Influence of Permeable Wellbore on Formation Testing While Drilling and Mobility Inversion

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2024-10-09 DOI:10.1155/2024/6711874
Lejun Wu, Ming Chen, Jianxin Liu, Zhiqiang Zhang, Xiaodong Li, Nian Peng, Tianshou Ma
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Abstract

Formation pressure and mobility represent two fundamental parameters that are essential for the development of oil and gas resources. These parameters can be obtained in real time through the process of formation testing while drilling (FTWD). It is highly probable that the drilling fluid will invade the formation during the FTWD process. Nevertheless, the prevailing theory regarding FTWD assumes that the wellbore is impermeable, thereby rendering its potential impact on FTWD and mobility inversion unclear. Therefore, to clarify the influence of the permeable wellbore on FTWD and mobility inversion, a mathematical model of FTWD seepage was first proposed by involving the permeable wellbore. Secondly, the finite element method was used to solve this model, and this model was verified by using the analytical models. The pressure response curves and isobaric surface near the FTWD probe were then compared for both the permeable and impermeable wellbores, and the influence of the permeable wellbore on the pressure response curves of FTWD was analyzed. Finally, the method of integral area was used to invert mobility, and the compressive influence of different factors on both the pressure response curves and mobility inversion was discussed for both the permeable and impermeable wellbores. The results indicated that the permeable wellbore has a significant impact on the pressure response curves and isobaric surface near the probe due to the limited pressure sweeping range around the probe and the invasion of drilling fluid. In the case of a permeable wellbore, the invasion of the drilling fluid into the formation can cause a supercharge effect around the well. This effect can cause an initial increase followed by a decrease in the pressure buildup phase. The pressure buildup always exceeds the original formation pressure, which can lead to an overestimation of the measured formation pressure compared to the original. Meanwhile, the permeable wellbore can also lead to an overestimation of the inversion mobility, but the impermeable wellbore has much less influence on the mobility inversion. To improve inversion accuracy, it is recommended to increase the rubber packer radius, lengthen the suction period, reduce the storage volume of the pipeline, and decrease the overbalanced pressure. However, these measures cannot mitigate the impact of the supercharge effect on formation pressure testing. This paper provides theoretical guidelines for the use of FTWD tools and data interpretation.

渗透井筒对钻井时地层测试和流动性反演的影响
地层压力和流动性是开发油气资源必不可少的两个基本参数。这些参数可以通过钻井过程中的地层测试(FTWD)实时获得。在 FTWD 过程中,钻井液极有可能侵入地层。然而,有关 FTWD 的主流理论认为井筒是不渗透的,因此不清楚其对 FTWD 和流动性反演的潜在影响。因此,为了明确渗透井筒对 FTWD 和流动性反演的影响,首先提出了一个涉及渗透井筒的 FTWD 渗流数学模型。其次,采用有限元法对该模型进行求解,并利用分析模型对该模型进行验证。然后,比较了渗透井筒和不渗透井筒的 FTWD 探头附近的压力响应曲线和等压面,分析了渗透井筒对 FTWD 压力响应曲线的影响。最后,使用积分面积法对流动性进行反演,讨论了不同因素对渗透井筒和不渗透井筒的压力响应曲线和流动性反演的压缩影响。结果表明,由于探头周围的压力扫描范围有限以及钻井液的侵入,渗透井筒对探头附近的压力响应曲线和等压面有很大影响。在渗透井筒的情况下,钻井液侵入地层会在井周围产生超充效应。这种效应会在压力积累阶段造成先上升后下降的情况。压力积累总是超过原来的地层压力,这可能导致测得的地层压力比原来的压力高估。同时,渗透井筒也会导致高估反演流动性,但不渗透井筒对流动性反演的影响要小得多。为了提高反演精度,建议增大橡胶封隔器半径、延长抽吸周期、减小管道存储量、降低过平衡压力。然而,这些措施并不能减轻超充效应对地层压力测试的影响。本文为 FTWD 工具的使用和数据解释提供了理论指导。
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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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