Effect of peat organic matter on sulfide weathering and thallium reactivity: Implications for organic environments
Abstract
Weathering of Tl-containing sulfides in a model (12-week) peat pot trial was studied to better understand their geochemical stability, dissolution kinetics, alteration products and the associated release and mobility of anthropogenic Tl in organic environments. We also present the effect of industrial acid rainwater on sulfide degradation and Tl migration in naturally acidic peat.
Sphalerite (ZnS) was much less stable in peat than other Tlcontaining sulfides (galena and pyrite), and thus acted as a major phase responsible for Tl mobilization. Furthermore, Tl incongruently leached out over Zn from ZnS, and accumulated considerably more in the peat solutions (<= 5 μg Tl/L) and the peat samples (<= 0.4 mg Tl/kg) that were subjected to acid rain watering compared to a deionized H2O regime.
This finding was in good agreement with the absence of secondary Tl-containing phases, which could potentially control the Tl flux into the peat. The behavior of Tl was not as conservative as Pb throughout the trial, since a higher peat mobility and migration potential of Tl was observed compared to Pb.
In conclusion, industrial acid precipitations can significantly affect the stability of ZnS even in acidic peat/ organic environments, making it susceptible to enhanced weathering and Tl release in the long term.