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Abstract: Lab dissolution experiments and reactive transport models reveal the interplay between alkalinity generation and secondary mineral formation in the Upper Deschutes Basin, Oregon (AGU25)

Lab dissolution experiments and reactive transport models reveal the interplay between alkalinity generation and secondary mineral formation in the Upper Deschutes Basin, Oregon

Sebastian Muñoz1,2, Jesse S Miller3, Evan Joseph Ramos4, Noah Jemison5, Yi Hou6, William Larsen7, Jonah Bernstein-Schalet1, Kly D Suquino8, Miriam Gammerman9, Preston Cosslett Kemeny10, Mark Torres9 and Daniel Enrique Ibarra1, (1)Brown University, Department of Earth, Environmental and Planetary Sciences, Providence, United States, (2)Institute at Brown for Environment and Society (IBES), Providence, United States, (3)Brown University, Earth, Environment, and Planetary Sciences, Providence, United States, (4)University of Pittsburgh, Department of Geology and Environmental Science, Pittsburgh, PA, United States, (5)University of Pittsburgh, Department of Geology and Environmental Science, Pittsburgh, United States, (6)ETH Zurich, Geological Institute, Department of Earth Sciences, Zurich, Switzerland, (7)Terradot, San Francisco, United States, (8)Rice University, Department of Earth, Environment, and Planetary Science, Houston, United States, (9)Rice University, Department of Earth, Environmental and Planetary Sciences, Houston, United States, (10)Woods Hole Oceanographic Institution, Woods Hole, United States
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