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Hydroclimatic development and anthropogenic impact on sediment loads in the Selenga catchment

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The present study focuses on the relationships between fluvial processes, climate and land-use changes in the Selenga River catchment. The results indicate that high sediment loads were reported both for altered and natural rivers. The reported multidecadal declines in sediment loads in the downstream part of the Selenga River can be attributed to the abandonment of cultivated lands and changing hydroclimatic factors, in particular a climate-driven decrease in water flows and intensified water use for irrigation purposes. Empirical sediment rating curves show that a series of peak flow events during spring and summer contributes to the main part (up to 98%) of the annual sediment and pollution loads. The highest contribution of flood sediment loads was determined for specific wet years and the lowest – for dry years, which generally reflects the increase in water runoff during high floods in the annual flow. While sediment flows are connected with hydroclimatic conditions in the catchment, the elemental composition of mass flows is mostly related to soil/petrologic conditions. With the exception of small impacted rivers where water quality effects associated with mining were observed, the formation of elemental composition and sediment-associated chemical constituents generally reflects catchment characteristics.
Rocznik
Strony
27--39
Opis fizyczny
Bibliogr. 21 poz., rys., tab.
Twórcy
  • Lomonosov Moscow State University, Moscow
Bibliografia
  • 1. Asselman N.E.M., 1999. Suspended sediments dynamics in large drainage basin: the River Rhine. Hydrological Processes 13, 1437-1450.
  • 2. Audry S., Schäfer J., Blanc G., Bossy C., Lavaux G., 2004. Anthropogenic components of 550 heavy metals (Cd, Zn, Cu, Pb) budgets in the Lot-Garonne fluvial system (France). Applied Geochemistry 19, 769-786.
  • 3. Böhm U., Kücken M., Ahrens W., Block A., Hauffe D., Keuler K., Rockel B., Will A., 2006. CLM − the climate version of LM:brief description and long-term applications. COSMO Newsletter 6, 225-235.
  • 4. Chalov S.R., Jarsjö J., Kasimov N., Romanchenko A., Pietron J., Thorslund J., Belozerova E., 2015. Spatio-temporal variation of sediment transport in the Selenga River Basin, Mongolia and Russia. Environmental Earth Sciences 73 (2), 663-680.
  • 5. Gellis A.C., 2013. Factors influencing storm-generated suspended-sediment concentrations and loads in four basins of contrasting land use, humid-tropical Puerto Rico. Catena 104, 39-57.
  • 6. Horowitz A.J., Stephens V.C., 2008. The effects of land use on fluvial sediment chemistry for the conterminous U.S. - results from the first cycle of the NAWQA Program: trace and major elements, phosphorus, carbon, and sulfur. The Science of The Total Environment 400, 290-314.
  • 7. Karthe D., Kasimov N., Chalov S., Shinkareva G., Malsy M., Menzel L., Theuring P., Hartwig M., Schweitzer C., Hofmann J., Priess J., Lychagin M., 2014. Integrating Multi-Scale Data for the Assessment of Water Availability and Quality in the Kharaa - Orkhon - Selenga River System. Geography, Environment, Sustainability 3(7), 65-86.
  • 8. Knox J.C., 1993. Large increase in flood magnitude in response tomodest changes in climate. Nature 361, 430-432.
  • 9. Kuznezov N.T., 1955. Hydrology of People Republic of Mongolia. Academy of sciences of USSR [In Russian].
  • 10. Megnounif A., Terfous A., Ouillon S., 2013. A graphical method to study suspended sediment dynamics during flood events in the Wadi Sebdou, NW Algeria (1973 – 2004). Journal of Hydrology 497, 24-36.
  • 11. McKee B.A, Aller R.C, Allison M.A, Bianchi T.S, Kineke G.C, 2004. Transport and transformation of dissolved and particulate materials on continental margins influenced by major rivers: benthic boundary layer and seabed processes. Continental Shelf Research 24 (7-8), 899-603.
  • 12. Ollivier P., Radakovitch O., Hamelin B., 2011. Major and trace element partition and fluxes in the Rhône River. Chemical Geology 285 (1-4), 15-31.
  • 13. Roussiez V., Probst A., Probst J.L., 2013. Significance of floods in metal dynamics and export in a small agricultural catchment. Journal of Hydrology 499, 71-81.
  • 14. Syvitski J., 2003. Supply and flux of sediment along hydrological pathways. Research for the 21st century. Global and Planetary Change 39, 1-11.
  • 15. Tananaev N.I., 2011. Hysteresis effect in the seasonal variations in the relationship between water discharge and suspended load in rivers of permafrost zone in Siberia and Far East. Water Resources 39(6), 648-656.
  • 16. Thorslund J., Jarsjö J., Chalov S.R., Belozerova E.V., 2012. Gold mining impact on riverine heavy metal transport in a sparsely monitored region: the upper Lake Baikal Basin case. Journal of Environmental Monitoring 14, 2780-2792.
  • 17. Törnqvist R., Jarsjö J., Pietroń J., Bring A., Rogberg P., Asokan S.M., Destouni G., 2014. Evolution of the hydro-climate system in the Lake Baikal basin. Journal of Hydrology 519, 1953-1962.
  • 18. Unger-Shayesteh K., Vorogushyn S., Farinotti D., Gafurov A., Duethmann D., Mandychev A., Merz B., 2013. What do we know about past changes in the water cycle of Central Asian headwaters? A review. Global Planet Change 110 (Part A), 4-25.
  • 19. Vanmaercke M., Zenebe A., Poesen J., Nyssen J., Verstraeten G., Deckers J., 2010. Sediment dynamics and the role of flash floods in sediment export from medium-sized catchments: a case study from the semi-arid tropical highlands in northern Ethiopia. Journal of Soils and Sediments 10, 611-627.
  • 20. Walling D.E., Fang D. 2003. Recent trends in the suspended sediment loads of the world’s rivers. Global and Planetary Change 39, 111-126.
  • 21. Zwolsman J.J.G., van Eck G.T.M., van der Weijden C.H.,1997. Geochemistry of dissolved trace metals (cadmium, copper, zinc) in the Scheldt estuary, southwestern Netherlands: impact of seasonal variability. Geochimica et Cosmochimica Acta 61, 1635-1652.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2024).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-a61d7811-2031-4696-ba2e-5bf0fc3208b3
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