The distribution of total and methylmercury concentrations in soils near the Idrija mercury mine, Slovenia, and the dependence of the mercury concentrations on the chemical composition and organic carbon levels of the soil

• Published in: Environmental earth sciences Vol. 65; no. 4; pp. 1309 - 1322
• Main Authors: Tomiyasu, Takashi, Matsuyama, Akito, Imura, Ryusuke, Kodamatani, Hitoshi, Miyamoto, Junko, Kono, Yuriko, Kocman, David, Kotnik, Jože, Fajon, Vesna, Horvat, Milena
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer-Verlag 01-02-2012; Springer Nature B.V
• Subjects: Biogeosciences; Carbon; Chemical composition; Correlation coefficient; Earth and Environmental Science; Earth Sciences; Earthquakes; Environmental Science and Engineering; Forest soils; Freshwater; Geochemistry; Geological hazards; Geology; Hydrology/Water Resources; Mercury; Methylmercury; Mine tailings; Mining; Organic carbon; Organic contaminants; Original Article; River flow; Rivers; Seismic activity; Soil contamination; Spectrometry; Terraces; Terrestrial Pollution; Vertical distribution; Water analysis; X-ray fluorescence; Slovenia; Slovenia, Idrija R; Soil; TOC; Total mercury; XRF; Methylmercury; Idrija mercury mine
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-011-1379-z

Although the mining activity of the Idrija mine in Slovenia ceased in 1995, a large amount of mining dregs containing high concentrations of mercury remains in the area. The mining dregs were transported with river flow and deposition along the Idrija River. To estimate the dispersion and change in the chemical form of mercury, a total of 28 soil core samples were taken around the river. The individual core samples were separated into layers for the analysis of their chemical composition, carbon contents, total mercury (T-Hg) and methylmercury (MeHg) concentrations. The chemical composition measured by X-ray fluorescence spectrometry was useful to estimate the dispersion of tailings: the fluvial terrace soil had a chemical composition similar to that of the tailings and could be distinguished clearly from the forest soil. The highest T-Hg concentration, 1,100 mg kg
−1
, was observed in the fluvial terrace soil near the mine. Although the concentration decreased gradually along with distance from the mine, concentrations higher than 200 mg kg
−1
of T-Hg were still observed in the fluvial terrace soil approximately 20 km downstream from the mine. In the vertical distribution of T-Hg in the hillslope soil, a higher value was observed in the upper layers, which suggests the recent atmospheric deposition of mercury. The concentration of MeHg was the lowest at the riverside and higher in the hillslope soil, which was the opposite of the T-Hg distribution. The total organic carbon content tracked similarly with the distribution of MeHg and a linear relation with a significantly high correlation coefficient was obtained. The distinction may be related to the different dispersion process of mercury, and the organic carbon contents may be an important factor for MeHg formation.