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Thomas J. Dick

Thomas J. Dick
Department of Chemistry and Biochemistry
Center for Computational Sciences
Duquesne University
600 Forbes Avenue
Pittsburgh, PA 15282-1530
Fax: (412) 396-5683

Phone: (412) 396-4627
E-mail: dick251@duq.edu

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Research Summary

CO 2 Sequestration in Brine Aquifers

Description: The combustion of fossil fuels releases large amounts of carbon dioxide into the atmosphere, which is known to cause global warming. One idea to get rid of the excess CO 2 is to use brine aquifers to sequester the gas by using mineral trapping in brine aquifers, where the CO 2 is introduced into solution, converted to carbonate, and associates ionically with metal ions to from insoluble metal carbonates. Our interest is to understand how brines can influence the sequestration of CO 2 in brine aquifers.

Goals: The goals of this project are to apply computational techniques to determine the properties under which CO 2 may be best sequestered in brine aquifers. FEP/MC simulations are used to determine the solubility of CO 2in various brine solutions and hybrid QM/MM dynamics simulations are performed to look at the conversion of CO 2 to carbonate in the presence of high concentrations of ions. Together, these simulations will provide a molecular explanation of the factors that most influence the CO 2 sequestration process from a thermodynamic, kinetic, and structural aspect.

Methane Clathrates- An Alternative Energy Source

Description: Gas clathrates are viable energy resources. Methane stored in naturally occurring clathrates potentially hold enough methane to ensure supply for many years; methane clathrates are also known to cause blockage in the natural gas pipelines. Clathrates have also been discussed as possible storage sites in CO 2 sequestration. Although these have been known about for over a century, there is little known about the clusters on an atomistic scale and what structural properties are critical in the formation and dissipation of gas clathrates.

Goals: The goals of this project are to apply computational techniques to determine the properties under which clathrates may be utilized as effective energy sources. QM calculations are used to determine stable clathrate structures and to calculate the interaction energy between the gas and the clathrate shell. MC simulations map out the phase diagram of the clathrate and provide structural information on the average configurations of the clathrates under their naturally occurring conditions. Together, these simulations will provide an understanding of the formation, dissipation, and gas exchange of clathrates from a thermodynamic and structural viewpoint.

 

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