Amy E Hofmann

Learn More
a Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, United States b Department of Earth Sciences, University of Toronto, Toronto, Ontario MSS 3B1, Canada c Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720, United States d Laboratoire de Géochimie des Isotopes Stables Institut de(More)
Molecular dynamics simulations show that the desolvation rates of isotopes of Li(+), K(+), Rb(+), Ca(2+), Sr(2+), and Ba(2+) may have a relatively strong dependence on the metal cation mass. This inference is based on the observation that the exchange rate constant, k(wex), for water molecules in the first hydration shell follows an inverse power-law mass(More)
  • 1