Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula
The rapid changes that are taking place in the climate of the Antarctic Peninsula are triggering hydrological processes which had been limited or inactive for relatively long periods of time. These processes are evident in ice-free areas on the northern edge of the Antarctic Peninsula, such as Cape...
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ftunibueairesbd:paper:paper_00044822_v70_n2_p249_SilvaBusso 2023-05-15T13:42:26+02:00 Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula 2013 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v70_n2_p249_SilvaBusso https://hdl.handle.net/20.500.12110/paper_00044822_v70_n2_p249_SilvaBusso unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v70_n2_p249_SilvaBusso http://hdl.handle.net/20.500.12110/paper_00044822_v70_n2_p249_SilvaBusso Groundwater Hydrology Permafrost Ross Archipelago chemical analysis climate change hydrochemistry hydrogeology hydrological modeling isotopic ratio surface water Antarctica Vega Island West Antarctica 2013 ftunibueairesbd https://doi.org/20.500.12110/paper_00044822_v70_n2_p249_SilvaBusso 2023-02-16T02:04:18Z The rapid changes that are taking place in the climate of the Antarctic Peninsula are triggering hydrological processes which had been limited or inactive for relatively long periods of time. These processes are evident in ice-free areas on the northern edge of the Antarctic Peninsula, such as Cape Lamb, and lead to intense draining of the surface and groundwater system throughout the brief Antarctic summer. The result is a movement of large amounts of water, sediments and nutrients that would be immobilized in other scenarios. This study proposes a model of the operation of the surface and groundwater system that could be valid for several ice-free areas in the region, based on the interpretation of field observations in Cape Lamb, the most extensive ice-free area on Vega Island. The model proposed is further supported by the interpretation of 56 chemical analyses of samples representing groundwater, active layer water, glacier ice and snowfall. The hydrochemical interpretation is supported primarily by four indicators (pH, electrical conductivity, D/18O ratio and SO4/Cl ratio) which have proven to be the most appropriate hydrochemical variables to differentiate the origin and interaction of the waters in the various sections of the system. Other/Unknown Material Antarc* Antarctic Antarctic Peninsula Antarctica Ice permafrost Ross Archipelago Vega Island West Antarctica Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Antarctic The Antarctic Antarctic Peninsula West Antarctica Vega Island ENVELOPE(-57.500,-57.500,-63.833,-63.833) Cape Lamb ENVELOPE(-57.621,-57.621,-63.909,-63.909) Ross Archipelago ENVELOPE(167.000,167.000,-77.500,-77.500) |
institution |
Open Polar |
collection |
Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) |
op_collection_id |
ftunibueairesbd |
language |
unknown |
topic |
Groundwater Hydrology Permafrost Ross Archipelago chemical analysis climate change hydrochemistry hydrogeology hydrological modeling isotopic ratio surface water Antarctica Vega Island West Antarctica |
spellingShingle |
Groundwater Hydrology Permafrost Ross Archipelago chemical analysis climate change hydrochemistry hydrogeology hydrological modeling isotopic ratio surface water Antarctica Vega Island West Antarctica Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula |
topic_facet |
Groundwater Hydrology Permafrost Ross Archipelago chemical analysis climate change hydrochemistry hydrogeology hydrological modeling isotopic ratio surface water Antarctica Vega Island West Antarctica |
description |
The rapid changes that are taking place in the climate of the Antarctic Peninsula are triggering hydrological processes which had been limited or inactive for relatively long periods of time. These processes are evident in ice-free areas on the northern edge of the Antarctic Peninsula, such as Cape Lamb, and lead to intense draining of the surface and groundwater system throughout the brief Antarctic summer. The result is a movement of large amounts of water, sediments and nutrients that would be immobilized in other scenarios. This study proposes a model of the operation of the surface and groundwater system that could be valid for several ice-free areas in the region, based on the interpretation of field observations in Cape Lamb, the most extensive ice-free area on Vega Island. The model proposed is further supported by the interpretation of 56 chemical analyses of samples representing groundwater, active layer water, glacier ice and snowfall. The hydrochemical interpretation is supported primarily by four indicators (pH, electrical conductivity, D/18O ratio and SO4/Cl ratio) which have proven to be the most appropriate hydrochemical variables to differentiate the origin and interaction of the waters in the various sections of the system. |
title |
Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula |
title_short |
Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula |
title_full |
Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula |
title_fullStr |
Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula |
title_full_unstemmed |
Hydrogeological model from hydrochemical and geocryologic records on the Cape Lamb of Vega Island, northern Antarctic Peninsula |
title_sort |
hydrogeological model from hydrochemical and geocryologic records on the cape lamb of vega island, northern antarctic peninsula |
publishDate |
2013 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v70_n2_p249_SilvaBusso https://hdl.handle.net/20.500.12110/paper_00044822_v70_n2_p249_SilvaBusso |
long_lat |
ENVELOPE(-57.500,-57.500,-63.833,-63.833) ENVELOPE(-57.621,-57.621,-63.909,-63.909) ENVELOPE(167.000,167.000,-77.500,-77.500) |
geographic |
Antarctic The Antarctic Antarctic Peninsula West Antarctica Vega Island Cape Lamb Ross Archipelago |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula West Antarctica Vega Island Cape Lamb Ross Archipelago |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Ice permafrost Ross Archipelago Vega Island West Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Ice permafrost Ross Archipelago Vega Island West Antarctica |
op_relation |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v70_n2_p249_SilvaBusso http://hdl.handle.net/20.500.12110/paper_00044822_v70_n2_p249_SilvaBusso |
op_doi |
https://doi.org/20.500.12110/paper_00044822_v70_n2_p249_SilvaBusso |
_version_ |
1766167866818691072 |