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Thermal decomposition reactions of tetraalkylammonium thiotungstates, (R4N)2WS4 (R = methyl to heptyl), were investigated with DSC and DTA-TG coupled with mass spectroscopy (MS). The results demonstrate that the complexity of thermal decomposition reactions is significantly influenced by the alkyl group, i.e., more complex steps are observed for the materials with longer alkyl chain lengths. Tetraethyl and tetrapropyl complexes show reversible and irreversible phase transitions detected by DSC experiments combined with thermodiffractometry. The tetrapentyl compound undergoes an irreversible phase transition while the tetraheptyl sample exhibits a glass-like transition and melting prior to decomposition. The whole series of compounds decompose without forming sulfur rich WSn (n = 3 or 4) intermediates. The final WS2 products are nearly stoichiometric for R = methyl to pentyl but for hexyl and heptyl samples the sulfur content is significantly reduced with a W/S ratio of about 1.5. The residual carbon and hydrogen contents increase in the final decomposition products in the same order as the number of C atoms in R4N increase. For the N content no clear trend is obvious. A general thermal decomposition mechanism is suggested which follows a bimolecular nucleophilic substitution reaction. In the SEM images only for R = heptyl the formation of macro-pores with a sponge-like morphology is seen, but for the other precursors compact materials are formed which in part display a well developed morphology. X-ray diffraction analysis of the final products shows the formation of amorphous WS2 up to the tetrapentyl precursor. But for the tetrahexyl and tetraheptyl materials the W:S ratio is significantly smaller than 1:2 and large amounts of C and H are determined by chemical analyses. In accordance with previously reported results it can be assumed that a carbosulfide phase is formed by a mixed C-W-S sandwich layered structure.  相似文献   
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The decomposition pattern of tetraalkyl-tetrathiomolybdates with general formula (R4N)2MoS4 (with R increasing from methyl to heptyl) was determined by means of differential thermal analysis (DTA), thermogravimetric analysis (TGA) and mass spectroscopy (MS) techniques. The complexity of thermal decomposition reactions increases with the size of the R4N group. Prior to decomposition at least one phase transition seems to occur in all complexes. The onset of thermal reactions was also a function of the tetra-alkylammonium precursor. All compounds decompose without forming sulfur rich MoS2+x intermediates. For R = methyl to pentyl precursors the MoS2 produced was nearly stoichiometric, however for R = hexyl and heptyl the S content was significantly reduced with a Mo:S ratio of about 1.5. The carbon and hydrogen residual contents in the product increased with the number of C atoms in R4N; for N contamination no clear trend was obvious. SEM images show that the formation of macro-pores was also a function of the alkyl group in R4N. The MoS2 materials obtained show a sponge-like morphology. Results of DSC experiments in combination with in situ X-ray diffraction also revealed the complex thermal behavior of (R4N)2MoS4 materials; reversible and irreversible phase transitions and glass-like transformations were identified in the low temperature range (35-140 °C), before the onset of decomposition.  相似文献   
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Two mechanisms of doping Li(3)NbO(4), which has an ordered, rock salt superstructure, have been established. In the "stoichiometric mechanism", the overall cation-to-anion ratio is maintained at 1:1 by means of the substitution 3Li(+) + Nb(5+) --> 4Ni(2+). In the "vacancy mechanism", Li(+) ion vacancies are created by means of the substitution 2Li(+) --> Ni(2+). Solid solution ranges have been determined for both mechanisms and a partial phase diagram constructed for the stoichiometric join. On the vacancy join, the substitution mechanism has been confirmed by powder neutron diffraction; associated with lithium vacancy creation, a dramatic increase in Li(+) ion conductivity occurs with increasing Ni content, reaching a value of 5 x 10(-4) Omega(-1) cm(-1) at 300 degrees C for composition x= 0.1 in the formula Li(3-2x)Ni(x)NbO(4). This is the first example of high Li(+) ion conductivity in complex oxides with rock salt-related structures.  相似文献   
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