镁铝水滑石层板与层间阴离子相互作用的理论研究
Theoretical Study of the Layer-Anio n Interactions in Magnesium Aluminum Layered Double Hydroxides
作者单位
罗青松 北京化工大学可控化学反应科学与技术基础教育部重点实验室, 北京100029 
李蕾 北京化工大学可控化学反应科学与技术基础教育部重点实验室, 北京100029 
王作新 北京化工大学可控化学反应科学与技术基础教育部重点实验室, 北京100029 
段雪 北京化工大学可控化学反应科学与技术基础教育部重点实验室, 北京100029 
摘要: 本文采用以ASED-MO(含原子对排斥的EHMO法)为基础的结构自动优化的EHTOPT程序,对镁铝水滑石(LDHs)层板与层间阴离子相互作用进行了理论研究.以Mg6Al2(OH)16X·H2O为分子结构单元,计算并分析了与不同层间阴离子形成稳定结构的能量变化、成键状况及电荷转移情况,揭示了层间作用力的本质.结果表明,LDHs层板与层间阴离子间存在静电吸引、氢键等非共价键弱相互作用,且氢键作用为主,其强弱与阴离子电荷分布
关键词: ASED-MO方法  镁铝水滑石  水滑石  理论研究
基金项目: 北京市自然科学基金资助项目(No.2002016)
Abstract: The interaction of the intercalated anions with the cationic sheets in ma gnesium aluminum layered double hydroxides has been in vestigated using the ASED-MO method.The energy changes,and the nature of the bonding have been studied during the formation of the layered structure with different anions,based on the model Mg6Al2(OH)16 X·H2 O.The calculations have shown that both Coulombic and hydrogen bonding inte ractions exist in the layered structure,and the strength of the hydrogen bonding interaction is con nected with the charge distribution of the anion and its orientation in space.Furthermore,it indicates that the variation in acid-base prop erties of the layers is affected by the charge distribution of the int ercalated anion.
Keywords: ASED-MO method  Mg-Al hydr otalcites  hydrotalcite  theoretical study
投稿时间:2001-05-28 修订日期:2001-07-09
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罗青松,李蕾,王作新,段雪.镁铝水滑石层板与层间阴离子相互作用的理论研究[J].无机化学学报,2001,17(6):835-842.
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