干湿循环脆性岩石直接拉伸断裂的宏细观力学模型OA北大核心CSTPCD
A micro-macro mechanical model of direct tensile fracture in brittle rocks under dry-wet cycles
针对三峡库区消落带等长期处于干湿循环条件下导致岩石损伤破坏的工程问题,探究在干湿循环和直接拉伸荷载共同作用下,脆性岩石的宏细观断裂力学特性这个难点问题.由于干湿循环条件下的直接拉伸试验较难实现,考虑干湿循环与直接拉伸荷载作用的宏细观力学关系模型非常欠缺.基于断裂力学理论方法,结合干湿循环试验研究方法,提出了一种干湿循环条件下脆性岩石直接拉伸断裂的宏细观力学模型.该模型是在考虑了干湿循环次数n与含水率ω对断裂韧度KIC和初始损伤因子D0综合影响的基础上,结合岩石初始细观裂纹损伤与裂纹断裂韧度的直接拉伸细观裂纹扩展力学模型建立的.对比分析抗拉强度、裂纹扩展极限长度llim、弹性模量、岩石劣化损伤的理论与试验结果,验证了模型的合理性.讨论了初始裂纹倾角φ、材料常数β等参数影响下,裂纹启裂应力及峰值应力随干湿循环次数n的变化规律.对比分析了干湿循环和单独含水条件对岩石劣化度力学特性的影响.
Aiming at the engineering problem of rock damage and failure caused by long-term dry-wet cycle conditions such as the hydro-fluctuation belt in the Three Gorges reservoir area,this paper investigates the challenging issue of the micro-macro mechanical properties of brittle rocks under the combined effects of dry-wet cycles and direct tensile loading.However,due to the challenges in conducting direct tensile tests under dry-wet cycles,there is a scarcity of macro-micro mechanical models that account for both dry-wet cycles and direct tensile loading.Based on the coupled method of the theory of fracture mechanics and the experiment of dry-wet cycle,a macro-micro mechanical model of direct tensile fracture of brittle rock under the influence of dry-wet cycle conditions is proposed.The model is developed by considering the combined effects of the number of dry-wet cycles(n)and water content(ω)on fracture toughness(KIC)and initial damage(D0).It is then integrated with a direct tensile microcrack propagation mechanical model that considers initial microcrack damage and crack fracture toughness in rocks.The theoretical results for tensile strength,wing crack limit length llim,elastic modulus,and rock deterioration damage are compared with experimental data to validate the reasonableness of the model.The influence of initial crack angle φ,material constant β,and other parameters on the variation of crack initiation stress and peak stress with the number of dry-wet cycles n is discussed.Furthermore,a comparative analysis is conducted to investigate the effects of dry-wet cycles and single water content conditions on the deterioration degree of rocks.
李晓照;车行;李海峰;戚承志
北京建筑大学土木与交通工程学院,北京 100044
土木建筑
脆性岩石干湿循环直接拉伸断裂宏细观力学模型
brittle rocksdry-wet cyclesdirect tensile fracturemicro-macro model
《岩土力学》 2024 (007)
1906-1916,2049 / 12
国家自然科学基金(No.51708016;No.12172036);北京市教委科研项目(No.KM202110016014);北京建筑大学金字塔人才工程(No.JDYC20200307).This work was supported by the National Natural Science Foundation of China(51708016,12172036),the Scientific Research Program of Beijing Municipal Education Commission(KM202110016014)and the Pyramid Talent Training Project of Beijing University of Civil Engineering and Architecture(JDYC20200307).
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