Activating Shale to Form Well Barriers: Theory and Field Examples

T. Kristiansen, T. Dyngeland, S. Kinn, R. Flatebø, N. Aarseth
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引用次数: 13

Abstract

Shale is a general term used for argillaceous (clay-rich) rocks which are the most abundant sediment on the earth. It is believed that clay rich rocks comprise more than 50-75% of the geologic column. Shale has very varying petrophysical and mechanical properties. Shale is in the most cases acting as a trap or seal for hydrocarbon migration, but has also in more recent years been targeted as a reservoir target in some basins. In some wells it has been observed on cement bond logs that shales in uncemented intervals have moved in and closed the annulus. Pressure communication testing has been performed on these sections and the sections has been qualified as well barrier elements (Williams et al., 2009) for plug and abandonment (P&A) purposes. The main mechanism behind the deformation process is believed to be shale creep. In this paper we will discuss shale creep and other shale deformation mechanisms and how an understanding of these can be used to activate shale that has not contacted the casing yet to form a well barrier. We have developed a numerical model based on first order principles to better understand the mechanical deformation process. We are also supporting the modeling results with laboratory experiments, before we discuss a couple of field cases where shale intervals have been activated and verified to have formed a well barrier as part of the well construction process in new wells.
激活页岩形成井障:理论与现场实例
页岩是地球上沉积物最丰富的泥质(富含粘土)岩石的总称。据信,富含粘土的岩石占地质柱的50-75%以上。页岩具有非常不同的岩石物理和力学性质。页岩在大多数情况下作为油气运移的圈闭或密封,但近年来在一些盆地也被视为储层目标。在一些井中,水泥胶结测井观察到,未胶结层段的页岩进入并封闭环空。在这些井段进行了压力通信测试,这些井段已被认定为井眼隔离元件(Williams et al., 2009),可用于封井弃井(P&A)。变形过程背后的主要机制被认为是页岩蠕变。在本文中,我们将讨论页岩蠕变和其他页岩变形机制,以及如何利用对这些机制的理解来激活尚未接触套管的页岩,以形成井眼屏障。为了更好地理解机械变形过程,我们开发了基于一阶原理的数值模型。我们还通过实验室实验来支持建模结果,然后我们讨论了几个现场案例,在这些案例中,页岩层段已经被激活并验证形成了井障,这是新井建井过程的一部分。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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