong;Yanan Zhang;Keping Zhou

作者机构:School of Resources and Safety EngineeringCentral South UniversityChangsha410083China Research Center for Mining Engineering and Technology in Cold RegionsCentral South UniversityChangsha410083China Department of Aerospace and Mechanical EngineeringThe University of ArizonaTucsonAZ85721USA 

出 版 物:《Journal of Rock Mechanics and Geotechnical Engineering》 (岩石力学与岩土工程学报(英文版))

年 卷 期:2023年第15卷第6期

页      面:1476-1490页

核心收录:

学科分类:081401[工学-岩土工程] 08[工学] 0818[工学-地质资源与地质工程] 0814[工学-土木工程] 

基  金:supported by the Hunan Provincial Natural Science Foundation of China(Grant No.2020JJ4704) the Fundamental Research Funds for the Central Universities of Central South University,China(Grant Nos.2021zzts0881 and 2021zzts0279) 

主  题:Freeze-thaw(F-T)cycle damage Dynamic properties Split Hopkinson pressure bar(SHPB) Increasing rate of porosity 

摘      要:In high-altitude cold areas,freeze-thaw(F-T)cycles induced by day-night and seasonal temperature changes cause numerous rock mass slope engineering *** investigate the dynamic properties of rock in the natural environment of a high-altitude cold area,standard specimens were drilled from the slope of the Jiama copper mine in Tibet,and dynamic compression tests were performed on watersaturated and frozen sandstone with different numbers of F-T cycles(0,10,20,30,and 40)by the split Hopkinson pressure bar(SHPB)system with a cryogenic control *** influence of water-saturated and frozen conditions on the dynamic performance of sandstone was *** following conclusions are drawn:(1)With increasing strain rate,the attenuation factor(la)of water-saturated sandstone and the intensifying factor(li)of frozen sandstone linearly *** the number of F-T cycles increases,the dependence factor(ld)of water-saturated sandstone linearly decreases,whereas the ld of frozen sandstone linearly increases.(2)The prediction equation of the dynamic compressive strength of water-saturated and frozen sandstone is obtained,which can be used to predict the dynamic compressive strength of sandstone after various F-T cycles based on the strain rate.(3)The mesoscopic mechanism of water-saturated and frozen sandstone’s dynamic compressive strength evolution is *** water softening effect causes the dynamic compressive strength of water-saturated sandstone to decrease,whereas the strengthening effect of pore ice causes it to increase.(4)The decrease in the relative dynamic compressive strength of water-saturated sandstone and the increase in the relative dynamic compressive strength of frozen sandstone can be attributed to the increased porosity.

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