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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Calculation of boron-isotope fractionation between B(OH)(3)(aq) and B(OH)(4)(-)(aq)
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Calculation of boron-isotope fractionation between B(OH)(3)(aq) and B(OH)(4)(-)(aq)

机译:B(OH)(3)(aq)和B(OH)(4)(-)(aq)之间的硼同位素分馏的计算

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Density functional and correlated molecular orbital calculations (MP2) are carried out on B(OH)(3)center dot nH(2)O clusters (n = 0, 6, 32), and B(OH)(4)(-)center dot nH(2)O (n = 0, 8, 11, 32) to estimate the equilibrium distribution of B-10 and B-11 isotopes between boric acid and borate in aqueous solution. For the large 32-water clusters, multiple conformations are generated from ab initio molecular dynamics simulations to account for the effect of solvent fluctuations on the isotopic fractionation. We provide an extrapolated value of the equilibrium constant alpha(34) for the isotope exchange reaction B-10(OH)(3)(aq) + B-11(OH)(4)(-) (aq) = B-11(OH)(3)(aq) + B-11(OH)(4)(-) (aq) of 1.026-1.028 near the MP2 complete basis set limit with 32 explicit waters of solvation. With some exchange-correlation functionals we find potentially important contributions from a tetrahedral neutral B(OH)(3)center dot H2O Lewis acid-base complex. The extrapolations presented here suggest that DFT calculations give a value for 10(3)In alpha(34) about 15% higher than the MP2 calculations.
机译:在B(OH)(3)中心点nH(2)O簇(n = 0、6、32)和B(OH)(4)(-)上进行密度泛函和相关的分子轨道计算(MP2)中心点nH(2)O(n = 0、8、11、32)来估计水溶液中硼酸和硼酸盐之间B-10和B-11同位素的平衡分布。对于较大的32个水簇,从头算分子动力学模拟会生成多种构型,以说明溶剂波动对同位素分馏的影响。我们为同位素交换反应B-10(OH)(3)(aq)+ B-11(OH)(4)(-)(aq)= B-11提供了平衡常数alpha(34)的外推值(OH)(3)(aq)+ B-11(OH)(4)(-)(aq)为1.026-1.028,在MP2完整基准设定极限附近,具有32个明确的溶剂化水。通过一些交换相关功能,我们发现四面体中性B(OH)(3)中心点H2O Lewis酸碱复合物的潜在重要贡献。此处介绍的推断表明DFT计算得出的alpha(34)中10(3)In的值比MP2计算高出约15%。

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