基于等效渗流通道模型的地热尾水回灌理论模型  被引量:14

Theoretical model of geothermal tail water reinjection based on the equivalent flow channel model

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作  者:赵志宏[1] 刘桂宏[1,2] 谭现锋 张平平 

机构地区:[1]清华大学土木工程系,北京100084 [2]中国矿业大学力学与建筑工程学院,江苏徐州221116 [3]中国地质大学(武汉)工程学院,湖北武汉430074 [4]山东省鲁北地质工程勘察院,山东德州253072

出  处:《水文地质工程地质》2017年第3期158-164,共7页Hydrogeology & Engineering Geology

基  金:国家自然科学基金项目(51509138);北京市自然科学基金项目(8152020);北京市优秀人才培养资助(201400002012G115)

摘  要:深层地热能是一种清洁环保的可再生能源,尾水回灌是深层地热可持续开发利用的重要保证,但目前国内地热尾水回灌还处在起步阶段,地热尾水回灌方案优化设计的理论模型尚不成熟。文章结合示踪试验,提出了基于等效渗流通道模型的热储参数反演与开采井热突破预测的完整理论框架。应用多孔介质溶质运移理论,修正了等效渗流通道中的溶质浓度解析解,并联合移动渐近线法提出了热储参数反演理论模型;推导了等效渗流通道中的对流传热解析模型,可对开采井中的水温变化进行预测。依托山东省德州市平原县魏庄社区地热对井示踪试验,应用该理论框架进行了示踪试验反演及开采井热突破预测,并对影响开采井热突破的主要因素进行了敏感性分析。Deep geothermal resources are clean, environmentally friendly and renewable, and geothermal tail water reinjection plays an important role in the sustainable management of deep geothermal reservoirs. However, the progress of geothermal tail water reinjection is slow in China, and theoretical models guiding geothermal tail water reinjection is still under development. Based on tracer tests and equivalent flow channel models, this study proposes a theoretical modeling framework in order to back-calculate the unknown parameters of geothermal reservoirs and predict the thermal breakthrough in the production well. The inverse modeling module combines the analytical solution of the tracer transport equation with the method of moving asymptotes, and an analytical model considering heat advection and transfer can be used to predict the thermal breakthrough in the production well. Based on the results of tracer tests in the double geothermal wells near Dezhou of Shandong, two equivalent flow channels were determined and their average flow velocity, dispersion coefficient, section area and channel length are estimated by using this theoretical framework. The possible thermal breakthrough in the production well and its main influencing factors are also discussed.

关 键 词:尾水回灌 砂岩热储 示踪试验 参数反分析 热突破 

分 类 号:P314.1[天文地球—固体地球物理学]

 

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