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Water Quality of the Yarlung Tsangpo (Brahmaputra) Huang Xiang and Mika Sillanpää November 19th, 2011, New Delhi International conference of ”River Waters: Perspectives and Challengies for Asia”
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Huang He Yangtze River Mekong River Salween River Irrawaddy Yarlung Tsangpo Ganges Indus Water Tower of Asia
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Yangtze River The longest river in Asia and the third longest in the world (6 300 km, 509 km in Tibet) It drains in total nearly 1/5 of China (1.8 million km 2, 23 060 km 2 in Tibet)
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The seventh longest river in Asia and the 12 th longest in the world (4 500 km, 509 km in Tibet) It drains in total 810 000 km 2 (38 300 km 2 in Tibet) Mekong River
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The second longest river in Southeast Asia (3 200 km, 1 393 km in Tibet) It drains in total 325 000 km 2 (102 500 km 2 in Tibet) Salween
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Yarlung Tsangpo The largest river on the Plateau Known as Brahmaputra downstream in India, it becomes the fifth largest river in the world (3 350 km, 2 057 km in Tibet) It drains in total 630 000 km 2 (240 480 km 2 in Tibet)
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Objectives -To assess temporal and spatial variations of chemical composition of the Yarlung Tsangpo -To address possible mechanisms governing the spatial variation of the water chemistry -To identify potential sources of contamination
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Sampling preparations Total of 35 quality parameters were under taken in consideration: Water temperature, pH, electrical conductivity (EC) and turbidity Major ions (Ca 2+, Na +, K +, Mg 2+, Cl -, NO 3 -, HCO 3 -, SO 4 2-, NH 4 +, PO 4 3- and F - ) Trace elements (Al, As, Ag, Cu, Fe, Li, Mn, Mo, Ti, Zn, Cd, Co, Cr, Ni, Pb and Hg) Total dissolved sulphur (S), -phosphorus (TDP), - nitrogen (TDN) and -silica (SiO 2 )
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UNIVERSITY OF EASTERN FINLAND LAEC Sampling
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Data interpretation - TDS in the Tibetan waters * Calculated according to Wetzel, 1975 TDS (mg/L)
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Water chemistry of the Tibetan rivers Mg 2+ Ca 2+ Na + K+K+ NO 3 - HCO 3 - SiO 2 SO 4 2- Cl - EC
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Data interpretation - Major ion composition
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Source: Huang X. Water Quality in the Tibetan Plateau: Chemical Evaluation of the Headwaters of Four Major Asian rivers”, dissertation, University of Eastern Finland, Finland, 2010.
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Source: Huang et al. River Res. Applic. 27: 113-121 (2011)
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UNIVERSITY OF EASTERN FINLAND LAEC No systematic water quality assessment over the Plateau! Current state As (246 µg/L)
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Source: Huang et al. Sci Tot. Env. 407: 6242-6254 (2009).
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Source: Huang et al. River Res. Applic. 27: 113-121 (2011)
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Mining in Gyama Four mines existed during the field work, but more mines are under construction Only sedimentation ponds to treat effluents Gyama stream drains into the Lhasa river, which is a tributary to Yarlung Tsangpo
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Cu, Pb, Zn, Fe, Cr, Mo,Mn and Al
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Why Tibetan waters - pressures on Tibetan waters
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Source: Huang et al. Sci Tot. Env. 407: 6242-6254 (2009).
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Source: Huang et al. River Res. Applic. 27: 113-121 (2011)
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Data interpretation - Major controlling factor in Yarlung Tsangpo
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Factors affecting water quality of Tibetan rivers Natural processes Mining activities Municipal wastes Climate change
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Thank you for your attention! Mika.Sillanpaa@lut.fi
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