多学科方法优化页岩开采的表征和完井过程

C. Carpenter
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引用次数: 0

摘要

本文由 JPT 技术编辑 Chris Carpenter 撰写,收录了 URTeC 3871303 号论文 "在阿科马盆地伍德福德页岩油气区采用多学科方法进行储层和完井优化 "的要点,作者为 Stephen C. Zagurski(SPE)、Steve Asbill(SPE)、Foundation Energy Management 以及 Christopher M. Smith(Advanced Hydrocarbon Stratraph)等。该论文未经同行评审。 与外围前陆盆地的形成有关的地下复杂性会对非常规资源的开发产生重大影响。在俄克拉荷马州东南部的阿科马盆地,在盆地形成过程中,推力和构造荷载的开始诱发了一系列复杂的倾覆/滑动和走向/滑动断层。作业者利用一系列技术加深了对储层及其危害的了解,并对未来开发计划和战略的经济影响有了深刻的认识。 伍德福德(Woodford)主要属于第二类角质源岩。该地层通常被划分为硅质泥岩或樱桃粉砂岩。盆地内不同的热成熟度使伍德福德处于湿气相和干气相窗口(在盆地内由西向东移动)。阿科马盆地内复杂的断层体系为伍德福德的水平开发增加了一层复杂性。作业者希望通过最近在富液航道上的一个开发单元,进一步了解伍德福德以及断层对储层的影响。该开发单元由一口现有的母井(X 井)和一对子井(Y 井和 Z 井)组成。XYZ 单元的背景始于母井 X 在填充开发 4-6 年前完工。在盆地的这一部分,X 井的初始生产率和迄今为止的累计生产量都位居油井的前 25%。井筒受到一对断层的影响,钻井位置位于伍德福德上半段。与大多数母井相比,X 井的位置更靠东,因为它距离单元边界约 1,600 英尺。这就限制了填充开发,只能打两口井,而不是三口井;阿科马油气区每个区段通常有四口井的间距,有时甚至有五口井的间距。计划在 X 井以东钻探 Y 井和 Z 井,井距为 1,100-1,600 英尺。由于地表位置的限制以及地表套管与着陆点之间的实际垂直深度(TVD)有限,该单元的井距略有受阻。单元内结构的复杂性部分影响了单元的填充开发。具体而言,Y井及其横向长度被缩短。在阿科马的这一部分,断层产水量通常是油井运营支出中权重最高的变量。因此,限制 XYZ 单元及周边地区过量产水的能力至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multidisciplinary Approach Optimizes Characterization, Completion in Shale Play
This article, written by JPT Technology Editor Chris Carpenter, contains highlights of paper URTeC 3871303, “Using a Multidisciplinary Approach to Reservoir and Completion Optimization Within the Woodford Shale Play of the Arkoma Basin,” by Stephen C. Zagurski, SPE, and Steve Asbill, SPE, Foundation Energy Management, and Christopher M. Smith, Advanced Hydrocarbon Stratigraphy, et al. The paper has not been peer reviewed. Subsurface complexities related to the formation of peripheral foreland basins can have significant effects on unconventional resource development. In the Arkoma Basin of southeast Oklahoma, the onset of thrusting and tectonic loading induced a complex series of dip/slip and strike/slip faults during basin formation. The operator used a series of technologies to increase understanding of the reservoir and its hazards and provide insight into economic implications for future development plans and strategies. The Woodford is primarily a Type II kerogen source rock. The formation typically is classified as either siliceous mudstone or cherty siltstone. Variable thermal maturity across the basin places the Woodford in both the wet-gas and dry-gas phase windows (moving west to east across the basin). Complex faulting regimes within the Arkoma add a layer of complexity to horizontal development of the Woodford. The operator wanted to increase the understanding of the Woodford and the effects of faulting through the reservoir in a recent development unit in the liquids-rich fairway. The development unit consists of an existing parent well (Well X) and a pair of child wells (Well Y and Well Z). The background of Unit XYZ begins with the completion of parent Well X 4–6 years before infill development. In this portion of the basin, Well X’s initial production rate and its cumulative production to date rank it in the top 25% of wells. The wellbore is subjected to a pair of faults and was drilled in the upper half of the Woodford. Placement of Well X is substantially further east than most parent wells because it is approximately 1,600 ft from the unit boundary. This limited infill development to two wells instead of three; the Arkoma typically has seen spacing of four, and sometimes five, wells per section. Wells Y and Z were planned and drilled east of Well X with 1,100–1,600 ft of well spacing. Well spacing in the unit was slightly hindered by surface location limitations and limited true vertical depth (TVD) between surface casing and landing point. Structural complexity within the unit partially impaired infill development of the unit. Specifically, Well Y and its lateral length was shortened. In this portion of the Arkoma, fault-derived water production typically is the highest-weighted variable in a well’s operating expenditure. Thus, the ability to limit excess water production within Unit XYZ and the surrounding acreage is of paramount importance.
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