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

REFERENCESBruant, R.G., Jr, Celia, M.A., Guswa, A.J., and Peters, C.A. (2002). Safe storage of CO 2 in deep saline aquifers.Environmental Science Technology 36(11), 240A–245A.Brun, A., and Engesgaard, P. (2002). Modelling of transport and biogeochemical processes in pollution plumes:Literature review and model development. Journal of Hydrology 256(3–4), 211–227.Bruno, J., and Ewing, R.C. (2006). Spent nuclear fuel. Elements 2(6), 343–349.Buffle, J., and van Leeuwen, H., eds. (1992). Environmental Particles. International Union of Pure and AppliedChemistry (IUPAC) Series on Analytical and Physical Chemistry of Environmental Systems, Lewis Publishers,Boca Raton, FL.Bundschuh, T., Knopp, R., Winzenbacher, R., Kim, J.I. and Köster, R. (2001). Quantification of aquatic nanoparticles after different steps of Bodensee water purification with laser-induced breakdown detection (LIBD).Acta Hydrochimica et Hydrobiologica 29, 7–15.Burns, P.C., and Klingensmith, A.L. (2006). Uranium mineralogy and neptunium mobility. Elements 2, 351–356.Cadoret, T., Marion, D., and Zinszner, B. (1995). Influence of frequency and fluid distribution on elastic wavevelocities in partially saturated limestones. Journal of Geophysical Research 100, 9789–9804.Cadoret, T. (1993). Effet de la Saturation Eau/Gaz sur les Propriétés Acoustiques des Roches, Ph.D. dissertation,University of Paris, VII.Caffarelli, L.A., Crandall, M.G., Kocan, M., and Swipolhkech, A. (1996). On viscosity solutions of fully nonlinearequations with measurable ingredients. Communications on Pure and Applied Mathematics 49, 365.Caine, J.S., Evans, J.P. and Forster, C.B. (1996). Fault zone architecture and permeability structure. Geology 24,1025–1028.Callaghan, P.T. (1991). Principles of Nuclear Magnetic Resonance Microscopy. Oxford University Press, NewYork.Cao, Z.T., Tester, J.W., and Trout, B.L. (2001). Computation of the methane-water potential energy hypersurfacevia ab initio methods. Journal of Chemical Physics 115(6), 2550–2559.Carle, S.F., and Fogg, G.E. (1997). Modeling spatial variability with one and multi-dimensional continuous Markovchains. Mathematical Geology 29(7), 891–918.Carle, S.F., LaBolle, E.M., Weissman, G.S., van Brocklin, D., and Fogg, G.E. (1998). Conditional simulation ofhydrofacies architecture: A transition probability/Markov chain approach. In Hydrogeologic Models ofSedimentary Aquifers, G.S. Fraser, and J.M. Davis, eds., Concepts in Hydrogeology No. 1, SEPM (Society forSedimentary Geology) Special Publication, pp. 147–170.Casey, W.H. (2006). Large aqueous aluminum-hydroxide molecules. Chemical Reviews 106, 1–16.Chappelle, F.H., and Lovley, D.R. (1990). Rates of microbial metabolism. Applied Environmental Microbiology56(6), 1865–1874.Chappelle F. H., and Lovley, D.R. (1992). Competitive exclusion of sulfate reduction by Fe(III)-reducing bacteria:A mechanism for producing discrete zones of high-iron ground water. Ground Water 30(1), 29–36.Charlet, L., and Polya, D.A. (2006). Arsenic in shallow, reducing groundwaters in southern Asia: An environmentalhealth disaster. Elements 2, 91–96.Chavarria, J.A., Malin, P., Catchings, R.D., and Shalev, E. (2003). A look inside the San Andreas fault at Parkfieldthrough vertical seismic profiling. Science 302, 1746–1748.Basic Research Needs for Geosciences: Facilitating 21 st Century Energy Systems 171