Arid
报告编号DE2009949970
Numerical Simulation Study of Silica and Calcite Dissolution Around a Geothermal Well by Injecting High pH Solutions with Chelating Agent.
Xu, T; Rose, P; Fayer, S; Pruess, K.
英文摘要Dissolution of silica, silicate, and calcite minerals in the presence of a chelating agent (NTA) at a high pH has been successfully performed in the laboratory using a high-temperature flow reactor. The mineral dissolution and porosity enhancement in the laboratory experiment has been reproduced by reactive transport simulation using TOUGHREACT. The chemical stimulation method has been applied by numerical modeling to a field geothermal injection well system, to investigate its effectiveness. Parameters from the quartz monzodiorite unit at the Enhanced Geothermal System (EGS) site at Desert Peak (Nevada) were used. Results indicate that the injection of a high pH chelating solution results in dissolution of both calcite and plagioclase minerals, and avoids precipitation of calcite at high temperature conditions. Consequently reservoir porosity and permeability can be enhanced especially near the injection well.
英文关键词Injection wells Chelating agents Geothermal fluids Silica Dissolution Simulation Permeability Precipitation
出版年2009
语种英语
国家United States
URLhttp://r.cnki.net/KCMS/detail/detail.aspx?DbCode=KJBG&dbname=KJBGW&filename=59fd668531c97d1d54ae2528
来源机构Technical Information Center Oak Ridge Tennessee
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/273691
推荐引用方式
GB/T 7714
Xu, T,Rose, P,Fayer, S,et al. Numerical Simulation Study of Silica and Calcite Dissolution Around a Geothermal Well by Injecting High pH Solutions with Chelating Agent.,2009.
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