1887

Abstract

Carbon dioxide sequestration in deep saline aquifers is being considered as one of the more important geological<br>sequestration types due to the potentially large storage capacity when compared to some other geological sequestration<br>reservoirs. CO2 will react with formation rock when injected in dolomite formations, due to the rock dissolution and<br>precipitation of reaction products permeability may be changed. Several parameters affect these interactions including<br>pressure, temperature, brine composition, CO2 injection rate, and overall injection scheme.

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/content/papers/10.3997/2214-4609-pdb.280.iptc14924_noPW
2012-02-07
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.280.iptc14924_noPW
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