Groundwater Dye Tracing in Lusaka, Zambia: Delineation of Contribution Areas for Drinking Water Sources

Monday, May 5, 2014: 5:00 p.m.
Curtis (Westin Denver Downtown)
Jonathan Levy, PhD , Geology and Environmental Earth Science, Miami University, Oxford, OH
Peter Petulo , Zambia Environmental Management Agency, Lusaka, Zambia
Joe Meiman , National Park Service, Park City, KY
Imasiku Nyambe , Geology, University of Zambia, Lusaka, Zambia
Samuel Mutiti , Biological & Environmental Sciences, Georgia College & State University, Milledgeville, GA

Lusaka, Zambia is a fast-growing city with more than 2 million people straining the karst groundwater which supplies 50% of its population. A well-developed epikarst underlying much of the city is often exposed by mining, increasing groundwater vulnerability. In densely populated areas, without proper waste or sewage disposal, drinking-water quality is severely degraded. To sustainably manage groundwater quantity and quality it is important to know groundwater recharge areas, flow paths, and travel times. Groundwater dye tracing is a commonly applied tool for such investigations but has not previously been used in Zambia.

Investigations focused on the community of Muloni, an unplanned development on the Cheta Limetsone west of Lusaka. Adjacent to Muloni is a commercial quarry where groundwater is intensively extracted. Muloni residents derive water from springs, boreholes, and hand-dug wells. Dye-tracing goals included delineation of source-water areas, quantification of groundwater travel times, and assessment of the possible effects of pumping at the quarries on drinking-water sources. Water quality assessments, based mainly on E. coli concentrations, were used to select the initial sites for the dye-trace injections.

Water quality results suggested separate recharge areas for some of the deep boreholes and the quarry (15 m below the village) which were relatively free of E. coli. The springs, shallow wells, and some boreholes seemed directly plumbed into the epikarst with E. coli concentrations in excess of 300 CFU/100 mL. Pumping from the quarries has resulted in no apparent reduction in spring flow.

Charcoal dye receptors were placed at springs, quarries, and shallow wells. Five liters of approximately 400 ppb Rhodamine WT and Fluorescein were injected into two different latrines upgradient of springs and wells. Receptors were collected and analyzed weekly over about three months, but no breakthrough was observed. Dye tracing experiments continue with higher dye concentrations at additional injection points.

Jonathan Levy, PhD, Geology and Environmental Earth Science, Miami University, Oxford, OH

Jonathan Levy is an Associate Professor in the Department of Geology and Environmental Earth Science at Miami University, Ohio.

Peter Petulo, Zambia Environmental Management Agency, Lusaka, Zambia
Peter Petulo works for the Zambia Environmental Management Agency in Lusaka, Zambia, focusing on groundwater resources. He will also soon be a post-graduate student at the University of Zambia.

Joe Meiman, National Park Service, Park City, KY
Joe Meiman has been a Hydrologist for the South East Region of the National Park Service since 2006. Before that he was the Park Hydrologist for Mammoth Cave National Park, 1989-2006.

Imasiku Nyambe, Geology, University of Zambia, Lusaka, Zambia
Imasiku Nyambe is a professor in the Department of Geology in the School of Mines at the University of Zambia in Lusaka. He is also the Directorate of Research and Graduate Studies and the Coordinator of the University of Zambia Integrated Water Resources Management Centre.

Samuel Mutiti, Biological & Environmental Sciences, Georgia College & State University, Milledgeville, GA
Sam Mutiti is an assistant professor at Georgia College and State University in the Department of Biological and Environmental Sciences. He received his Ph.D. in 2009 from the Department of Geology at Miami University. He received an M.S. from in Environmental Science, also at Miami University in 2003 and has previous BSc. and post-graduate degrees in exploration geology and computer science from the University of Wales and the University of Cambridge.