Wpływ zbiornika retencyjnego na fizykochemiczne właściwości rzeki himalajskiej (Tista, Indie) = Impact of a dam reservoir on the chemistry of a Himalayan river (the Teesta, India)

Prokop, Paweł; Wiejaczka, Łukasz; Kozłowski, Rafał; Sarkar, Subir

doi:0033-2143 (print)

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Wpływ zbiornika retencyjnego na fizykochemiczne właściwości rzeki himalajskiej (Tista, Indie) = Impact of a dam reservoir on the chemistry of a Himalayan river (the Teesta, India) Prokop, PawełWiejaczka, ŁukaszKozłowski, RafałSarkar, Subir

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Wpływ zbiornika retencyjnego na fizykochemiczne właściwości rzeki himalajskiej (Tista, Indie) = Impact of a dam reservoir on the chemistry of a Himalayan river (the Teesta, India)

Przegląd Geograficzny T. 89 z. 1 (2017)

Prokop, Paweł ; Wiejaczka, Łukasz ; Kozłowski, Rafał ; Sarkar, Subir

chemizm wód ; jakość wody ; zbiornik zaporowy ; rzeka Tista ; Himalaje

W artykule przedstawiono rolę nowo wybudowanego zbiornika retencyjnego w kształtowaniu właściwości fizykochemicznych i składu chemicznego rzeki Tisty (dopływ Brahmaputry) w Himalajach. Badania terenowe przeprowadzono w okresie pomonsunowym w latach 2013-2015. Analiza składu chemicznego wody w profilu podłużnym rzeki powyżej i poniżej zbiornika wykazała, że w zbiorniku następuje obniżenie stężenia większości podstawowych jonów (Cl– , K+, Na+, Mg2, NO3 i PO4 3–), odwrotny trend zaobserwowano tylko w przypadku jonów Ca2+, SO4 2– i NH4+. Istnienie zapory nie wpływa na stężenie jonów F– . Poniżej zbiornika odnotowano nieznaczne wzbogacenie wód w jony metali: Cu, Ni, Zn, Cr, C i Sr. Mniejsze stężenie jonów w rzece poniżej zapory wskazuje na procesy samooczyszczania wody retencjonowanej w zbiorniku. Zmiany właściwości fizykochemicznych oraz stężeń jonów następujące w zbiorniku są niwelowane przez czynniki środowiskowe jeszcze na obszarze Himalajów na odcinku do 15 km poniżej zapory.

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