采集、分析和整合井筒测井资料,以表征裂缝性地热储层:以法国rittershoffen为例

G. Sosio, Schlumberger, A. Mandiuc, A. Campana, J. Vidal, R. Hehn, C. Baujard, GéoPlusEnvironnement, És Géothermie
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引用次数: 0

摘要

ECOGI项目位于里特肖芬(法国东部阿尔萨斯)的一个深层地热双峰中,为一家工业工厂生产热能。GRT-1和GRT-2这两口井的目标是在地表以下2000米深度的Buntsandstein沉积物和花岗岩基底附近的一个大正断层附近的局部天然裂缝区。通过电缆测井,对两口井进行了广泛的测量。压力和温度测井、核测井(密度和孔隙度)、电阻率测井、偶极声波测井和井筒图像测井均在目标裂缝含水层和部分覆盖层的裸眼中进行。这些测井数据经过处理和解释,建立了一个完整的现场模型,描述了其地质特性,特别是裂缝网络,流体和热流的动态行为,以及地质力学特性。声学成像仪的井筒成像结果被解释为了解天然裂缝网络的几何形状,这是Rittershoffen地热系统的主要流体通道。结果与温度测井相结合,以了解哪些裂缝是张开的,从而在钻井泥浆侵入时冷却。利用密度测井和声波测井推导出近井岩石的力学特性和应力大小;通过对井筒图像中钻井诱发特征的解释,可以确定作用于井筒的局部应力的方向。利用所获得的地质力学模型预测了沿井发生的力学或水力失稳,并将预测结果与井中实际观察到的事件进行了比较,验证了地质力学模型的有效性。以井为中心的裂缝和地质力学分析结果被整合到三维储层模型中,用于了解现场地热作业的性能和风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ACQUISITION, ANALYSIS, AND INTEGRATION OF WELLBORE LOGS TO CHARACTERIZE A FRACTURED GEOTHERMAL RESERVOIR: THE CASE OF RITTERSHOFFEN, FRANCE
The Exploitation de la Chaleur d’Origine Géothermique pour l’Industrie (ECOGI) site lies in a deep geothermal doublet in Rittershoffen (Alsace, Eastern France), producing heat for an industrial plant. The two wells, GRT-1 and GRT-2, targeted local natural fracture zones in the vicinity of a large normal fault across the Buntsandstein sediments and the granitic basement at a depth of 2,000 m below surface. An extensive measurement campaign was carried out in both wells by means of wireline logging. Pressure and temperature logs, nuclear logs (density and porosity), resistivity logs, dipole sonic logs, and wellbore image logs were acquired in the open hole over the target fractured aquifer and partially across the overburden. These logs were processed and interpreted to build an integrated model of the site, describing its geological properties, notably the fracture network, its dynamic behavior in terms of fluid and heat flow, and its geomechanical properties. Wellbore imaging results from acoustics imagers were interpreted to understand the geometry of the natural fracture network, which acts as the main fluid pathway in the Rittershoffen geothermal system. The results were integrated with temperature logging to understand which fractures were open and therefore cooling down when invaded by the drilling mud. Density and sonic logs were used to derive the mechanical properties of the near-wellbore rock and the stress magnitudes; the interpretation of drilling-induced features in the wellbore images allowed determining the orientation of the local stress acting on the wellbore. The geomechanical model obtained was used to predict the occurrence of mechanical or hydraulic instability along the well and compare the prediction with the events actually observed in the well, providing a validation of the geomechanical model. The results of well-centric fracture and geomechanical analysis were integrated in a 3D reservoir model and used to understand the performance and the risks associated with geothermal operations at the site.
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