Two decades of trends in ground water chemical composition in The Great Vasyugan Mire, Western Siberia, Russia

Λεπτομέρειες βιβλιογραφικής εγγραφής
Parent link:Environmental Earth Sciences: Scientific Journal.— , 2011
Vol. 73, Iss. 11.— 2015.— [Р. 7329-7341]
Κύριος συγγραφέας: Eckstein Y. Y.
Συγγραφή απο Οργανισμό/Αρχή: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Άλλοι συγγραφείς: Savichev O. G. Oleg Gennadievich, Pasechnik E. Yu. Elena Yurievna
Περίληψη:Title screen
Boreal wetlands cover approximately 30 % of the West Siberian Plain (WSP). The Great Vasyugan Mire, Northern Hemisphere's largest contiguous wetlands, occupies low-lying plains in the Ob and Irtysh's interfluve. Most research has investigated the peat generating processes and reserves in the WSP wetlands. Little information exists about temporal changes in the chemical composition of the wetland waters within the Ob-Irtysh interfluve. Although the region's climate is continental with extended cold winters and short hot summers, Western Siberia is experiencing rapid climatic changes. The consequences of these changes include permafrost loss, snow cover reduction, and river flow changes. In this study whether and how increasing surface air temperatures contributed to changes in the chemical composition of the atmospheric precipitation and water in the mire were investigated.
Режим доступа: по договору с организацией-держателем ресурса
Γλώσσα:Αγγλικά
Έκδοση: 2015
Θέματα:
Διαθέσιμο Online:<http://dx.doi.org/10.1007/s12665-014-3908-z>
Μορφή: Ηλεκτρονική πηγή Κεφάλαιο βιβλίου
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=644305

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200 1 |a Two decades of trends in ground water chemical composition in The Great Vasyugan Mire, Western Siberia, Russia  |f Y. Y. Eckstein, O. G. Savichev, E. Yu. Pasechnik 
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330 |a Boreal wetlands cover approximately 30 % of the West Siberian Plain (WSP). The Great Vasyugan Mire, Northern Hemisphere's largest contiguous wetlands, occupies low-lying plains in the Ob and Irtysh's interfluve. Most research has investigated the peat generating processes and reserves in the WSP wetlands. Little information exists about temporal changes in the chemical composition of the wetland waters within the Ob-Irtysh interfluve. Although the region's climate is continental with extended cold winters and short hot summers, Western Siberia is experiencing rapid climatic changes. The consequences of these changes include permafrost loss, snow cover reduction, and river flow changes. In this study whether and how increasing surface air temperatures contributed to changes in the chemical composition of the atmospheric precipitation and water in the mire were investigated. 
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