Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (105 pascals) pressure and at higher temperatures
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Bulletin↗
Geology topics
James R. Fisher
Publications and source records attributed to James R. Fisher.
Heat capacities of gibbsite, Al(OH)3, between 13 and 480 K and magnesite, MgCO3, between 13 and 380 K and their standard entropies at 289.15 K, and the heat capacities of Calorimetry Conference benzoic acid between 12 and 316 K
The heat capacities of gibbsite and magnesite were measured between 13 and 380 K by means of an adiabatic calorimeter. The heat capacity of gibbsite was measured continuously between 340 and 480 K by means of a differential scanning calorimeter. Tables of the thermodynamic functions C° P , (H° T –H° O )/T ,– (G° T –H° O )/T , and S° T –S° O are presented for these phases at integral temperatures. S° T –S° O are 68.44±0.14 J/(K•mol) and 65.09±0.13 J/(K•mol) at 298.15 K for gibbsite and magnesite, respectively. The heat capacities of Calorimetry Conference benzoic acid have been remeasured between 12 and 316 K.
Journal of Research of the U.S. Geological Survey↗
The volumetric properties of H2O — A graphical portrayal
A graphical display of the volumetric properties of H 2 O is presented as density (0.01 to 1.0 g-cm -3 ) contoured on pressure-temperature coordinates and pressure (1-10,000 bars) contoured on density-temperature coordinates over the temperature range 0-1,000 °C. Data were obtained from sources published during 1964-1969; several minor inconsistencies are observed and attributed to inadequacies in the equations of state used to describe experimental data obtained above 1,000 bars.
Journal of Research of the U.S. Geological Survey↗