GSA Connects 2022 meeting in Denver, Colorado

Paper No. 257-9
Presentation Time: 3:55 PM

EXPERIMENTAL LEACHING STUDY OF LITHIUM ORES IN VARIOUS ENVIRONMENTAL ACIDS


TOUPAL, Jonas1, VANN, David R.1, ZHU, Chen2 and GIERE, Reto1, (1)Department of Earth and Environmental Science, University of Pennsylvania, 240 S. 33rd Street, Philadelphia, PA 19104, (2)Department of Geological Sciences, Indiana University, 1001 E. 10th Street, Bloomington, IN 47405

Transitioning to a carbon-neutral future requires an increase in mining of metals used in the green infrastructure, such asLi [1]. Lithium production has nearly doubled between 2016-2020 [2]. There is limited information on the aqueous geochemical signatures near Li deposits and the changes due to their mining [3]. Elevated Li concentrations have been reported in creeks and rivers near Cínovec, Czech Republic, a Li-mica deposit [4], in fresh waters near a spodumene deposit in SE Ireland [5], and high Li concentrations are observed in a stream running through an active Portuguese spodumene mine [6]. Here, we expose four different Li ores (zinnwaldite; lepidolite; spodumene pegmatite; greisen rich in Li-mica) to four different environmentally common acids (dilute sulfuric acid; acetic acid; oxalic acid; deionized water as control solution) with the goal of understanding the potential Li release from these materials under these conditions. The experiment is set up to run for nine months.

After six months of the experiment (9/10 samples collected), Li concentrations reach ~5 mg/L at the 6-month point, following a logarithmic trend. It is of note that the lepidolite sample behaves opposite to the other samples, having a minimum Li value at the 6-month point. We interpret the decline in Li concentrations post peak value as being caused by the precipitation of secondary minerals such as clays, as shown in [7]. Our study also aims to include Si isotope analysis to understand the weathering rates, SEM and XRD analysis to characterize the precipitates, and PHREEQC thermodynamic modeling of the potentially precipitating secondary phases.

Our results will be applicable to hard-rock Li deposits as they showcase the potential release of significant amounts of Li into the environment, but also hint at the natural remediation process via secondary mineral precipitation.

[1] Choubey et al. (2016) Minerals Engineering 89:119-137.

[2] USGS (2015-2021) Mineral Commodity Summaries.

[3]Bradley et al. (2017) USGS Report 2010-5070-0.

[4] Toupal et al.(2022) J of Geochemical Exploration234.

[6] Kavanagh et al. (2018) Resources57:1-29.

[6] Rodrigues (2019) Environmental Earth Sciences 78:533.

[7] Li and Liu (2020) Geochemica et Cosmochimica Acta284:156-172.