岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2013年
z2期
3049-3055
,共7页
贾海梁%刘清秉%项伟%张伟丽%郎林智
賈海樑%劉清秉%項偉%張偉麗%郎林智
가해량%류청병%항위%장위려%랑림지
岩石力学%饱和砂岩%冻融循环作用%损伤模型%开孔隙率
巖石力學%飽和砂巖%凍融循環作用%損傷模型%開孔隙率
암석역학%포화사암%동융순배작용%손상모형%개공극솔
rock mechanics%saturated sandstone%freeze-thaw cycles%damage evolution model%open porosity
首先分析饱和砂岩所经历的冻融作用的特点,认为冻融作用是一种低周疲劳荷载,且砂岩冻融循环作用下的受力状态可简化为单向拉伸荷载的循环作用。基于以上分析,在疲劳损伤理论的基础上,建立砂岩在冻融循环作用下的损伤演化方程。同时,通过对饱和砂岩冻融循环过程中的物理性质的观测,及对砂岩自身结构特点的分析,选取砂岩的开孔隙率作为损伤变量。之后通过试验数据对所建立的损伤模型进行验证,并探讨损伤方程中各参数的确定方法。经过验证,该损伤模型能较好地反映饱和砂岩在冻融循环作用下的损伤扩展规律,可以为相关的研究提供参考。
首先分析飽和砂巖所經歷的凍融作用的特點,認為凍融作用是一種低週疲勞荷載,且砂巖凍融循環作用下的受力狀態可簡化為單嚮拉伸荷載的循環作用。基于以上分析,在疲勞損傷理論的基礎上,建立砂巖在凍融循環作用下的損傷縯化方程。同時,通過對飽和砂巖凍融循環過程中的物理性質的觀測,及對砂巖自身結構特點的分析,選取砂巖的開孔隙率作為損傷變量。之後通過試驗數據對所建立的損傷模型進行驗證,併探討損傷方程中各參數的確定方法。經過驗證,該損傷模型能較好地反映飽和砂巖在凍融循環作用下的損傷擴展規律,可以為相關的研究提供參攷。
수선분석포화사암소경력적동융작용적특점,인위동융작용시일충저주피로하재,차사암동융순배작용하적수력상태가간화위단향랍신하재적순배작용。기우이상분석,재피로손상이론적기출상,건립사암재동융순배작용하적손상연화방정。동시,통과대포화사암동융순배과정중적물이성질적관측,급대사암자신결구특점적분석,선취사암적개공극솔작위손상변량。지후통과시험수거대소건립적손상모형진행험증,병탐토손상방정중각삼수적학정방법。경과험증,해손상모형능교호지반영포화사암재동융순배작용하적손상확전규률,가이위상관적연구제공삼고。
Freeze-thaw cycles applying to saturated sandstone are considered as a kind of low frequency fatigue load after the analysis of its features. And the stress condition of sandstone under freeze-thaw cycles can be simplified to cycles of uniaxial tension. According to the above analysis,damage evolution equation is established based on the fatigue damage theory. Then,the open porosity of sandstone which has been tested during the freeze-thaw experiment is selected as the damage variable. After that,the new damage evolution model is tested and verified by the comparison between experiment data and theoretical value,and how to get the values of parameters in the equation is also discussed. The new model is proved to be able to describe the basic damage evolution law of sandstone,this could be the reference for similar researches.