Experimental Investigation of the Complete Inner Shell Hydration Energies of Ca2+: Threshold Collision-Induced Dissociation of Ca2+(H2O)x Complexes (x=2-8)

被引:35
作者
Carl, Damon R. [1 ]
Armentrout, P. B. [1 ]
机构
[1] Univ Utah, Dept Chem, Salt Lake City, UT 84112 USA
基金
美国国家科学基金会;
关键词
GAS-PHASE REACTIONS; SODIUM-CATION INTERACTIONS; SEQUENTIAL BOND-ENERGIES; CHARGED ALKALINE-EARTH; ION FUNNEL INTERFACE; ACIDIC AMINO-ACIDS; BINDING-ENERGIES; THEORETICAL DISSECTION; METAL DICATIONS; WATER;
D O I
10.1021/jp301446v
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The sequential bond energies of Ca2+(H2O)(x) complexes, where x = 1-8, are measured by threshold collision-induced dissociation (TCID) in a guided ion beam tandem mass spectrometer. From an electrospray ionization source that produces an initial distribution of Ca2+(H2O)(x) complexes where x = 6-8, complexes down to x = 2 are formed using an in-source fragmentation technique. Ca2+(H2O) cannot be formed in this source because charge separation into CaOH+ and H3O+ is a lower energy pathway than simple water loss from Ca2+(H2O)(2). The kinetic energy dependent cross sections for dissociation of Ca2+(H2O)(x) complexes, where x = 2-9, are examined over a wide energy range to monitor all dissociation products and are modeled to obtain 0 and 298 K binding energies. Analysis of both primary and secondary water molecule losses from each sized complex provides thermochemistry for the sequential hydration energies of Ca2+ for x = 1-8 and the first experimental values for x = 1-4. Additionally, the thermodynamic onsets leading to the charge separation products from Ca2+(H2O)(2) and Ca2+(H2O)(3) are determined for the first time. Our experimental results for x = 1-6 agree well with previously calculated binding enthalpies as well as quantum chemical calculations performed here. Agreement for x = 1 is improved when the basis set on calcium includes core correlation.
引用
收藏
页码:3802 / 3815
页数:14
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