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The [9]-coordinated X site in the crystal structure of tourmaline-group minerals

机译:电气石族矿物晶体结构中的[9]配位X位点

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摘要

The [9]-coordinated X site in tourmaline is usually occupied by Na, Ca, K, or is vacant. In contrast to earlier statements in the literature our recent evaluation of 81 tourmaline samples with Al on the Z site has clearly shown that the distance, as could have been expected, is positively correlated to the average effective ionic radius of the X-site occupants (r = 0.98 for 81 tourmaline samples, with Al _6 at the Z site and (OH) _3 at the V site). Olenite and "oxy-rossmanite" samples, in which the V site is not completely occupied by OH, show a significant deviation to this correlation. X-site vacancies (up to ~0.7 apfu), as well as a significant variation of and distances, do not seem to have a significant effect on the distance. Tourmalines of the elbaiteolenite- rossmanite series (with Al _6 at the Z site) show a positive correlation between the and the distance (r = 0.80; 40 samples) due to inductive effects in the structure.
机译:电气石中[9]协调的X位点通常被Na,Ca,K占据或处于空位。与文献中较早的陈述相反,我们对81个电气石样品的Z位上有Al的最新评估清楚地表明,如所期望的,距离与X-的平均有效离子半径成正相关(81个电气石样品的r = 0.98,Z位置的Al _6和V位置的(OH)_3)。 V位不完全被OH占据的奥利石和“氧-罗斯曼”样品显示出与该相关性的显着偏差。 X位置的空位(最大〜约apfu 0.7)以及距离的显着变化,似乎对距离没有显着影响。 Elbaiteolenite-rossmanite系列的电气石(Z位置的Al _6为Al _6)由于结构中的感应效应,在距离之间显示正相关(r = 0.80; 40个样本)。

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