The present paper studies long-term (1923–2005) changes in the hydrological regime of the medium (100–1,000 km2) river of the Ordovician oil shale field of north-east Estonia. The changing regime in the heavily mined catchments is contrasted with a morphologically similar reference catchment (River Keila) where there has been no mining activity. The Gumbel Method and Rodionov Regime Shifts Algorithm (STARS) were used to study high- and low-water changes of the mining area. The study shows that mine water has no significant impact on the River Purtse annual run-off; however, it has influence on the low water period and minimum flow values, increasing the amount of run-off. Mine water discharge can affect the course of the run-off during the high water period and high water season peaks. Therefore, in terms of the river maximum flows return period, there are no major differences between the mining and natural catchments.
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Research Article|
January 27 2012
Impact of the shale mine on the River Purtse hydrological regime in north-east Estonia
Riina Vaht;
1University of Tartu, Department of Geography, Vanemuise 46, Tartu 51014, Estonia
E-mail: [email protected]
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Mait Sepp;
Mait Sepp
1University of Tartu, Department of Geography, Vanemuise 46, Tartu 51014, Estonia
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Aarne Luud
Aarne Luud
2Estonian University of Life Sciences, Kreutzwaldi 1, Tartu 51014, Estonia
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Hydrology Research (2012) 43 (4): 422–429.
Article history
Received:
December 22 2010
Accepted:
April 11 2011
Citation
Riina Vaht, Mait Sepp, Aarne Luud; Impact of the shale mine on the River Purtse hydrological regime in north-east Estonia. Hydrology Research 1 August 2012; 43 (4): 422–429. doi: https://doi.org/10.2166/nh.2012.143
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