Abstract
A portion of this research was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences. The Center for Frontiers of Subsurface Energy Security (CFSES) is a DOE Energy Frontier Research Center, under Contract No. DE-SC0001114. The authors gratefully acknowledge the financial support provided by the NSF-CDI under contract number DMS 0835745 and King Abdullah University of Science and Technology (KAUST)-AEA-UTA08-687. The last author is supported by Award no. KUSF1-032-04, made by KAUST.
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