Abstract
A suggested mechanism for hydroxide mobility in water identifies the rate limiting step as a cleavage of a second shell hydrogen bond which converts a H7O4- ion (triply coordinated hydroxide) to (HOHOH)- (deprotonated water dimer). Proton transfer is enabled by an additional O-O bond contraction, not required in H5O2+. This explains why the activation energy for hydroxide mobility is larger than that of proton mobility by about 0.5 kcal/mol. The transfer cycle is terminated by hydrogen-bond formation to the other oxygen center. Available experimental data, and most of the computational results, can be rationalized in the framework of the above model.
| Original language | English |
|---|---|
| Pages (from-to) | 247-252 |
| Number of pages | 6 |
| Journal | Chemical Physics Letters |
| Volume | 319 |
| Issue number | 3-4 |
| DOIs | |
| State | Published - 17 Mar 2000 |
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