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Geochemical Clogging in Carbonate Mineralization on Carbon Dioxide Sequestration / 二酸化炭素地中貯留における炭酸塩鉱物の沈殿現象に関する地化学的研究Yoo, Seung Youl 24 September 2012 (has links)
Kyoto University (京都大学) / 0048 / 新制・課程博士 / 博士(工学) / 甲第17131号 / 工博第3621号 / 新制||工||1550(附属図書館) / 29870 / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 松岡 俊文, 教授 大津 宏康, 准教授 水戸 義忠 / 学位規則第4条第1項該当
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Synthesis of Amphiphilic α- and γ-AApeptides for Antimicrobial, Self-Assembly, and Mineralization StudiesAmin, Mohamad N. 01 January 2013 (has links)
Seven novel, amphiphilic AApeptides were prepared. Two cationic, lipo-α-AApeptides, NA-75 and NA-77 were found to possess potent antimicrobial activity against Gram-positive bacteria, with almost no hemolytic activity. In addition to NA-75 and 77, four amphiphilic, γ-AApeptides, NA-133, 135, 137, and 139, and one anionic lipo-α-AApeptide, NA-81, were prepared for molecular self-assembly studies, with several interesting nanostructures observed by TEM. Mineralization of calcium carbonate from gaseous CO2 and Ca2+ in the presence of the 7 AApeptide amphiphiles was also observed by optical microscopy. Several AApeptides were found to be able to influence CaCO3 crystal morphology. Another α-AApeptide, NA-63, was synthesized by a novel, alternative method, which has several potential advantages over the previous synthesis methods.
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Carbon Sequestration Potential in Simulated Saline Lake WatersYurman, Scott N 06 May 2012 (has links)
This investigation tested simulated saline lake environments as mineralization sites for sequestering anthropogenic CO2. Four unique saline lakes were simulated in the laboratory. Two sets of experiments were conducted by diffusing CO2(g) through each simulated lake over 30 days. The first set tested the carbonate system response to elevated CO2(g). The second set of experiments replicated the same process but used ammonium hydroxide to elevate pH. Water samples were collected daily to test for cation loss via mineralization. Rapid mineralization occurred with the pH enhancer and cation activity was greatly reduced by as much as 38,000 mg/L Ca due to precipitation. This resulted in a mass of 100,000 mg/L of CO2 being sequestered via Ca and Mg-carbonate mineralization. With proper geochemical conditions, saline lake environments can therefore potentially serve a purpose in sequestering CO2(g).
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