Abstract
Selenium is an important trace element. Its geochemical cycles involve various oxidation states, including Se2-, yet thermodynamic data for selenides are sparse. A general method for selenide thermochemistry has been developed by using oxidative drop-solution calorimetry in a molten oxide solvent. The samples are dropped from room temperature into molten sodium molybdate (3Na2O·4MoO3) solvent at 975 K, with oxygen bubbling through the melt to ensure rapid and complete conversion of selenide to dissolved selenate species. This method is analogous to that developed for sulfides (Deore and Navrotsky 2006). Complete dissolution of selenides is documented by furnace tests and visual inspection, and supported by consistent results for enthalpy. Enthalpies of formation (ΔfH°, kJ/mol) from the elements were determined for zinc selenide (ZnSe) (-169.94 ± 4.31 kJ/mol), cadmium selenide (CdSe) (-139.04 ± 6.13 kJ/mol), and lead selenide (PbSe) (-99.26 ± 6.06 kJ/mol). These three ΔfH° values agree with previously published data, often obtained by less direct means. This is the first report of the enthalpy of formation of CdSe measured by any calorimetric method. For ZnSe, a more reliable ΔfH° value is proposed since prior data are quite scattered. The results confirm that oxidative drop-solution calorimetry is an available method for selenide thermochemistry. It should be applicable to binary and multinary selenides with large homogeneity ranges, to solid solutions, and to nanophase materials.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
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- Thermal equation of state of CaGeO3 perovskite
- Quantitative absorbance spectroscopy with unpolarized light: Part I. Physical and mathematical development
- Quantitative absorbance spectroscopy with unpolarized light: Part II. Experimental evaluation and development of a protocol for quantitative analysis of mineral IR spectra
- Oxide-melt solution calorimetry of selenides: Enthalpy of formation of zinc, cadmium, and lead selenide
- Precise dating of biotite in distal volcanic ash: Isolating subtle alteration using 40Ar/39Ar laser incremental heating and electron microprobe techniques
- Rationale for the existence of four- and eight-reversals in antigorite
- Structural relaxation around substitutional Cr3+ in pyrope garnet
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Articles in the same Issue
- The crystal structure of vurroite, Pb20Sn2(Bi,As)22S54Cl6: OD-character, polytypism, twinning, and modular description
- Mineralogy of the Paso Robles soils on Mars
- Dingdaohengite-(Ce) from the Bayan Obo REE-Nb-Fe Mine, China: Both a true polymorph of perrierite-(Ce) and a titanic analog at the C1 site of chevkinite subgroup
- Thermal equation of state of CaGeO3 perovskite
- Quantitative absorbance spectroscopy with unpolarized light: Part I. Physical and mathematical development
- Quantitative absorbance spectroscopy with unpolarized light: Part II. Experimental evaluation and development of a protocol for quantitative analysis of mineral IR spectra
- Oxide-melt solution calorimetry of selenides: Enthalpy of formation of zinc, cadmium, and lead selenide
- Precise dating of biotite in distal volcanic ash: Isolating subtle alteration using 40Ar/39Ar laser incremental heating and electron microprobe techniques
- Rationale for the existence of four- and eight-reversals in antigorite
- Structural relaxation around substitutional Cr3+ in pyrope garnet
- Metasomatic thorite and uraninite inclusions in xenotime and monazite from granitic pegmatites, Hidra anorthosite massif, southwestern Norway: Mechanics and fluid chemistry
- Interlayer potassium and its neighboring atoms in micas: Crystal-chemical modeling and XANES spectroscopy
- Effect of chemical environment on the hydrogen-related defect chemistry in wadsleyite
- Fracture toughness, hardness, and elastic modulus of kyanite investigated by a depth-sensing indentation technique
- Crystal chemistry of the natrojarosite-jarosite and natrojarosite-hydronium jarosite solid-solution series: A synthetic study with full Fe site occupancy
- A new experimental thin film approach to study mobility and partitioning of elements in grain boundaries: Fe-Mg exchange between olivines mediated by transport through an inert grain boundary
- Titanium as a cathodoluminescence activator in alkali feldspars
- Biogenic vs. abiogenic magnetite nanoparticles: A XMCD study
- Solubility of andradite, Ca3Fe2Si3O12, in a 10 mol% NaCl solution at 800 °C and 10 kbar: Implications for the metasomatic origin of grandite garnet in calc-silicate granulites
- A 3D reconstruction of plagioclase crystals in a synthetic basalt
- Rudashevskyite, the Fe-dominant analogue of sphalerite, a new mineral: Description and crystal structure
- Birchite, a new mineral from Broken Hill, New South Wales, Australia: Description and structure refinement
- Crystal structure of synthetic Al4B2O9: A member of the mullite family closely related to boralsilite
- Interaction of gypsum with As(V)-bearing aqueous solutions: Surface precipitation of guerinite, sainfeldite, and Ca2NaH(AsO4)2·6H2O, a synthetic arsenate
- Jahnsite-(NaFeMg), a new mineral from the Tip Top mine, Custer County, South Dakota: Description and crystal structure
- Evidence for anomalously large degree of polymerization in Mg2SiO4 glass and melt
- Theoretical infrared absorption coefficient of OH groups in minerals