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SENSITIVITY ANALYSIS of URANIUM SPECIATION MODELING in GROUNDWATER SYSTEMS with a FOCUS on MOBILITY Andrew Scott Clemson University

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SENSITIVITY ANALYSIS of URANIUM SPECIATION MODELING in GROUNDWATER SYSTEMS with a FOCUS on MOBILITY Andrew Scott Clemson University Clemson University TigerPrints All Dissertations Dissertations 12-2010 SENSITIVITY ANALYSIS OF URANIUM SPECIATION MODELING IN GROUNDWATER SYSTEMS WITH A FOCUS ON MOBILITY Andrew Scott Clemson University Follow this and additional works at: https://tigerprints.clemson.edu/all_dissertations Part of the Environmental Engineering Commons Recommended Citation Scott, Andrew, "SENSITIVITY ANALYSIS OF URANIUM SPECIATION MODELING IN GROUNDWATER SYSTEMS WITH A FOCUS ON MOBILITY" (2010). All Dissertations. 635. https://tigerprints.clemson.edu/all_dissertations/635 This Dissertation is brought to you for free and open access by the Dissertations at TigerPrints. It has been accepted for inclusion in All Dissertations by an authorized administrator of TigerPrints. For more information, please contact [email protected]. SENSITIVITY ANALYSIS OF URANIUM SPECIATION MODELING IN GROUNDWATER SYSTEMS WITH A FOCUS ON MOBILITY __________________________ A Dissertation Presented to The Graduate School of Clemson University __________________________ In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy Environmental Engineering and Science __________________________ by Andrew Lee Scott December 2010 __________________________ Accepted by: Dr. Timothy A. DeVol, Committee Chair Dr. Alan W. Elzerman Dr. Robert A. Fjeld Dr. Brian A. Powell ABSTRACT Uranium is an important natural resource used in production of nuclear reactor fuel and nuclear weapons. The mining and processing of uranium has left a legacy of environmental contamination that remains to be addressed. There has been considerable interest in manipulating the oxidation state of uranium in order to put it into an environmentally immobile form. Uranium forms two stable oxidation states in nature, uranium (IV) being much less soluble than uranium (VI), and therefore the preferred state with regard to limiting the potential exposure of man. One of the tools used in evaluating potential effects of manipulating the natural systems to prefer U(IV) formation is chemical equilibrium modeling. These models show the thermodynamically preferred chemical species that are formed in a particular defined system. Chemical equilibrium modeling is very dependent on the data that is used to support the calculations, the initial definition of the system, and the other constraints placed on the reactions. This research is designed to show the relative effects of inorganic chemical perturbations in the particular systems modeled, as well as the effects of humic/fulvic acids, mineral and bacterial sorption and temperature (to a limited extent), with a focus on uranium solubility, by performing a sensitivity analysis using Geochemist’s Workbench, a commercially available chemical equilibrium software package. Four groundwater systems of interest were selected upon which to perform the sensitivity analysis: the Yucca Mountain (YM) J-13 well water system (Harrar, et al., 1990), the mean well water system from the Simpsonville, SC (SSC) area (Woodruff, 2002), the Savannah River National Laboratory (SRNL) F-Area groundwater system, and ii Idaho National Engineering and Environmental Laboratory (INEEL) Snake River aquifer system (Ayaz, et al, 2000). The results of the sensitivity analysis are presented in terms of metrics called the uranium ratio (UR) and the sensitivity index (SIUR), defined as follows: U aq ()mol URmin −URmax UR = and SIUR = U tot ()mol URbaseline Where: URmin = UR at the minimum constraint concentration evaluated URmax = UR at the maximum constraint concentration evaluated URbaseline = UR at the baseline for the system The discussion of the results of the sensitivity analysis focuses on the relative effect varying a given constraint has on the system, defined as follows: significant or major effects (SIUR >1), moderate effects (0.1 < SIUR < 1), minor effects (0.01 < SIUR < 0.1%), no apparent effects (SIUR <0.01%). The sensitivity analysis of the YM solubility controlled system indicated that aqueous carbonate concentrations dictated UR to a large extent. Phosphate and strontium, both of which were not included in the basis, were indicated to be of potential significance to uranium solubility in this system. Temperature also seems to have a strong role in uranium solubility in this system. Interestingly, pH seemed to have little effect on the UR. The presence, concentration and composition of the organic acid simulant appeared to be of little concern. iii The solubility controlled SSC system precipitated Soddyite and Quartz in the baseline case at equilibrium indicating oversaturation of silicon and uranium in the natural groundwater. Similarly to the YM system, carbonate seemed to dominate the uranium solubility of the system, but silicon and temperature also had significant effects. The presence, concentration and composition of organic acids in this system could effect aqueous uranium concentrations by as much as 20-30%. The SRNL system was modeled under both solubility and sorption controlled assumptions. The solubility controlled SRNL system was impressively unresponsive to physical, inorganic and organic constraint variations across the tested range, giving strong evidence that this system is indeed sorption controlled. Both pH and total uranium concentration exerted strong effects in the sorption controlled system, illustrating the importance of availability of sorption sites relative to the amount of uranium in solution. Other constraints, surprisingly including carbonate, had relatively little effect. The presence, concentration and composition of organic acids had little effect. Bacterial sorption was shown to have a significant potential to affect the aqueous uranium concentration in this system, especially as the total uranium in the system was reduced. The sorption controlled INEEL system showed much more sensitivity than did the - SRNL system, and seemed to be significantly (> 10%) effected by the variation of HCO3 + 2+ 2- - 2+ , pH, pe, Na , Ca , SO4 , Cl , and Mg in both the mineral-only and mineral-bacterial cases. The UR in this system was not shown to be sensitive to the presence, concentration or composition of organic acids. The mineral-only and mineral-bacterial sorption controlled systems behaved nearly identically. iv There are obvious limitations in the models and supporting data. Further, the sensitivity analysis did not evaluate synergistic or antagonistic effects of multiple constraint variability, except in a very rudimentary way. More research in these areas is suggested. Given these limitations, the sensitivity analysis can identify potentially unrecognized factors that may have a strong impact, and those that have little effect, on uranium mobility in the environment. This gives environmental scientists another tool to evaluate resource allocation and narrow down many potential avenues of research to those that have the greatest potential to bear fruit, ultimately aimed at defining and perhaps controlling uranium mobility in the environment. v DEDICATION This work is dedicated to my wife, Kim, without whose loving support, patience and encouragement it would not have been written; my daughter Jaime, for helping me keep it all in perspective; my son, Bradley, for generously giving up time with his Dad; my parents, Dwight and Mary Brown, for always being there to pick me up when I fell; my father and mother-in-law, Camille and Edna George, for considering me a son in every sense; and to my grandmother, Garnette Roll, who was unshakably convinced that one day, I would become a ‘Doctor’. vi ACKNOWLEDGEMENTS I would like to thank my advisors, Dr. Fjeld and Dr. DeVol, for their guidance, support, and wisdom. Their unflagging confidence and gentle criticism lead directly to the completion and quality of this work. I owe additional thanks to my committee members, Dr. Elzerman and especially Dr. Powell, for their assistance, time, and insightful comments. They contributed directly to the quality and completeness of this project. Dr. John Coates gave valuable advice and contributed by listening to, and providing feedback on, many of the concepts and ideas contained herein. I am grateful to the RES3T team in Germany for the provision of their database, which was so crucial to the sorption modeling. Dr. Craig Bethke, the author of Geochemist’s Workbench, seemed to always be available to provide assistance with the technical aspects of chemical equilibrium modeling with his software, as was the vendor, Tom Meuzlaar of Rock Ware. All the folks on the GWB listserver are also due thanks for providing much needed advice and feedback during the modeling effort. The staff, faculty, and students in the Department of Environmental Engineering and Earth Sciences were outstanding and supportive in too many ways to mention. Finally, I would like to thank the U.S. Army for providing this opportunity by selecting and funding me for this assignment, and specifically, Colonel Mark Melanson, for helping me to keep my focus on the objective. vii TABLE OF CONTENTS Page TITLE PAGE ................................................................................................................ i ABSTRACT .................................................................................................................. ii DEDICATION .............................................................................................................. vi ACKNOWLEDGEMENTS .......................................................................................... vii TABLE OF CONTENTS…………………………………………………………….
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