Сообщение
vano » Вт май 23, 2006 3:12 pm
А он точно не восстанавливается ничем до GeO (который летуч) ?
SciFinder говорить что есть такие статьи:
Davydov, V. I. Equilibrium vapor pressures of germanium dioxide. Zhurnal Neorganicheskoi Khimii (1957), 2 1460-6. CODEN: ZNOKAQ ISSN:0044-457X. CAN 52:43702 AN 1958:43702 CAPLUS
Bergman, G. A. The equilibrium vapor pressure over germanium dioxide. Zhurnal Neorganicheskoi Khimii (1958), 3 2422-4. CODEN: ZNOKAQ ISSN:0044-457X. CAN 55:52264 AN 1961:52264 CAPLUS
а еще есть статья японцев:
The vapor pressure of germanium dioxide. Shimazaki, Eiichi; Matsumoto, Noboru; Niwa, Kichizo. Univ. Hokkaido, Sapporo, Bulletin of the Chemical Society of Japan (1957), 30 969-71. CODEN: BCSJA8 ISSN: 0009-2673. Journal language unavailable. CAN 52:48348 AN 1958:48348 CAPLUS
Abstract
cf. Brewer, C.A. 47, 3678d. The apparent vapor pressure of cryst. GeO2 of hexagonal a-quartz structure, or the dissocn. pressure for the reaction GeO2 = GeO + 1/2O2, was measured over the temp. range 1040-1100° by the Knudsen's effusion method (cf. S. and Wada, C.A. 50, 12581f); the results are expressed by the equation: log pmm. = -25,517/T + 16.245. From the free-energy equation the heat of reaction, the free energy, and the entropy change of the reaction were calcd. as DH298 = 121.7 ± 0.3 kcal./mol., DG298 = 101.7 kcal./mol. and DS298 = 67.3 e.u., resp. The heat of reaction agrees well with the value calcd. from accessible thermal data. The normal entropy of solid GeO2 was calcd. as S298 = 10.8 ± 1.0 e.u., which agrees with the computed value (cf. Bues and von Wartenberg, C.A. 46, 5421b).
И статья американцев:
The equilibrium Ge(s) + GeO2(s) = 2GeO(g). The heat of formation of germanic oxide. Jolly, Wm. L.; Latimer, Wendell M. Univ. of California, Berkeley, Journal of the American Chemical Society (1952), 74 5757-8. CODEN: JACSAT ISSN: 0002-7863. Journal language unavailable. CAN 47:8435 AN 1953:8435 CAPLUS
Abstract
The vapor pressure of GeO over Ge and GeO2 was measured using a Knudsen effusion cell at temps. 758-859°K. Inconsistencies between these results and those of Bues and v. Wartenberg (C.A. 46, 5421b) are discussed. The calcd. thermodynamic consts. for the reaction 1/2; Ge(solid) + 1/2; GeO2(solid) = GeO(gas) are: DF° = 54,600 + 6.9T log T - 62T cal./mole; DH° = 54,600 - 3T cal./mole; DS° = 59 - 6.91 log T cal./degree mole. The heat of oxidation of Ge metal to GeO2 was measured calorimetrically in an alk. soln. of NaOCl at 25°. It was calcd. from these and other thermal data that the heat of formation of GeO2(solid) is -129.2 ± 2.0 kcal./mole, in good agreement with direct measurements (Becker and Roth, C.A. 26, 5487; Hahn and Juza, C.A. 35,