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AN ANALYSIS OF THE INFLUENCE OF THE PRESSURIZATION RATE ON THE BOREHOLE BREAKDOWN PRESSURE

机译:压力变化率对井壁破裂压力的影响分析

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This paper investigates the dependence of breakdown pressure, the critical pressure at which tensile failure of the rock is initiated by injecting fluid in a borehole, on the rate of pressurization. The mathematical model explicitly accounts for the existence of micro-cracks at the borehole wall that trigger the failure process. Breakdown, in this context, occurs when the stress intensity factor of a critically oriented micro-crack reaches the rock toughness. The model is presently restricted to low-permeability/low-porosity rocks. By considering one-dimensional lubrication flow in the crack coupled with the non-local elastic response of the crack, the evolution of the net pressure, crack opening and stress intensity factor is obtained as functions of the pressurization rate. The relation between breakdown pressure and pressurization rate in the case of zero initial net pressure is shown to be controlled by only one dimensionless number: the ratio between the initial width of the unstressed micro-crack and the induced elastic opening at failure. It is further shown that (i) the fluid pressure in the early stages of the pressurization history drops in the crack and that cavitation can occur, and (ii) local back-flow in the crack takes place. The dependence of breakdown pressure, P-b, on the pressurization rate, A, is determined as well as the range of A, where p(b) varies significantly. The lower and pseudo upper bounds of this range of pressurization rate correspond to limiting regimes of slow and pseudo fast pressurization. (C) 1997 Elsevier Science Ltd. [References: 20]
机译:本文研究了击穿压力(通过在井眼中注入流体而引发岩石的拉伸破坏的临界压力)对加压速率的依赖性。该数学模型明确说明了在井眼壁处存在微裂纹,这些微裂纹触发了破坏过程。在这种情况下,当临界取向的微裂纹的应力强度因子达到岩石韧性时,就会发生破裂。该模型目前仅限于低渗透率/低孔隙率的岩石。通过考虑裂纹中的一维润滑流动以及裂纹的非局部弹性响应,可以得出净压力,裂纹开度和应力强度因子的变化与增压率的关系。初始净压力为零的情况下,击穿压力与增压率之间的关系仅受一个无因次数控制:无应力微裂纹的初始宽度与失效时引起的弹性开口之间的比率。进一步表明,(i)加压历史早期的流体压力在裂缝中下降,并且会发生气穴现象,并且(ii)裂缝中发生局部回流。确定了击穿压力P-b对加压速率A的依赖性以及A的范围,其中p(b)显着变化。此加压速率范围的下限和拟上限对应于缓慢加压和拟快速加压的限制范围。 (C)1997 Elsevier Science Ltd. [参考:20]

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