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Abstract: Coupled hydrologic and reactive transport modeling reveal influences of porosity change and resulting geochemical distinctions across brine-to-freshwater transitions (AGU25)

Coupled hydrologic and reactive transport modeling reveal influences of porosity change and resulting geochemical distinctions across brine-to-freshwater transitions

Sarah Virginia McKnight1, Lee Munk2, Xingyuan Chen3, Glenn E Hammond3, David F Boutt4, Matthew Winnick4, Zhi Li3, Peishi Jiang3, Faria T Zahura5, Bing Li6, Tasneem Ahmadullah7, Sundar Niroula5, Jiawei Fan8 and Yi Xiao5, (1)University of Dayton, Department of Geology and Environmental Geosciences, Dayton, United States, (2)University of Alaska Fairbanks, Department of Geosciences, Fairbanks, United States, (3)Pacific Northwest National Laboratory, Richland, United States, (4)University of Massachusetts, Earth, Geographic, and Climate Sciences, Amherst, United States, (5)Pacific Northwest National Laboratory, Richland, WA, United States, (6)PNNL, Beijing, China, (7)Pacific Northwest National Laboratory, Environmental Molecular Sciences Laboratory, Richland, WA, United States, (8)University of Illinois Urbana-Champaign, Agroecosystem Sustainability Center, Institute for Sustainability, Energy, and Environment, Urbana, United States
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