Assessment of trace metal contamination in stream sediments of the Tuul River, Mongolia
Abstract
Thirty four sediment samples were collected in Ulaanbaatar basin, along the Tuul River which is the main source of water for the capital city Ulaanbaatar, Mongolia. The catchment can be divided three parts (upper, middle, and lower) according to the extent of urbanization. The upper part of the river basin is comparatively less affected by human activity and it can be represent the natural background condition. The middle part is the urban area of Ulaanbaatar and lower part extends SW of the end of the urban area mostly used for agriculture and farming activity. The present study focused on the levels of potentially toxic metals such as As, Pb, Zn, Cu, Ni and Cr in order to assess the extent of environmental pollution and to discuss the origin of these contaminants in sediments of the Tuul River using X-ray fluorescence analyses. Metal concentrations in the sediments are discussed by comparison with average Upper Continental Crust values (UCC) and ecological risk assessment by reference to sediment quality guidelines (SQG). The results showed thet average abundances of metals are measurable contrast between upper, middle and lower parts of the river. The Upper part and its surrounding area's sediment signature indicated that more depletion comparatively other parts (Pb, Zn, Cu, Ni and Cr), whereas enrichment sign did not detect. However, among the Upper part sediments, two samples (NA1 and NA2) enriched with trace metals which sampled from Nalaikh area were significantly affected by coal mining activity. Most metals are (As, Pb, Zn, Cu and Ni) higher in the middle part (within the city) than the upper and lower part due to the urban activities. The small tributaries such as Selbe, Uliastai, Gachuurt and Tolgoit were significantly affected by urban activities and highest values are detected from them. Lower part significantly enriched with Cr (av 98 ppm). Highest concentration of Cr (183 ppm) was at Shuvuu which is receiving point of domestic and industrial wastewater discharge. However all three parts show depletion in some chalcophile and HFSE elements (Cu, Ni, Cr, Sr, Nb, Zr, Th, Sc). This depletion of elements relative to UCC suggest that the river sediments were derived from a highly felsic crustal source. The assessment of ecological risk assessment result showed that adverse aquatic biological effects caused by As and Cr. While, concentration of Pb, Zn, Cu and Ni are generally below their respective Threshold effect level (TEL), in middle part reaches to reach values bordering on the Probable effect level (PEL). This indicated that anthropogenic contribution in the urban areas, increasing values above a naturally low regional background.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2011
- Bibcode:
- 2011AGUFM.V13B2596D
- Keywords:
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- 1051 GEOCHEMISTRY / Sedimentary geochemistry;
- 1065 GEOCHEMISTRY / Major and trace element geochemistry