Basic Research Needs for Geosciences - Energetics Meetings and ...

REFERENCESBenner, S.G., Hansel, C.M., Wielinga, B.W., Barber, T.M., and Fendorf, S. (2002). Reductive dissolution andbiomineralization of iron hydroxide under dynamic flow conditions. Environmental Science Technology 36,1705–1711.Benson, S., and Hepple, R. (2005) Prospects for early detection and options for remediation of leakage from CO 2storage projects. In Carbon Dioxide Capture for Storage in Deep GeologicFformations – Results from the CO 2Capture and Storage Project, Vol. 2 – Geologic Storage of Carbon Dioxide with Monitoring and Verification,S.M. Benson, ed., Elsevier, 1189–1203.Berlyand, L., and Kolpakov, A. (2001). Network approximation in the limit of small Interparticle distance of theeffective properties of a high-contrast random dispersed composite. Archives of Rational Mechanical Analysis159(3), 179–227.Berner, R.A. (1995). Chemical weathering and its effect on atmospheric CO 2 and climate. Chemical WeatheringRates of Silicate Minerals, 31, 565–583.Berner, R.A., Lasaga, A.C., and Garrels, R.M. (1983). The carbonate-silicate geochemical cycle and its effect onatmospheric carbon dioxide over the past 100 million years. American Journal of Science 283, 641–683.Bethke, C.M., and Johnson, T.M. (2002). Paradox of groundwater age. Geology 30(2), 107–110.Bickmore, B.R., Nagy, K.L., Gray, A.K. and Brinkerhoff, A.R. (2006). The effect of Al(OH) 4 - on the dissolution ofquartz. Geochimica et Cosmochimica Acta 70, 290–305.Binley, A., and Beven, K. (2003). Vadose zone flow model uncertainty as conditioned on geophysical data. GroundWater 41(2), 119–127.Blencoe, J.G. (2004) The CO 2 -H 2 O system. IV. Empirical equations for representing vapor-liquid equilibria at 110–350°C. American Mineralogist 89, 1447–1455.Blencoe, J.G., Drummond, S.E., Seitz, J.C., and Nesbitt, B.E. (1996). A vibrating-tube densimeter for fluids at highpressures and temperatures. International Journal of Thermophysics 17, 179–190.Blencoe, J.G., Seitz, J.C., and Anovitz, L.M. (1999). The CO 2 -H 2 O system. II. Calculated thermodynamic mixingproperties for 400°C, 0.1-400 MPa. Geochimica et Cosmochimica Acta 63, 2393-2408.Blencoe, J.G., Naney, M.T., and Anovitz, L.M. (2001). The CO 2 -H 2 O system. III. A new experimental method fordetermining liquid-vapor equilibria at high subcritical temperatures. American Mineralogist 86, 1100–1111.Blunt, M.J. (2001). Flow in porous media—Pore-network models and multiphase flow. Current Opinion in Colloidand Interface Science 6, 1970207.Bodnar, R.J., Burnham, C.W., and Sterner, S.M. (1985). Synthetic fluid inclusions in natural quartz. III.Determination of phase equilibrium properties in the system H 2 O-NaCl to 1000ºC and 1500 bars. Geochimica etCosmochimica Acta 49, 1861–1873.Borcea, L., and Papanicolaou, G.C. (1998). Network approximation for transport properties of high contrastmaterials. SIAM Journal of Applied Mathematics 58(2), 501–539.Brantley, S.L. (2004). Reaction kinetics of primary rock-forming minerals under ambient conditions, Surface andGround Water, Weathering, and Soils, Treatise on Geochemistry 5, J.I. Drever, ed., 73–117.Brown, G.E. (2001). Surface science—How minerals react with water. Science 294(5540).Brown, G.E., Henrich, V.E., Casey, W.H., Clark, D.L., Eggleston, C., Felmy, A., Goodman, D.W., Gratzel, M.,Maciel, G., McCarthy, M.I., Nealson, K.H., Sverjensky, D.A., Toney, M.F., and Zachara, J.M. (1999). Metaloxide surfaces and their interactions with aqueous solutions and microbial organisms. Chemical Reviews 99,77–174.170 Basic Research Needs for Geosciences: Facilitating 21 st Century Energy Systems