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Ternary rare earth and actinoid transition metal carbides viewed as carbometalates

机译:三元稀土和act系过渡金属碳化物被视为金属碳酸盐

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Ternary carbides A(x)T(y)C(z) (A = rare earth metals and actinoids; T = transition metals) with monoatomic species C4- as structural entities are classified according to the criteria (i) metal to carbon ratio, (ii) coordination number of the transition metal by carbon atoms, and (iii) the dimensionality of the anionic network [TyCz](n-). Two groups are clearly distinguishable, depending on the metal to carbon ratio. Those where this ratio is equal to or smaller than 2 may be viewed as carbometalates, thus extending the sequence of complex anions from fluoro-, oxo-, and nitridometalates to carbometalates. The second group, metal-rich carbides with metal to carbon ratios equal to or larger than 4 is better viewed as typical intermetallics ("interstitial carbides"). The chemical bonding properties have been investigated by analyzing the Crystal Orbital Hamilton Population (COHP). The chemical bonding situation with respect to individual T-C bonds is similar in both classes. The main difference is the larger number of metal-metal bonds in the crystal structures of the metal-rich carbides. (c) 2006 Elsevier Inc. All rights reserved.
机译:根据标准(i)金属与碳的比率对具有单原子物种C4-作为结构实体的三元碳化物A(x)T(y)C(z)(A =稀土金属和and系元素; T =过渡金属)进行分类。 (ii)过渡金属与碳原子的配位数,以及(iii)阴离子网络[TyCz](n-)的尺寸。根据金属与碳的比例,两组可以明显区分。该比率等于或小于2的那些可被视为碳酸盐,因此将络合阴离子的序列从氟金属,氧代金属和亚硝基金属酸盐扩展到碳酸盐。第二类,金属与碳之比等于或大于4的富金属碳化物,最好被视为典型的金属间化合物(“间隙碳化物”)。通过分析晶体轨道汉密尔顿人口(COHP),研究了化学键合性质。在两个类别中,关于单个T-C键的化学键合情况相似。主要区别在于,富金属碳化物的晶体结构中存在大量的金属-金属键。 (c)2006 Elsevier Inc.保留所有权利。

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