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Synthesis and characterization of Al_(13)-oxalate gel with Keggin structure 被引量:1

Synthesis and characterization of Al_(13)-oxalate gel with Keggin structure
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摘要 In this study, the Al13-oxalate gel synthesized from Al13 solution was characterized by XRD, FTIR and MAS 27Al NMR. The results are: 1) the gel shows obvious XRD diffraction peaks, which is different from common Al gels and their oxalate precipitations; 2) the peak of Al-O stretch vibration of Al13-oxalate complexes at 810 cm-1 indicates that the gel was formed directly by the complexes, and the characteristic peaks of IR and solid-state NMR respectively occur at 725 cm-1 and ~6.1×10-5 chemical shift, which are respectively assigned to (Al-O)Td vibration and (Al-O)4 tetrahedron, suggesting that the gel has a unique Keggin structure; 3) Al13 polyoxocation can directly form gel with oxalate, even in a high-pH environment (=7.8). This finding provides new evidence for the universality of Al13 in natural environments. Through chemical analysis, the chemical formula of the gel was determined to be AlO4Al12(OH)24(H2O)12(C2O4)7/2. In this study, the Al13-oxalate gel synthesized from Al13 solution was characterized by XRD, PTIR and MAS 27A1 NMR. The results are: 1) the gel shows obvious XRD diffraction peaks, which is different from common AI gels and their oxalate precipitations; 2) the peak of A1-O stretch vibration of Al13-Oxalate complexes at 810 cm^-1 indicates that the gel was formed directly by the complexes, and the characteristic peaks of IR and solid-state NMR respectively occur at 725 cm^-1 and -6.1×10^-5 chemical shift, which are respectively assigned to (AI-O)Td vibration and (A1-O)4 tetrahedron, suggesting that the gel has a unique Keggin structure; 3) Al13 polyoxocation can directly form gel with oxalate, even in a high-pH environment (=7.8). This finding provides new evidence for the universality of Al13 in natural environments. Through chemical analysis, the chemical formula of the gel was determined to be AlO4Al12(OH)24(H2O)12(C2O4)7/2,
出处 《Chinese Journal Of Geochemistry》 EI CAS 2009年第4期364-368,共5页 中国地球化学学报
基金 supported by the specialized re-search fund for the Doctoral Program of Higher Edu-cation of China (Grant No 2006029009) the Program for New Century Excellent Talents in China University of Mining and Technology (Grant No NCET-07-0801)
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