Contributions of visible and invisible pores to reactive transport in dolomiteTutolo, B. M., Luhmann, A. J., Kong, X.-Z., Bagley, B. C., Alba-Venero, D., Mitchell, N., Saar, M. O., and Seyfried, Jr., W. E.2020Refereed Publications in Journals Peer-ReviewedGeochemical Perspectives Letters I4, pp. 42–46Abstract ▾(Published: July 1, 2020)DOIDOI: 10.7185/geochemlet.2022Cite
Permeability, porosity, and mineral surface area changes in basalt cores induced by reactive transport of CO₂‐rich brineLuhmann, A. J., Tutolo, B. M., Bagley, B. C., Mildner, D. F. R., Seyfried, Jr., W. E., and Saar, M. O.2017Refereed Publications in Journals Peer-ReviewedWater Resources Research 53, pp. 1–20Abstract ▾(Published: March 1, 2017)DOIDOI: 10.1002/2016wr019216Cite
Experimental dissolution of dolomite by CO2-charged brine at 100°C and 150bar: Evolution of porosity, permeability, and reactive surface areaLuhmann, A. J., Kong, X.-Z., Tutolo, B. M., Garapati, N., Bagley, B. C., Saar, M. O., and Seyfried, Jr., W. E.2014Refereed Publications in Journals Peer-ReviewedChemical Geology 380, pp. 145–160Abstract ▾(Published: July 1, 2014)DOIDOI: 10.1016/j.chemgeo.2014.05.001Cite
