Neutron Scattering and Diffraction Studies of Fluids and Fluid-Solid Interactions

Abstract

Research Article| January 01, 2006 Neutron Scattering and Diffraction Studies of Fluids and Fluid-Solid Interactions David R. Cole; David R. Cole Chemical Sciences Division Oak Ridge National Laboratory Oak Ridge, Tennessee 37831-6110, U.S.A., e-mail: [e-mail] Search for other works by this author on: GSW Google Scholar Kenneth W. Herwig; Kenneth W. Herwig Spallation Neutron Source Oak Ridge National Laboratory Oak Ridge, Tennessee 37831-6475, U.S.A. Search for other works by this author on: GSW Google Scholar Eugene Mamontov; Eugene Mamontov Spallation Neutron Source Oak Ridge National Laboratory Oak Ridge, Tennessee 37831-6475, U.S.A. Search for other works by this author on: GSW Google Scholar John Z. Larese John Z. Larese Department of Chemistry University of Tennessee Knoxville, Tennessee, 37996, U.S.A. Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2006) 63 (1): 313–362. https://doi.org/10.2138/rmg.2006.63.13 Article history first online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation David R. Cole, Kenneth W. Herwig, Eugene Mamontov, John Z. Larese; Neutron Scattering and Diffraction Studies of Fluids and Fluid-Solid Interactions. Reviews in Mineralogy and Geochemistry 2006;; 63 (1): 313–362. doi: https://doi.org/10.2138/rmg.2006.63.13 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Geologic fluids (defined liberally as gases, liquids, and supercritical solutions) act as reaction media, reactants, and carriers of energy and matter in the natural environment. Among the many different types of geologic fluids, those containing volatile C-O-H-N-S species and those enriched in chloride salts (brines) are of particular interest. They occur widely in varied geochemical settings, commonly contain significant quantities of dissolved and suspended compounds (complex hydrocarbons, organic macromolecules, colloids/nanoparticles), play a crucial role as primary reaction media, and are important sources and sinks of greenhouse gases. The consequences of coupled reactive-transport processes common to most geological environments depend on... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.