A coupled geothermal model of the Alpokalja area, Hungary—Austria

A. Kovács, Á. R. Szalkai, Zsolt Kercsmár, T. Cserny
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引用次数: 0

Abstract

A coupled groundwater flow and heat transport model was developed for a trans-boundary geothermal reservoir located in the Alpokalja area. The study area lies in the western part of the Pannonian Basin, at the border between Hungary and Austria. The study area contains several famous geothermal water utilizations on both sides of the border, which has an impact on natural groundwater conditions. The aim of the modeling study was to evaluate the natural-state and production-state groundwater conditions, and to make predictions on cross-boundary interferences. A three-dimensional finite element-type coupled geothermal model was constructed to provide a coherent quantitative representation of geothermal flow systems. The model described the hydraulic behavior of the flow system, the interaction between different reservoirs, and geothermal conditions.
匈牙利-奥地利Alpokalja地区的耦合地热模型
建立了位于Alpokalja地区的跨界地热储层的地下水流-热输运耦合模型。研究区位于潘诺尼亚盆地的西部,匈牙利和奥地利之间的边界。研究区边界两侧有几个著名的地热水利用区,这些地热水利用区对天然地下水条件有影响。模拟研究的目的是评估自然状态和生产状态的地下水条件,并对跨界干扰进行预测。建立了三维有限元型耦合地热模型,为地热流系统提供了连贯的定量表征。该模型描述了流体系统的水力特性、不同储层之间的相互作用以及地热条件。
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来源期刊
Central European Geology
Central European Geology Earth and Planetary Sciences-Geology
CiteScore
1.40
自引率
0.00%
发文量
8
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