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<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" altimg="si5.gif" display="inline" overflow="scroll"><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:math> mineral sequestration: physically activated dissolution of serpentine and pH swing process

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Serpentinite Carbonation for CO2 Sequestration

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Dissolution kinetics of chrysotile at pH 7 to 10

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Microbially mediated mineral carbonation: Roles of phototrophy and heterotrophy

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Chapter 1. CONTINUUM FORMULATION OF MULTICOMPONENT-MULTIPHASE REACTIVE TRANSPORT

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CHAPTER 4. TRANSITION STATE THEORY

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Subarctic Weathering of Mineral Wastes Provides a Sink for Atmospheric CO₂

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Chapter 9. CHEMICAL WEATHERING RATES OF SILICATE MINERALS IN SOILS

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Chapter 8. CHEMICAL WEATHERING OF SILICATES IN NATURE: A MICROSCOPIC PERSPECTIVE WITH THEORETICAL CONSIDERATIONS

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