Cadmium sources, mobility, and natural attenuation in contrasting environments: carbonate-rich and carbonate-poor rocks in the Capillitas mineral deposit, Argentina.

YACIUK P; COLOMBO F; LECOMTE KL; DE MICCO G; BOHÉ AE

APPLIED GEOCHEMISTRY

PERGAMON-ELSEVIER SCIENCE LTD

Lugar: Amsterdam; Año: 2022 vol. 136

0883-2927

Cadmium is one of the most toxic metals commonly released due to mining activities. However, its dynamic in contrasting mining environments has not been exhaustively studied. Through mineralogical and hydrochemical analyses, this study identifies Cd mineral sources and its mobility in surficial waters from two different mining environments (i.e. carbonate-rich and carbonate-poor mineral assemblages) within the polymetallic Capillitas deposit, in NW Argentina. Furthermore, a freshwater tributary stream without mining operations is analyzed as natural background. Results show that sphalerite weathering is the main process releasing Cd into surficial waters in both locations. Sphalerite is Cd-rich in the carbonate-poor rocks of the high-to intermediate-sulfidation environment. At this site, the mineral assemblage is poorly neutralizing and the metal dissolved concentrations increase downstream. The carbonate-rich rocks release Cd up to 1.25 mg L