Permeability and Flow Field Evolution Due to Dissolution of Calcite in a 3-D Porous Rock Under Geothermal Gradient and Through-Flow

Author:

Sandeep V. R.,Chaudhuri Abhijit,Kelkar Sharad

Publisher

Springer Science and Business Media LLC

Subject

General Chemical Engineering,Catalysis

Reference22 articles.

1. Andre, J.B., Rajaram, H.: Dissolution of limestone fractures by cooling waters: early development of hypogene karst systems. Water Resour. Res. 41, W01015 (2005)

2. Bear, J.: Dynamics of Fluids in Porous Media. American Elsevier, New York (1972)

3. Bear, J., Cheng, A.H.-D.: Modeling Groundwater Flow and Contaminant Transport. Springer, New York (2010)

4. Chaudhuri, A., Rajaram, H., Viswanathan, H., Zyvoloski, G., Stauffer, P.: Buoyant convection resulting from dissolution and permeability growth in vertical limestone fractures. Geophys. Res. Lett. (2009). doi: 10.1029/2008GL036533

5. Chaudhuri, A., Rajaram, H., Viswanathan, H.: Early-stage hypogene karstification in a mountain hydrologic system: a coupled thermo-hydro-chemical model incorporating buoyant convection. Water Resour. Res. (2013). doi: 10.1002/wrcr.2042

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