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由于溶剂共享离子对(SSIP)而导致水合壳层水的结构重排:以水合 MgCl 和 LaCl 溶液为例。

Restructuring of Hydration Shell Water due to Solvent-Shared Ion Pairing (SSIP): A Case Study of Aqueous MgCl and LaCl Solutions.

机构信息

Radiation & Photochemistry Division, Bhabha Atomic Research Centre, Homi Bhabha National Institute, Mumbai 400085, India.

School of Chemistry, Centre for Excellence in Basic Sciences, Mumbai 400098, India.

出版信息

J Phys Chem B. 2020 Sep 17;124(37):8141-8148. doi: 10.1021/acs.jpcb.0c05681. Epub 2020 Sep 3.

Abstract

Hydration of ions plays a crucial role in interionic interactions and associated processes in aqueous media, but selective probing of the hydration shell water is nontrivial. Here, we introduce Raman difference with simultaneous curve fitting (RD-SCF) analysis to extract the OH-stretch spectrum of hydration shell water, not only for the fully hydrated ions (Mg, La, and Cl) but also for the ion pairs. RD-SCF analyses of diluted MgCl (0.18 M) and LaCl (0.12 M) solutions relative to aqueous NaCl of equivalent Cl concentrations provide the OH-stretch spectra of water in the hydration shells of fully hydrated Mg and La cations relative to that of Na. Integrated intensities of the hydration shell spectra of Mg and La ions increase linearly with the salt concentration (up to 2.0 M MgCl and 1.3 M LaCl), which suggests no contact ion pair (CIP) formation in the MgCl and LaCl solutions. Nevertheless, the band shapes of the cation hydration shell spectra show a growing signature of Cl-associated water with the rising salt concentration, which is a manifestation of the formation of a solvent-shared ion pair (SSIP). The OH-stretch spectrum of the shared/intervening water in the SSIP, retrieved by second-round RD-SCF analysis (2RD-SCF), shows that the average H-bonding of the shared water is weaker than that of the hydration water of the fully hydrated cation (Mg or La) but stronger than that of the anion (Cl). The shared water displays an overall second-order dependence on the concentration of the interacting ions, unveiling 1:1 stoichiometry of the SSIP formed between Mg and Cl as well as La and Cl.

摘要

离子的水合作用在水介质中的离子相互作用和相关过程中起着至关重要的作用,但选择性探测水合壳层水并非易事。在这里,我们引入了同时进行曲线拟合的拉曼差(RD-SCF)分析,以提取水合壳层水的 OH 伸缩光谱,不仅适用于完全水合的离子(Mg、La 和 Cl),也适用于离子对。相对于具有等效 Cl 浓度的水相 NaCl,对稀释的 MgCl(0.18 M)和 LaCl(0.12 M)溶液进行 RD-SCF 分析,提供了完全水合的 Mg 和 La 阳离子水合壳层中水相对于 Na 的 OH 伸缩光谱。Mg 和 La 离子水合壳层光谱的积分强度随盐浓度线性增加(最高可达 2.0 M MgCl 和 1.3 M LaCl),这表明在 MgCl 和 LaCl 溶液中没有形成接触离子对(CIP)。然而,随着盐浓度的升高,阳离子水合壳层光谱的谱带形状显示出 Cl 相关水的特征越来越明显,这是形成溶剂共享离子对(SSIP)的表现。通过第二轮 RD-SCF 分析(2RD-SCF)检索到的 SSIP 中共享/介入水的 OH 伸缩光谱表明,共享水的平均氢键比完全水合阳离子(Mg 或 La)的水合水弱,但比阴离子(Cl)强。共享水显示出与相互作用离子浓度的二阶依赖关系,揭示了在 Mg 和 Cl 以及 La 和 Cl 之间形成的 SSIP 的 1:1 化学计量。

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