地球化学模型在强化地热系统水力增产中的应用

IF 1.5 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Junbeum Lee, E. Chung
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引用次数: 3

摘要

摘要在强化地热系统中,压裂液的使用通常会导致热液储层的地球化学性质发生变化。在本研究中,使用PHREEQC通过地球化学建模来估计地球化学变化,并将建模结果与现场数据进行比较和评估。结果,该模型显示出电导率随时间的增加,这与测量结果一致。从两个结果的比较中发现,注入的水与地下水混合,当流体的水力停留时间超过一天时,地下水的影响显著。此外,基岩地下水的化学性质会对地热储层的地球化学反应产生重大影响。从结果可以得出结论,考虑地下水或地层水的化学性质对于EGS的成功运行至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of geochemical modelling for hydraulic stimulation in enhanced geothermal systems
ABSTRACT In an enhanced geothermal system (EGS), the use of fracking fluid generally causes changes in the geochemical properties of a hydrothermal reservoir. In this study, the geochemical changes were estimated through geochemical modelling using PHREEQC, and the modelling results were compared with field data and evaluated. As a result, the model showed an increase of the electrical conductivity in time which is consistent with the measurements. From the comparison between two results, it was found that the injected water was mixed with groundwater and the influence of the groundwater was significant when the hydraulic retention time of the fluid was longer than a day. Also, the chemical properties of the bedrock groundwater significantly could influence on the geochemical reactions in the geothermal reservoir. From the results, it can be concluded that the consideration of the chemical properties of groundwater or formation water is essential for the successful EGS operation.
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来源期刊
Geosystem Engineering
Geosystem Engineering GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
2.70
自引率
0.00%
发文量
11
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