Production Forecasting of Unruly Geoenergy Extraction Wells Using Gaussian Decline Curve Analysis

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-09-28 DOI:10.1155/2023/5534305
Ruud Weijermars
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引用次数: 0

Abstract

Fast and rigorous well performance evaluation is made possible by new solutions of the pressure diffusion equation. The derived Gaussian pressure transient (GPT) solutions can be practically formulated as a decline curve analysis (DCA) equation for history matching of historic well rates to then forecast the future well performance and estimate the remaining reserves. Application in rate transient analysis (RTA) mode is also possible to estimate fracture half-lengths. Because GPT solutions are physics-based, these can be used for production forecasting as well as in reservoir simulation mode (by computing the spatial and temporal pressure gradients everywhere in the reservoir section drained by either an existing or a planned well). The present paper focuses on the physics-based production forecasting of so-called “unruly” wells, which at first seem to have production behavior noncompliant with any DCA curve. Four shale wells (one from the Utica, Ohio; one from the Eagle Ford Formation, East Texas; and two from the Wolfcamp Formation, West Texas) are analyzed in detail. Physics-based adjustments are made to the Gaussian DCA history matching process, showing how the production rate of these wells is fully compliant with the rate implied by the hydraulic diffusivity of the reservoir sections where these wells drain from.
利用高斯递减曲线分析预测不规则地能采油井产量
压力扩散方程的新解使快速、严格的井况评价成为可能。推导出的高斯压力瞬态(GPT)解实际上可以表示为递减曲线分析(DCA)方程,用于历史井率的历史匹配,从而预测未来井的动态并估计剩余储量。应用于速率瞬态分析(RTA)模式也可以估计裂缝半长。由于GPT解决方案是基于物理的,因此既可以用于产量预测,也可以用于油藏模拟模式(通过计算现有井或计划井排出的油藏段各处的空间和时间压力梯度)。本文的重点是对所谓的“不稳定”井进行基于物理的产量预测,这些井的生产行为起初似乎不符合任何DCA曲线。4口页岩井(1口来自俄亥俄州尤蒂卡;一个来自德克萨斯州东部的鹰福特地层;以及来自德克萨斯州西部沃尔夫坎普组的两个)进行了详细分析。对高斯DCA历史匹配过程进行了基于物理的调整,显示了这些井的产量如何完全符合这些井所处油藏段的水力扩散率所隐含的速率。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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