摘要
在深部高地应力地层中取心,岩心层裂(饼化)是一种常见的工程现象。岩心层裂和岩体的物性、力学性质以及原地应力密切相关。为研究钻井取心过程中岩心层裂现象的机理,结合川西南部地区A井和B井取心过程中的岩心层裂现象,考虑岩石矿物组分与岩石脆性指数的关系,基于应力集中的非均匀岩石拉伸破坏模型,给出了岩心层裂现象产生的判据,采用理论计算对饼化现象进行了验证。研究结果表明:脆性矿物含量越高,岩石脆性越强,越易生成裂缝;岩心套取是一个卸载水平方向最大主应力的过程,卸载速度越快,损伤处的附加拉应力越大,且对应被激活损伤的尺寸就越小,当附加拉应力大于岩石抗拉强度时,会出现岩心层裂现象,随着取心的继续此过程将重复地发生下去。
Coring in deep high geostress formation,core discing( layer cake) is a common phenomenon of engineering. The physical properties,mechanical properties of rock mass and the in-situ are closely related to core discing. In order to research the mechanism of core discing,combined with the coring of A and B Wells in southern sichuan,considering the component of rock mineral and rock brittleness index,based on the stress concentration of the heterogeneous rock tensile failure model,giving the criterion of core discing,the theoretical calculation and numerical simulation method verified this phenomenon. The results show that the brittleness mineral content is higher,the stronger the rock brittleness; coring is an unloading cycle of the horizontal maximum principal stress,the faster of unloading,the larger of additional tensile stress tends to excite smaller damages. When additional tensile stress is greater than tensile strength of rocks,core discing can occur,as the coring continues,this process will be repeated
引文
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