包括5年累积在内的多次流动/累积测试分析:以澳大利亚页岩气井为例

C. Clarkson, Alexander Côté
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引用次数: 2

摘要

对页岩储层中完成的多裂缝水平井(MFHWs)进行长期(多年)建井测试,为研究和分析典型建井测试周期中不常见的流态序列提供了独特的机会。在这项研究中,对澳大利亚Beetaloo盆地页岩气储层中完成的MFHW进行了两次积累期(包括罕见的近5年的积累期)和之前的延长流动测试。分析的目的是:(a)确定每个试验(流动/积聚,F/BU)期间观察到的流动状态的顺序;(b)储层渗透率和水力裂缝性质的提取估计;(c)研究这些性质在每次后续试验中的演变。对澳大利亚Velkerri B页岩中完成的Amungee NW-1H MFHW进行了分析。由于套管变形和无法磨铣桥塞,大部分流量来自井的跟段。第一个F/BU阶段从2016年到2021年进行(近5年的建设),而第二个F/BU于2021年启动(目前仍在继续建设)。累积之前的延长(>1个月)生产测试(ept)使用速率瞬态分析(RTA)方法(流态识别/直线/型曲线分析(TCA))进行分析,该方法针对页岩气性质(如解吸)进行了改进,而累积则使用经典的压力瞬态分析(PTA)方法进行分析。第一个(~5年)积累周期(BU 1)表现为双线性-线性-椭圆-伪径向流动,然后是第二个线性流动周期。前两种流动形式被解释为与裂缝间流动有关,而后一种流动形式被认为与井内的线性流动相对应。由于解释了相对较短的裂缝半长(对应于裂缝的高导流部分),裂缝周围的椭圆/径向流可以合理地发生。渗透率估算值与诊断性裂缝注入试验(DFIT)分析结果吻合良好。其他测试期(EPT 1和2,BU 2)的流型解释基本一致,尽管EPT 1的流型解释受到噪声数据的挑战。ept 1和ept 2的渗透率值小于累积测试,表明压降引起应力敏感性。bu1和bu2的性质分析结果非常一致,表明由储层参数应力敏感性引起的任何影响在很大程度上是可逆的。所有测试得出的渗透率都比实验室数据大得多,因此可以解释天然裂缝正在提高系统渗透率。裂缝半长也比通常报道的MFHWs短得多。该油田获得的测试数据几乎都是教科书级别的,再加上测试周期的长度,得出了页岩气储层中MFHW最完整的流态序列之一。在所有测试阶段都观察到一个径向流动周期(被解释为裂缝间径向流动),这使得我们可以对每次后续测试中的储层渗透率/皮肤及其演变进行可靠的估计,而这方面的报道很少。径向流导出的渗透率,结合早期的线性流分析,还可以估算出所有测试的裂缝半长。该案例研究大大增加了我们对页岩气储层特征和与MFHWs相关的流态序列的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of Multiple Flow/Buildup Tests Including a 5-year Buildup: Case Study of an Australian Shale Gas Well
Long-term (multiyear) buildup tests conducted for multifractured horizontal wells (MFHWs) completed in shale reservoirs offer the unique opportunity to study and analyze flow-regimes sequences that are not commonly observed with typical buildup test periods. In this study, two buildup periods (including a rarely observed, nearly 5-year buildup), and the preceding extended flow tests, were analyzed for an MFHW completed in an Australian shale gas reservoir within the Beetaloo Basin. The objectives of the analyses were to (a) identify the sequence of flow regimes observed for each test (flow/buildup, F/BU) period; (b) extract estimates of reservoir permeability and hydraulic fracture properties; and (c) study the evolution of these properties with each subsequent test. An MFHW, the Amungee NW-1H, completed in the Velkerri B shale in Australia, was analyzed. Due to a casing deformation and inability to mill out plugs beyond this, most of the flow contribution was from the heel stages of the well. The first F/BU period was conducted from 2016 to 2021 (a nearly 5-year buildup), while the second F/BU was initiated in 2021 (buildup is currently continuing). The extended (>1 month) production tests (EPTs) preceding the buildups were analyzed using rate-transient analysis (RTA) methods [flow-regime identification/straightline /type curve analysis (TCA)] modified for shale gas properties (e.g., desorption), while the buildups were analyzed using classic pressure-transient analysis (PTA) methods. The first (~5-year) buildup period (BU 1) revealed a sequence of bilinear-linear-elliptical-pseudoradial flow followed by a second linear flow period. The first two flow regimes are interpreted to be associated with interfracture flow, while the latter is assumed to correspond to linear flow to the well. Elliptical/radial flow around fractures is rationalized to occur due to interpreted relatively short fracture half-lengths (corresponding to the high-conductivity portion of the fractures). Permeability estimates are in good agreement with diagnostic fracture injection test (DFIT) analysis. Flow-regime interpretations for the other test periods (EPTs 1 and 2, BU 2) are largely consistent, although EPT 1 flow-regime interpretation was challenged by noisy data. Permeability values derived from EPTs 1 and 2 are smaller than from buildup tests, suggesting stress sensitivity caused by drawdown. Properties derived from the analysis of BU 1 and 2 are in good agreement, suggesting that any effects caused by stress sensitivity of reservoir parameters are largely reversible. Permeability derived from all tests are much larger than those obtained from laboratory data, leading to the interpretation that natural fractures are elevating system permeability. Fracture half-lengths are also much shorter than those typically reported for MFHWs. The mostly “textbook” quality well test data obtained for this field example, combined with the length of the test periods, resulted in one of the most complete flow-regime sequences observed for an MFHW completed in a shale gas reservoir. The existence of a radial flow period observed for all test periods (interpreted to be interfracture radial flow) allows for confident estimates of reservoir permeability/skin and their evolution with each subsequent test, which is rarely reported. The radial-flow-derived permeability, combined with early linear flow analysis, also allowed fracture half-length to be estimated for all tests. This case study adds significantly to our understanding of shale gas reservoir characteristics and flow-regime sequences associated with MFHWs.
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