受限环境下的金属配合物

L. Stievano, S. Calogero, L. Storaro, M. Lenarda, F. Wagner
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引用次数: 4

摘要

采用197Au穆斯堡尔光谱、x射线衍射和红外光谱研究了金硫脲(T)配合物AuT2+在贝德尔粘土和铝柱贝德尔中的插层作用。在接近阳离子交换容量的浓度下,AuT2+配合物被发现与粘土片呈对角线取向,而在较低的浓度下,它们在柱状贝德星中平躺在层间距上。在高达400°C的温度下,研究了插层AuT2+的热分解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Metal complexes in a constrained environment
Intercalation of the gold thiourea (T) complex, AuT2+, into beidellite clay and aluminium pillared beidellite was studied by 197Au Mossbauer spectroscopy, X-ray diffraction and infrared spectroscopy. At a concentration close to the cation exchange capacity, the AuT2+ complexes are found to be oriented diagonal to the clay sheets, while at a much lower concentration and in the pillared beidellite they lie flat in the interlayer spacing. Thermal decomposition of the intercalated AuT2+ was studied at temperatures up to 400 °C.
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