Contributions of visible and invisible pores to reactive transport in dolomiteB. Tutolo, A. Luhmann, X. Kong, B. Bagley, D. Alba-Venero, N. Mitchell, M. Saar, W. Seyfried, Jr.2020 Peer-ReviewedGeochemical Perspectives Letters, 42-46 URLDOI: 10.7185/geochemlet.2022[Cite]View Abstract
Permeability, porosity, and mineral surface area changes in basalt cores induced by reactive transport of <scp>CO</scp><sub>2</sub>‐rich brineA. Luhmann, B. Tutolo, B. Bagley, D. Mildner, W. Seyfried, M. Saar2017 Peer-ReviewedWater Resources Research 53, 1908-1927 URLDOI: 10.1002/2016wr019216[Cite]View Abstract
Whole rock basalt alteration from CO2-rich brine during flow-through experiments at 150 °C and 150 barA. Luhmann, B. Tutolo, C. Tan, B. Moskowitz, M. Saar, W. Seyfried2017 Peer-ReviewedChemical Geology 453, 92-110 URLDOI: 10.1016/j.chemgeo.2017.02.002[Cite]View Abstract
CO2 sequestration in feldspar-rich sandstone: Coupled evolution of fluid chemistry, mineral reaction rates, and hydrogeochemical propertiesB. Tutolo, A. Luhmann, X. Kong, M. Saar, W. Seyfried2015 Peer-ReviewedGeochimica et Cosmochimica Acta 160, 132-154 URLDOI: 10.1016/j.gca.2015.04.002[Cite]View Abstract
Thermal damping and retardation in karst conduitsA. Luhmann, M. Covington, J. Myre, M. Perne, S. Jones, E. Alexander Jr., M. Saar2015 Peer-ReviewedHydrology and Earth System Sciences 19, 137-157 URLDOI: 10.5194/hess-19-137-2015[Cite]View Abstract
