Solution Calorimetry Under Hydrothermal Conditions

Research Article| January 01, 2013 Solution Calorimetry Under Hydrothermal Conditions Peter Tremaine; Peter Tremaine Department of Chemistry, University of Guelph, 50 Stone Road East, Guelph, Ontario, N1G 2W1, Canada, tremaine@uoguelph.ca, harcis@uoguelph.ca Search for other works by this author on: GSW Google Scholar Hugues Arcis Hugues Arcis Department of Chemistry, University of Guelph, 50 Stone Road East, Guelph, Ontario, N1G 2W1, Canada, tremaine@uoguelph.ca, harcis@uoguelph.ca Search for other works by this author on: GSW Google Scholar Author and Article Information Peter Tremaine Department of Chemistry, University of Guelph, 50 Stone Road East, Guelph, Ontario, N1G 2W1, Canada, tremaine@uoguelph.ca, harcis@uoguelph.ca Hugues Arcis Department of Chemistry, University of Guelph, 50 Stone Road East, Guelph, Ontario, N1G 2W1, Canada, tremaine@uoguelph.ca, harcis@uoguelph.ca Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © 2013 Mineralogical Society of America Reviews in Mineralogy and Geochemistry (2013) 76 (1): 219–263. https://doi.org/10.2138/rmg.2013.76.7 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Peter Tremaine, Hugues Arcis; Solution Calorimetry Under Hydrothermal Conditions. Reviews in Mineralogy and Geochemistry 2013;; 76 (1): 219–263. doi: https://doi.org/10.2138/rmg.2013.76.7 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 The first quantitative studies of the thermodynamics of hydrothermal solutions were made in 1903 by A.A. Noyes and W.D. Coolidge (1903), who used the change in conductance associated with ionization to measure the ionization constants of water and aqueous acids and bases up to about 300 °C at steam saturation. The need to develop nuclear reactor coolant chemistry in the 1950's led national laboratories in several countries to develop new experimental methods for measuring solubility products, equilibrium constants and activity coefficients under the corrosive conditions encountered at elevated temperatures. Complementary studies by geochemists investigating geothermal systems and ore body... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.