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Aluminosilicate Dissolution And Silicate Carbonation During Geologic Co2 Sequestration, Yujia Min
Aluminosilicate Dissolution And Silicate Carbonation During Geologic Co2 Sequestration, Yujia Min
McKelvey School of Engineering Theses & Dissertations
Geologic CO2 sequestration (GCS) is considered a promising method to reduce anthropogenic CO2 emission. Assessing the supercritical CO2 (scCO2)¬–gas or liquid phase water (g, l)–mineral interactions is critical to evaluating the viability of GCS processes. This work contributes to our understanding of geochemical reactions at CO2¬–water (g, l)–mineral interfaces, by investigating the dissolution of aluminosilicates in CO2-acidified water (l). Plagioclase and biotite were chosen as model minerals in reservoir rock and caprock, respectively. To elucidate the effects of brine chemistry, first, the influences of cations in brine including Na, Ca, and K, have been investigated. In addition to the cations, …
Calcium Carbonate Formation In Energy-Related Subsurface Environments And Engineered Systems, Qingyun Li
Calcium Carbonate Formation In Energy-Related Subsurface Environments And Engineered Systems, Qingyun Li
McKelvey School of Engineering Theses & Dissertations
Geologic CO2 sequestration (GCS) in subsurface saline aquifers is a promising strategy to mitigate climate change caused by increasing anthropogenic CO2 emissions from energy production. At GCS sites, interactions between fluids and geomedia are important because they can affect CO2 trapping efficiency and the safety of CO2 storage. These interactions include the dissolution and precipitation of minerals. One of the most important minerals is calcium carbonate, because it can permanently trap CO2.
In this work, Portland cement was used as a model geomedium to investigate the chemical reactions, mechanical alterations, transport of reactive fluids, and the interplay of all these …