摘要
通过对常用水力压裂模型中忽略岩石断裂韧度效应这一现象的讨论,给出了全面考虑水力压裂中各种影响因素的能量平衡方程,并由此建立了通过水力压裂实验直接确定岩石视在K_(1c)值的方法。最后通过对影响岩石视在断裂韧度因素的讨论,论证了水力压裂法确定的岩石视在K_(1c)值大大地大于标准3点弯曲实验值的必然性。
Based on the discussion of the phenomenon that the effect of fracture toughness is neglected in general hydraulic fracturing models, this paper gives the energy balance equation in-colding all parameters in hydraulic fracturing and proposes a method of determining the apparent fracture toughness of rock from hydraulic fracture experimental data. The discussion on the factors affecting apparent toughness indicates the inevitability that the apparent fracture toughness of rock measured by hydraulic fracture experimental data is significantly higher than that measured by the standard three-point bending method.
出处
《重庆大学学报（自然科学版）》
EI
CAS
CSCD
1992年第2期1-6,共6页
Journal of Chongqing University
基金
国家自然科学基金
关键词
水力压裂
能量平衡
断裂韧度
hydraulic fracture
energy balance
fracture toughness
