THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN)
Abstract. The article presents investigation of groundwater occurrence in the Ebba River catchment totaled in central Spitsbergen (Petuniabukta region). It was recognized that groundwater occurs there seasonally in the summer melting season when the melting of active layer take place and enable flow...
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Polish Geological Institute - NRI
2010
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Online Access: | https://gq.pgi.gov.pl/bp/article/view/28878 |
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ftjgq:oai:geojournals.pgi.gov.pl:article/28878 2024-09-09T19:22:05+00:00 THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) Marciniak, Marek Dragon, Krzysztof 2010-10-31 application/pdf https://gq.pgi.gov.pl/bp/article/view/28878 eng eng Polish Geological Institute - NRI https://gq.pgi.gov.pl/bp/article/view/28878/20550 https://gq.pgi.gov.pl/bp/article/view/28878 Copyright (c) 2020 Biuletyn Państwowego Instytutu Geologicznego Biuletyn Państwowego Instytutu Geologicznego; Vol. 441 No. 441 (2010): Hydrogeologia z.X; 93 - 100 Biuletyn Państwowego Instytutu Geologicznego; Tom 441 Nr 441 (2010): Tom 441; 93 - 100 0867-6143 active layer groundwater flow Svaibard Arctic regions info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 2010 ftjgq 2024-07-30T03:29:10Z Abstract. The article presents investigation of groundwater occurrence in the Ebba River catchment totaled in central Spitsbergen (Petuniabukta region). It was recognized that groundwater occurs there seasonally in the summer melting season when the melting of active layer take place and enable flow of groundwater. Using data from four groups of piezometers located in different parts of the valley the hydrogeological parameters that characterize this shallow aquifer (thickness of the active layer, hydraulic conductivity, groundwater level fluctuations) were recognized. Using Dairy's low the amount of water that recharge Ebba River was calculated using field data. This calculation enabled more precise estimation of other component of Ebba River recharge (surface and overland water inflow, recharge from glaciers). These calculations were confirmed by interpretation of groundwater and surface water chemistry differentiation. Article in Journal/Newspaper Arctic Spitsbergen Geological Quarterly Arctic Petuniabukta ENVELOPE(16.532,16.532,78.687,78.687) Ebba ENVELOPE(139.583,139.583,-66.575,-66.575) |
institution |
Open Polar |
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Geological Quarterly |
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ftjgq |
language |
English |
topic |
active layer groundwater flow Svaibard Arctic regions |
spellingShingle |
active layer groundwater flow Svaibard Arctic regions Marciniak, Marek Dragon, Krzysztof THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) |
topic_facet |
active layer groundwater flow Svaibard Arctic regions |
description |
Abstract. The article presents investigation of groundwater occurrence in the Ebba River catchment totaled in central Spitsbergen (Petuniabukta region). It was recognized that groundwater occurs there seasonally in the summer melting season when the melting of active layer take place and enable flow of groundwater. Using data from four groups of piezometers located in different parts of the valley the hydrogeological parameters that characterize this shallow aquifer (thickness of the active layer, hydraulic conductivity, groundwater level fluctuations) were recognized. Using Dairy's low the amount of water that recharge Ebba River was calculated using field data. This calculation enabled more precise estimation of other component of Ebba River recharge (surface and overland water inflow, recharge from glaciers). These calculations were confirmed by interpretation of groundwater and surface water chemistry differentiation. |
format |
Article in Journal/Newspaper |
author |
Marciniak, Marek Dragon, Krzysztof |
author_facet |
Marciniak, Marek Dragon, Krzysztof |
author_sort |
Marciniak, Marek |
title |
THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) |
title_short |
THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) |
title_full |
THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) |
title_fullStr |
THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) |
title_full_unstemmed |
THE INFLUENCE OF GROUNDWATER DISCHARGE ON THE RUNOFF OF AN ARCTIC STREAM (EBBA RIVER, CENTRAL SPITSBERGEN) |
title_sort |
influence of groundwater discharge on the runoff of an arctic stream (ebba river, central spitsbergen) |
publisher |
Polish Geological Institute - NRI |
publishDate |
2010 |
url |
https://gq.pgi.gov.pl/bp/article/view/28878 |
long_lat |
ENVELOPE(16.532,16.532,78.687,78.687) ENVELOPE(139.583,139.583,-66.575,-66.575) |
geographic |
Arctic Petuniabukta Ebba |
geographic_facet |
Arctic Petuniabukta Ebba |
genre |
Arctic Spitsbergen |
genre_facet |
Arctic Spitsbergen |
op_source |
Biuletyn Państwowego Instytutu Geologicznego; Vol. 441 No. 441 (2010): Hydrogeologia z.X; 93 - 100 Biuletyn Państwowego Instytutu Geologicznego; Tom 441 Nr 441 (2010): Tom 441; 93 - 100 0867-6143 |
op_relation |
https://gq.pgi.gov.pl/bp/article/view/28878/20550 https://gq.pgi.gov.pl/bp/article/view/28878 |
op_rights |
Copyright (c) 2020 Biuletyn Państwowego Instytutu Geologicznego |
_version_ |
1809762357451161600 |