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Fundamental studies of stepwise ionic solvation
The theoretical solvation of aqueous species and ions is paramount to the understanding of
the properties under most conditions of relevance to reactions occurring in crustal fluids.
These solvation properties are still not adequately represented through theoretical means even
at relatively low temperatures and pressures. Currently vast strides are being made in
fundamental cluster chemistry at Berkeley (especially of water)
and experimental mass spectrometry at Alberta.
Our research program involves the measurement of
the energetics associated with ligand clustering around positive and negative ions and will build
on the recent molecular results for ionic clustering. For this purpose
we have constructed (after many years of machining) a Kebarle-style pulsed-electron high pressure
mass spectrometer (p-HPMS) using high-temperature enthalpy calorimeters as models. Imperative to this
measurement technique is the unambiguous knowledge of temperature and sampling conditions.
Concurrent analyses of structural and theoretical values using GAUSSIAN are also underway.
Long term uses in addition to the elucidation of fundamental reaction schemes
are involved with the development of new theoretical approaches for the prediction of high
temperature and pressure properties of various
important geological species in water.
The same measurements are also directly informative on the nature and chemistry of volcanic
gas reactions and gaseous species in the stratisphere.
Tour and history of the p-HPMS Laboratory
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Dr. Jamey K. Hovey Ion-cluster Laboratory Leader. | ||
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Prof. Terry Seward Geochemistry Group Leader. | ![]() |
Dr. Oleg Suleimenov Postdoctoral Fellow (plans to start working with us soon .... |
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