David M. Mason
California Institute of Technology
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Journal of Chemical Physics | 1956
David Altman; Milton Farber; David M. Mason
From a series of ten different experiments performed at this laboratory and from experiments reported elsewhere, the following thermodynamic properties have been obtained (ΔHf298 in kcal/mole and S°298 in cal/°C/mole): TiCl4(l), ΔHf298=—191.2; TiCl4(g), ΔHf298=—181.6; TiCl3(s), ΔHf298=—170.7, S°298 =34.4; TiCl3(g), ΔHf298=—128.7, S°298=74.9; TiCl2(s), ΔHf298=—120.6, S°298=24.7; TiCl2(g), ΔHf298 =—69.4, S°298=65.9. A theoretical value for S°298 of 56.1 was calculated for TiCl(g). Estimated values for the Cp of these compounds are also included.
Journal of Chemical Physics | 1956
Walter F. Krieve; Stephen P. Vango; David M. Mason
The heats of formation of TiCl4(l), TiCl3(s), and TiCl2(s) were determined by chlorinating Ti, TiCl3(s), and TiCl2(s), respectively, in a nickel‐bomb calorimeter to give TiCl4(l). The directly measured heat of chlorination at 25° of Ti is —190.0±0.4, of TiCl3(s) is 20.9±0.1, and of TiCl2(s) is 69.9±0.8 kcal/mole—1. Relative to a value for the heat of formation of TiCl4(l) of —190.0±0.4, the corresponding values for the heats of formation of TiCl3(s) and TiCl2(s) are —169.1±0.4 and —120.1±0.8 kcal/mole—1, respectively.
Journal of Chemical Physics | 1956
Walter F. Krieve; David M. Mason
Equilibrium in the TiCl3(s)–HCl(g) system was studied in the temperature range 350 to 475°C by measuring the total pressure in an isochoric vessel. The equilibrium data for the above reaction in this temperature range is given by log10K (atmos) = (—2.27×103/T)+1.82. From these data, the enthalpy and entropy of reaction at the average temperature of about 690°K are 10.4±0.4 kcal and 17.5±0.5 cal/deg, respectively. From an estimated value for the ΔCp of reaction, the enthalpy and entropy of reaction at 25°C are estimated to be 12.7±1.0 kcal and 22.5±2.0 cal/deg, respectively. The difference between the enthalpies of formation of TiCl3(s) and TiCl4(l) is 19.0±1.0 kcal/mole—1 at 25°C. The equilibrium is shifted toward TiCl4(g) and H2(g) with increase in temperature, and 25°C the reduction of TiCl4(g) by H2(g) to give TiCl3(s) is nearly complete, although the rate of the reaction is very low.
The Journal of Physical Chemistry | 1959
Robert G. Rinker; T. P. Gordon; David M. Mason; William H. Corcoran
The Journal of Physical Chemistry | 1960
Robert G. Rinker; Thomas P. Gordon; David M. Mason; Roy R. Sakaida; William H. Corcoran
Journal of Chemical & Engineering Data | 1964
Ira. Petker; David M. Mason
The Journal of Physical Chemistry | 1955
David M. Mason; Ira. Petker; Stephen P. Vango
Aiche Journal | 1961
Walter F. Krieve; David M. Mason
The Journal of Physical Chemistry | 1956
Gerard W. Elverum; David M. Mason
The Journal of Physical Chemistry | 1956
David M. Mason; Stephen P. Vango