Abstracts
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282 - Evaluating mining impacts on groundwater quality in Lake<br />
Poopó basin, Bolivia using geochemical and isotope tracers<br />
Sylvia Barroso 1 , Ronald Zapata 2 & Ramon Aravena 3<br />
1<br />
BC Ministry of Forests, Lands and Natural Resources, Nanaimo, British Columbia, Canada<br />
2<br />
Department of Engineering – University of San Francisco Xavier, Sucre, Bolivia<br />
3<br />
Department of Earth & Environmental Sciences – University of Waterloo, Waterloo,<br />
Ontario, Canada<br />
Historical and present mining activities have seriously impacted water quality in the Bolivian<br />
Altiplano (High Plain). The environmental effects of mining in the Poopó River<br />
and Antequera River sub-watersheds of the Lake Poopó Basin were considered, along<br />
with physiography, geology, and mine waste management. Stable isotopes, 18 O and 2 H in<br />
water, and 34 S and 18 O in sulfate complemented with chemical data were used to evaluate<br />
the impacts of mine tailings in groundwater. In the Poopó River watershed, tailings leachate,<br />
and slurry from the refinement of zinc and lead ore was held in a ~5 hectare tailings<br />
impoundment situated at the apex of a colluvial fan, and isolated from the adjacent river.<br />
In the Antequera River watershed, a >10 ha tailings reservoir was located within the river<br />
channel, creating a dilute acidic (pH 2) mixture of precipitation and wastewater. As a result<br />
of evaporation, the isotopic composition of water in the tailings impoundments was higher<br />
than in groundwater and surface water. Springs, rivers, and shallow groundwater had an<br />
average isotopic composition of -13‰, and -100‰ for δ 18 O and δ 2 H, respectively. Water<br />
isotopes in groundwater from drilled wells were lower (median δ 18 O=-15‰, and δ 2 H=-<br />
110‰), originating from recharge at higher elevation. Stable isotopes of sulfate combined<br />
with geochemical data were useful indicators of mixing between polluted and ambient<br />
waters. In comparison to other sources, tailings samples had a very negative sulfate isotope<br />
composition with average values of -5‰ and -12‰ for δ 34 S and δ 18 O, respectively. Water<br />
sources impacted by mine waste had lower sulfate isotope composition and higher concentrations<br />
of cadmium and other trace metals. In Poopó impacts were evident in shallow<br />
groundwater adjacent to the tailings pond. In Antequera, impacts of leachate from the<br />
impoundment were noted at distance in down gradient groundwater and surface waters.<br />
Options for provision of fresh water in this region are limited. Groundwater in drilled wells<br />
contained elevated, naturally occurring, boron, aluminum and arsenic; while shallow dug<br />
wells were contaminated by natural and anthropogenic pollutants, including tailings leachate<br />
and evaporite salts. Sources of uncontaminated water were low temperature springs and<br />
creeks at higher elevation, upstream of industrial activities and human settlements.<br />
IAH-CNC 2015 WATERLOO CONFERENCE<br />
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