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Reservoir Simulations of Low-Temperature Geothermal Reservoirs.

机译:低温地热油藏的油藏模拟。

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摘要

The eastern United States generally has lower temperature gradients than the western United States. However, West Virginia, in particular, has higher temperature gradients compared to other eastern states. A recent study at Southern Methodist University by Blackwell et al. has shown the presence of a hot spot in the eastern part of West Virginia with temperatures reaching 150°C at a depth of between 4.5 and 5 km. This thesis work examines similar reservoirs at a depth of around 5 km resembling the geology of West Virginia, USA. The temperature gradients used are in accordance with the SMU study.;In order to assess the effects of geothermal reservoir conditions on the lifetime of a low-temperature geothermal system, a sensitivity analysis study was performed on following seven natural and human-controlled parameters within a geothermal reservoir: reservoir temperature, injection fluid temperature, injection flow rate, porosity, rock thermal conductivity, water loss (%) and well spacing. This sensitivity analysis is completed by using ‘One factor at a time method (OFAT)’ and ‘Plackett-Burman design’ methods. The data used for this study was obtained by carrying out the reservoir simulations using TOUGH2 simulator.;The second part of this work is to create a database of thermal potential and time-dependant reservoir conditions for low-temperature geothermal reservoirs by studying a number of possible scenarios. Variations in the parameters identified in sensitivity analysis study are used to expand the scope of database. Main results include the thermal potential of reservoir, pressure and temperature profile of the reservoir over its operational life (30 years for this study), the plant capacity and required pumping power. The results of this database will help the supply curves calculations for low-temperature geothermal reservoirs in the United States, which is the long term goal of the work being done by the geothermal research group under Dr. Anderson at West Virginia University.
机译:美国东部地区的温度梯度通常低于美国西部地区。但是,与其他东部州相比,西弗吉尼亚州尤其具有较高的温度梯度。 Blackwell等人在南方卫理公会大学的最新研究。已显示西弗吉尼亚州东部存在热点,温度达到150°C,深度在4.5至5 km之间。本论文研究了类似于美国西弗吉尼亚州地质的约5 km深度的类似储层。使用的温度梯度与SMU研究一致。为了评估地热储层条件对低温地热系统寿命的影响,对以下七个自然和人为控制参数进行了敏感性分析研究地热储层:储层温度,注入流体温度,注入流量,孔隙率,岩石导热系数,失水率(%)和井距。通过使用“一次一个因素(OFAT)方法”和“ Plackett-Burman设计”方法来完成此敏感性分析。本研究使用的数据是通过使用TOUGH2模拟器进行储层模拟获得的。第二部分工作是通过研究许多地热储层来创建低温地热储层的热势和时间相关储层条件的数据库。可能的方案。在敏感性分析研究中确定的参数的变化用于扩展数据库的范围。主要结果包括储层的热潜能,储层在其使用寿命(本研究为30年)中的压力和温度曲线,电站容量和所需的泵送功率。该数据库的结果将有助于美国低温地热储层的供应曲线计算,这是西弗吉尼亚大学安德森博士领导的地热研究小组所做工作的长期目标。

著录项

  • 作者

    Bedre, Madhur Ganesh.;

  • 作者单位

    West Virginia University.;

  • 授予单位 West Virginia University.;
  • 学科 Engineering Geophysical.;Engineering Chemical.
  • 学位 M.S.Ch.E.
  • 年度 2012
  • 页码 74 p.
  • 总页数 74
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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