
Wednesday, April  2, 2008 : 1:40 p.m.
Regional-Scale Chemical Evolution of Groundwater in the Wilcox Aquifer, Northern Mississippi Embayment
This study aims to integrate groundwater geochemistry and numerical modeling to evaluate groundwater residence time within the Wilcox aquifer in the northern Gulf Coastal Plain. We are focusing on the confined section of the aquifer (with well depths ranging between 116 and 518 meters) along the regional flow path, which extends from the subcrop of the Wilcox Group in southeastern Missouri  to the farthest downgradient municipal wells southwest of Memphis Paducah , Kentucky Gulf of Mexico ). Second, increasing enrichment with distance from the recharge area in a confined aquifer is consistent with paleoclimatic variations (i.e., depletion of the isotopic composition of recharge over time). To resolve these two explanations, estimate residence time and assess cross-formational leakage, we plan to use 36Cl,and temperature in numerical models of groundwater flow coupled to solute transport and heat flow.
Estifanos Haile, University of Kentucky EDUCATION Ph. D., Geology, University of Kentucky (UK), ~Dec 2008 Licentiate, Hydrogeology, Royal Institute of Technology (KTH), Sweden, 2005 B. Sc., Geology, Addis Ababa University, Ethiopia, 1998 WORK EXPERIENCE Jan 2006 – present: Teaching Assistant, UK. Dec 2002 to Dec 2005: Teaching and Research Assistant, KTH, Sweden. Sep 1998 – Aug 2000: Graduate Assistant, University of Asmara, Eritrea.