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磷酸钾水溶液中的离子水合与缔合

Ion hydration and association in aqueous potassium phosphate solutions.

作者信息

Eiberweiser Andreas, Nazet Andreas, Hefter Glenn, Buchner Richard

机构信息

†Institut für Physikalische und Theoretische Chemie, Universität Regensburg, Universitätsstr. 31, D-93040 Regensburg, Germany.

‡Chemistry Department, Murdoch University, 90 South Street, Murdoch, WA 6150, Australia.

出版信息

J Phys Chem B. 2015 Apr 23;119(16):5270-81. doi: 10.1021/acs.jpcb.5b01417. Epub 2015 Apr 9.

Abstract

Ionic hydration and ion association in aqueous solutions of KH2PO4, K2HPO4, and K3PO4 at 25 °C up to high concentrations have been investigated using dielectric relaxation spectroscopy (DRS). The three phosphate anions were found to be extensively hydrated, with total hydration numbers at infinite dilution of ~11 (for H2PO4(-)), ~20 (HPO4(2-)), and ~39 (PO4(3-)). These values are indicative of the existence of a second hydration shell around HPO4(2-) and especially PO4(3-). Two types of hydrating water molecules could be quantified: irrotationally bound (ib, H2O molecules essentially "frozen" on the DRS time scale) and "slow" (loosely bound water molecules with identifiably slower dynamics than bulk water). For H2PO4(-) over the entire concentration range and for HPO4(2-) and PO4(3-) at concentrations c ≲ 1 mol L(-1), only "slow" H2O was detected; however, at higher concentrations of the latter two anions, an increasing fraction of ib water appears, making up ~50% of the total hydration number close to the saturation limit of K2HPO4. Contrary to common belief, all three salts showed significant ion pair formation, with standard association constants of the 1:1 species increasing in the order: KH2PO4(0)(aq) < KHPO4(-)(aq) < KPO4(2-)(aq). The main type of ion pair in solution shifted from solvent-shared ion pairs (SIPs) to double-solvent-separated ion pairs (2SIPs) in the same sequence.

摘要

利用介电弛豫光谱(DRS)研究了25℃下KH2PO4、K2HPO4和K3PO4水溶液中离子水合作用及离子缔合,直至高浓度情况。发现三种磷酸根阴离子都被大量水合,在无限稀释时的总水合数分别约为11(对于H2PO4(-))、约20(HPO4(2-))和约39(PO4(3-))。这些数值表明在HPO4(2-)尤其是PO4(3-)周围存在第二水合层。可以定量两种类型的水合水分子:非旋转结合(ib,H2O分子在DRS时间尺度上基本“冻结”)和“慢”水(与本体水相比动力学明显较慢的松散结合水分子)。对于整个浓度范围内的H2PO4(-)以及浓度c≲1 mol L(-1)时的HPO(2-)和PO4(3-),仅检测到“慢”H2O;然而,对于后两种阴离子的较高浓度,ib水的比例增加,在接近K2HPO4饱和极限时占总水合数的约50%。与普遍看法相反,所有三种盐都显示出显著的离子对形成,1:1物种的标准缔合常数按以下顺序增加:KH2PO4(0)(aq) < KHPO4(-)(aq) < KPO4(2-)(aq)。溶液中主要的离子对类型以相同顺序从溶剂共享离子对(SIPs)转变为双溶剂分离离子对(2SIPs)。

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