Abstracts
IAH_CNC_WEB2
IAH_CNC_WEB2
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
171 - Evaluating the Effects of Increased Lithium Brine<br />
Extraction from the Salar de Atacama: Conceptual and Numerical<br />
Groundwater Models<br />
Mark King<br />
Groundwater Insight, Inc., Canada<br />
Steve Shikaze<br />
Matrix Solutions Inc., Canada<br />
Hector Maya<br />
Rockwood Lithium, Chile<br />
Jaime Solari & Laura Vitoria<br />
SGA, Chile<br />
Most of the world’s lithium reserves occur in dry salt lakes (salars) located in a section of<br />
the high Andes near the common borders of Chile, Argentina and Bolivia. Almost all of<br />
the current lithium production from this region originates from two companies operating<br />
in the Salar de Atacama. One of these companies, Rockwood Lithium, is currently seeking<br />
government approval to increase its brine production rate. This paper provides an overview<br />
of conceptual and numerical groundwater models constructed to evaluate the potential<br />
impacts of this proposed increase in brine extraction.<br />
The Salar de Atacama is located in an extreme desert environment, with annual precipitation<br />
of less than 50 mm/yr. The lithium-containing brine is located under the flat surface<br />
of the salar, in a porous evaporite matrix. The nucleus of the salar contains brine with as<br />
much as ten times the dissolved solids content of seawater. Meanwhile, subsurface waters<br />
in the outer border areas of the basin are relatively fresh, and are used as a freshwater<br />
resource. A key environmental feature of the Salar de Atacama are the shallow border lagoons,<br />
which are an important breeding habitat for migratory flamingoes. Consequently, a<br />
key criteria for any increase in brine pumping rates is that the water levels in these shallow<br />
border lagoons remain unaffected.<br />
In this environment of extreme salinity contrasts, the effects of increased brine pumping<br />
were evaluated with the numerical model SEAWAT. This numerical code has the capability<br />
of simulating density-dependent flow, which is a key process in the salar border area,<br />
where there is an interface between subsurface brines and saline to fresh waters. In this<br />
evaluation, local-scale SEAWAT models were coordinated with a regional-scale, flow-only<br />
MODFLOW model. This paper presents an overview of the conceptual and numerical<br />
approaches used to evaluate this unique and complex environment.<br />
131 - A Conceptual Model for Pore Water Release from Coal Waste<br />
Rock Piles in the Elk Valley, British Columbia, Canada<br />
Terryn Kuzyk, S. Lee Barbour, & M. Jim Hendry<br />
Department of Civil and Geological Engineering, University of Saskatchewan, Saskatoon,<br />
Saskatchewan, Canada<br />
118 IAH-CNC 2015 WATERLOO CONFERENCE