Particle vs. Laboratory modelling of In Situ compaction

R.M. Holt
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引用次数: 9

Abstract

Physical (in particular mechanical) behaviour is altered because of the stress release occurring when a core sample is retrieved from the Earth. Numerical and experimental simulations have been performed in order to assess the main discrepancies between laboratory measured and virgin in situ rock mechanical behaviour, and in particular, the main characteristics of virgin compaction behaviour. In the laboratory, synthetic sandstones were cemented under stress, permitting virgin compaction as well as stress-released core compaction experiments. Numerically, a discrete particle model (PFC) was used to mimic closely the laboratory procedures. Cement bond breakage causes a transition from stiff to soft behaviour above a certain stress level during virgin compaction. Both techniques show that core compaction may exceed virgin compaction during initial loading.

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现场压实的颗粒模型与实验室模型
物理(特别是机械)行为被改变,因为从地球取回岩心样本时发生的应力释放。已经进行了数值和实验模拟,以评估实验室测量的岩石力学行为与原生岩石力学行为之间的主要差异,特别是原生岩石压实行为的主要特征。在实验室中,合成砂岩在应力作用下被胶结,允许进行原始压实和应力释放岩心压实实验。数值上,采用离散粒子模型(PFC)来模拟实验过程。在初始压实过程中,在一定的应力水平以上,水泥胶结断裂导致从硬到软的转变。两种技术都表明,在初始加载过程中,岩心压实可能超过原生压实。
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