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Pressure Transient Behavior of Horizontal and Slant Wells Intersecting a High- Permeability Layer

机译:水平和倾斜孔交叉的压力瞬态行为与高渗透层相交

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This paper describes numerical simulation studies designed to investigate the behavior of horizontal wells that intersect high permeability layers sandwiched between two lower permeability layers. The paper investigates the pressure transient behavior of 1) purely horizontal wells drilled in the middle layer and 2) slant horizontal wells that intersect all three layers, as the permeability of the high permeability layer is varied. A previous paper1 focused on late time interference effects and radial composite behavior caused by a limited high permeability layer. This study focuses on the early time dual permeability effect and its impact on recognition of conventional horizontal well diagnostic derivative slopes. The horizontal well simulations show a dual permeability effect as the contrast between the high permeability layer and the adjacent layers is increased. The vertical radial flow regime is seldom visible and masked by wellbore storage effects. Interestingly, what is observed however, is a plateau (or sometimes valley) caused by the dual permeability effect followed by a transition to horizontal radial flow regime. This may be explained as a combined effect of recharge and linear flow in the lower permeability layers. The plateau (or a valley) caused by the dual permeability effect, can easily be confused as representing the vertical radial regime. Similarly, the transitional data prior to horizontal radial flow, which includes the dual permeability effects, can be incorrectly analyzed and lead to misleading results. This paper will demonstrate the increased complexity of the pressure transient behavior when the well is slanted through all layers while intersecting the high permeability layer.
机译:本文介绍了数值模拟研究,旨在研究与夹在两个较低渗透层之间的高渗透层相交的水平井的行为。本文研究了1)纯净水平孔的压力瞬态孔在中间层和2)与所有三层相交的倾斜水平孔,随着高渗透层的渗透性而变化。以前的Paper1重点是由有限的高渗透层引起的晚期干扰效应和径向复合行为。本研究重点研究了早期双渗透率效应及其对常规水平井诊断衍生斜坡识别的影响。水平井仿真显示了双渗透率效应,作为高渗透层和相邻层之间的对比度增加。垂直径向流动制度很少可见并通过井筒储存效果掩盖。有趣的是,观察到的是由双渗透效应接下来的平坦(或有时谷),然后是水平径向流动状态的过渡。这可以解释为较低渗透层中的再充电和线性流动的组合效果。由双渗透率效应引起的高原(或山谷)可以很容易地混淆,因为代表垂直径向制度。类似地,可以错误地分析包括双渗透率效应的水平径向流动前的过渡数据,并导致误导性结果。本文将展示当井在相交高渗透层时通过所有层倾斜时的压力瞬态行为的复杂性增加。

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