A high-temperature high-pressure calorimeter for determining heats of solution up to 623 K.
A high-temperature high-pressure isoperibol calorimeter for determining the heats of solution and reaction of very dilute substances in water (10(-4) m) at temperatures up to 623 K is described. The energies of vaporization of water at steam saturation pressure were measured as a function of temperature and the results agree with the corresponding values from steam tables to better than 0.08+/-0.18%. The novelties of the present instrument relative to flow type heat capacity calorimeters are that measurements can be made at orders of magnitude lower concentrations and that measurement of heat of reaction involving solids or gases or in the presence of high concentrations of supporting electrolytes, acids, and bases is possible. Furthermore, the advantage of using enthalpy data over heat capacity data for calculations of the standard state Gibbs free energies of electrolytes is that the experimental heat data of this research need only be integrated once to derive higher temperature free energy data from lower temperatures. The derived heat capacities can be used mathematically to obtain free energies by double integration. However, the resulting errors are much smaller than if experimental aqueous heat capacities were used for the integrations.
Djamali
Essmaiil
E
Department of Chemistry and Center for Hydrothermal Research, San Diego State University, San Diego, California 92182, USA. djamali@sciences.sdsu.edu
Turner
Peter J
PJ
Murray
Richard C
RC
Cobble
James W
JW
D002138:Calibration; D002151:Calorimetry / Q000295:instrumentation / Q000379:methods*; D004560:Electricity; D006358:Hot Temperature; D011312:Pressure; D012996:Solutions; D013816:Thermodynamics; D014835:Volatilization; D014867:Water / Q000737:chemistry*
D012996:Solutions; D014867:Water