通过数值模拟和现场实测观测研究了井筒-裂缝分离对温度测井解释的影响

A. M. Khan, Abdullah Binziad, Abdullah Alsubaii
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摘要

温度测井是一种基于冷却异常来量化裂缝高度的老技术。在压裂后的测量中经常观察到温度异常。造成这些异常的原因之一是井筒与裂缝的不对中,这取决于井筒的几何形状和优先裂缝面。为了避免对裂缝高度的误解,本文进行了系统的研究。两种数学工具相结合:(1)井筒周围三维空间的几何分辨率;(2)以无因次形式求解传热偏微分方程(PDE)的数值格式,以模拟井筒周围的温度演变。最后,对这些发现进行了测试,并与深部热碎屑储层的几个现场案例进行了验证。温度测井分三次进行,用于斜度井的解释。第一个工具利用井筒斜度、井筒方位角和裂缝方位角来解析三维空间中的相对位置和详细几何形状。对于给定的一组输入,该工具可以获得与井筒一致的总裂缝高度的百分比。然后将输出与带有显式有限差分代码的数值工具耦合,以在给定几何空间的适当边界条件下求解成角/分离裂缝的相关PDE。结果表明,裂缝离井筒越远,如果压裂后不久进行温度测井,则越难以观察到冷却过程。通过现场测量和模型验证,延迟温度通道可以使冷锋从裂缝向井筒移动,是捕获冷却时间的可行解决方案。现场实例显示了一些复杂的温度行为,从建模工具中得到的理解有助于解释异常趋势。讨论了构造伪温度测井的可能性,减少了通过次数,并将该方法扩展到多种应用。这种创新的方法避免了在斜度井中出现裂缝遏制错误指示的陷阱。它可用于提高高分辨率温度测井资料的实用性,提高效率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Implications of Wellbore-Fracture Separation on Temperature Log Interpretation Studied Through Numerical Modeling and Field Measurements and Observations
Temperature logging is an old technique that quantifies fracture height based on cooldown anomalies. Warm anomalies are very frequently observed in post-fracturing measurements. One of the reasons for these anomalies is misalignment of the wellbore with the fracture, which depends on the geometry of wellbore and preferential fracture plane. A systematic study is presented here to avoid misinterpretation of fracture height. Two mathematical tools were coupled: (1) a geometrical resolution of the 3D space around the wellbore and (2) a numerical scheme solving the heat transfer partial differential equation (PDE) in dimensionless form to simulate temperature evolution around the wellbore. Finally, the findings were tested and corroborated with a few field cases in deep, hot, clastic reservoirs. The temperature log was conducted with three passes and was used for interpretation in deviated wellbores. The first tool utilized the wellbore deviation, wellbore azimuth, and fracture azimuth to resolve the relative positions and detailed geometry in 3D space. The tool yielded the fraction of total fracture height that will be coincident with the wellbore for a given set of inputs. The outputs were then coupled with the numerical tool with an explicit finite difference code to solve the relevant PDE with appropriate boundary conditions for the given geometrical space for the angled/separated fracture. The results showed that the further the fracture separates from wellbore, the more difficult it is to observe cooldown if the temperature logging is conducted soon after fracturing. Delaying the temperature passes allows the cold front from fracture to move towards wellbore and is a viable solution to capture cooldown, as seen from field measurements and validated by the model. The field cases demonstrated some complicated temperature behaviors, and the understanding developed from the modeling tools aided in interpreting the anomalous trends. The possibility of constructing pseduo temperature logs, lowering the number of passes, and extending the approach for multiple applications is discussed. The innovative approach avoids pitfalls of false indications of fracture containment in deviated wells. It can be used to improve the utility of high-resolution temperature logging data to enhance efficiency.
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