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Collab Fracture Characterization: Preliminary Results from the Modeling and Flow Testing of Experiment 1

机译:协同断裂表征:实验1的建模和流动测试的初步结果

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The EGS Collab project is developing ~10-20 m-scale field sites where fracture stimulation and flow models can be validated against controlled, small-scale, in-situ experiments. At the first experimental site, a hydraulic fracture will be created in metamorphic rock at the 4850 level in the former Homestake Mine. The experimental concept is for fracturing to be initiated at an injection well and continue until it intersects a production well approximately 10 meters away. Initial step-pressure flow testing of the fracture are to be performed to describe pressure-aperture-flow relationships. The flow field between the injector and producer boreholes will be characterized using a series of forced gradient dipole tracer tests. A number of fracture characterization models have been used to assist in the design of the tracer tests. The tracer test program will use conservative, sorbing, and particulate tracers, as well as sampling for radon gas to describe the fracture surface area (i.e., potential heat transfer area), flow pathway distribution, and volume. Tracer concentration at the production well (i.e. break through curves) will be measured using a series of inline sensors, liquid sampling devices, filtering of the effluent, and the measuring of gas concentrations in the effluent. Tracer monitoring data will be compared against results from a collection of numerical simulators developed at U.S. national laboratories and universities for the purpose of validating these flow and transport models. Ultimately these same models will be used to predict the heat transfer characteristics of the fracture and will be compared to a thermal characterization field test where cold water will be injected at the injection well and the temperature will be measured at the production well. This paper discusses the early tracer transport model predictions and parameters sensitivity that affect the tracer breakthrough curves at the production well.
机译:EGS Collab项目正在开发约10-20 m规模的现场,可以通过受控的小规模现场实验验证裂缝的刺激和流动模型。在第一个实验点,将在原霍姆斯特克矿的4850级变质岩中产生水力压裂。实验概念是在注入井处开始压裂,并继续进行直到与相距约10米的生产井相交为止。应对裂缝进行初始的阶跃压力流测试,以描述压力-孔-流的关系。注入井和生产井之间的流场将通过一系列强制梯度偶极示踪剂测试来表征。许多裂缝特征模型已用于协助示踪剂测试的设计。示踪剂测试程序将使用保守示踪剂,吸附剂和颗粒示踪剂,并对sampling气取样以描述裂缝的表面积(即潜在的传热面积),流路分布和体积。将使用一系列在线传感器,液体采样设备,废水过滤以及废水中气体浓度的测量来测量生产井中的示踪剂浓度(即突破曲线)。示踪剂监测数据将与美国国家实验室和大学开发的一系列数字模拟器的结果进行比较,以验证这些流量和运输模型。最终,这些相同的模型将用于预测裂缝的传热特性,并将其与热特性现场测试进行比较,在现场测试中,将在注入井处注入冷水,并在生产井处测量温度。本文讨论了影响生产井中示踪剂穿透曲线的早期示踪剂传输模型预测和参数敏感性。

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