The characterization, mobility, and persistence of roaster-derived arsenic in soils at Giant Mine, NWT

Citation data:

Applied Geochemistry, ISSN: 0883-2927, Vol: 82, Page: 102-118

Publication Year:
2017
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DOI:
10.1016/j.apgeochem.2017.04.004
Author(s):
Mackenzie J. Bromstad, Lori A. Wrye, Heather E. Jamieson
Publisher(s):
Elsevier BV
Tags:
Environmental Science, Earth and Planetary Sciences
article description
Approximately 20,000 tonnes of arsenic (As)-bearing emissions from roasting gold (Au)-bearing arsenopyrite ore were aerially released from 1949 to 1999 at Giant Mine, near Yellowknife, Canada. Soil samples collected within 4 km of the former roaster from sites undisturbed by mining or other human activity contain up to 7700 mg/kg total As. Total As concentrations are highest within a few cm of the surface, and particularly enriched in soil pockets on rock outcrops. Scanning electron microscopy and synchrotron microanalysis show that roaster-derived arsenic trioxide (As 2 O 3 ) has persisted in shallow soils in the area. Roaster-generated maghemite and hematite are also present. These anthropogenic forms of As are much more common in near-surface soils than natural As-bearing minerals. Comparison of the proportions of As, Sb, and Au concentrations in outcrop soil samples and historic As 2 O 3 -rich dust captured by emission controls suggest most of the roaster-derived As in soils at Giant was likely deposited before 1964. Topographic restriction by rock outcrops and a dry, cold climate likely contribute to the persistence of As 2 O 3 in outcrop soils.

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