Please use this identifier to cite or link to this item: https://hdl.handle.net/10593/15569
Title: The relationship between dissolved solids yield and the presence of snow cover in the periglacial basin of the Obruchev Glacier (Polar Urals) during the ablation season
Authors: Stachnik, Łukasz
Uzarowicz, Łukasz
Keywords: Polar Urals
Obruchev Glacier
solute yield
periglacial basin
ablation season
Issue Date: 2011
Publisher: Wydział Nauk Geograficznych i Geologicznych Uniwersytetu im. Adama Mickiewicza
Citation: Quaestiones Geographicae vol. 30 (1), 2011. pp. 95-103
Abstract: Hydrochemical investigations were carried out in the periglacial basin of Obruchev Glacier (Polar Urals, Russia) in order to provide a quantitative and qualitative comparison of dissolved solids yields during the ablation season with and without snow cover taking into account the mineral composition of rocks and deposits occurring in the studied area. The concentration of dissolved solids in the waters of the investigated basin is very low (about 7.0–8.9 μS cm–1). It is most of all due to harsh local climate conditions as well as the presence of minerals resistant to weathering in the parent material. Both factors contribute to the low rate of chemical weathering in the area. Results obtained indicate that a larger dissolved solids yield was transported during the period with snow cover (106 kg km–2 day–1, on average), than at the same time of the year but without snow cover (13 kg km–2 day–1, on average) indicating that melting snow is an important factor influencing the yield of dissolved solids in surface waters.
URI: http://hdl.handle.net/10593/15569
ISBN: 978-83-62662-62-3
ISSN: 0137- 477X
Appears in Collections:Quaestiones Geographicae vol. 30 (1), 2011

Files in This Item:
File Description SizeFormat 
QG30(1)j95-103.pdf1.67 MBAdobe PDFView/Open
Show full item record



This item is licensed under a Creative Commons License Creative Commons