1887

Abstract

After CO2 is injected into a deep underground saline formation, the initial geochemical equilibrium state is changed, and a series of geochemical reactions between CO2, the pore fluid and the minerals present is initiated. Most of these geochemical reacti

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/content/papers/10.3997/2214-4609.20144118
2011-11-08
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20144118
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