Stable water isotopes and the physical environment

This paper presents the characteristics of the fractionation of water isotopes which occurs during evaporation and freezing of water. It shows how these characteristics can be used for studying some aspects of the physical environment, namely hydrological and glaciological issues. On the one hand, c...

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Published in:Belgeo
Main Authors: Roland Souchez, Réginald Lorrain, Jean-Louis Tison
Format: Article in Journal/Newspaper
Language:English
French
Published: Société Royale Belge de Géographie and the Belgian National Committee of Geography 2002
Subjects:
geo
Online Access:https://doi.org/10.4000/belgeo.16199
https://doaj.org/article/2014b4923fbf4ce8b764b7a78219f043
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:2014b4923fbf4ce8b764b7a78219f043 2023-05-15T13:47:19+02:00 Stable water isotopes and the physical environment Roland Souchez Réginald Lorrain Jean-Louis Tison 2002-06-01 https://doi.org/10.4000/belgeo.16199 https://doaj.org/article/2014b4923fbf4ce8b764b7a78219f043 en fr eng fre Société Royale Belge de Géographie and the Belgian National Committee of Geography 1377-2368 2294-9135 doi:10.4000/belgeo.16199 https://doaj.org/article/2014b4923fbf4ce8b764b7a78219f043 undefined Belgeo, Vol 2, Pp 133-144 (2002) stable isotopes hydrology glaciology climatic archives Antarctica arid environment geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2002 fttriple https://doi.org/10.4000/belgeo.16199 2023-01-22T19:27:41Z This paper presents the characteristics of the fractionation of water isotopes which occurs during evaporation and freezing of water. It shows how these characteristics can be used for studying some aspects of the physical environment, namely hydrological and glaciological issues. On the one hand, case studies regarding the hydrological cycle are considered. They deal with the relative contributions of runoff and groundwater to the discharge of rivers, of plant transpiration and direct evaporation in the arid regions atmosphere and of different water sources in aquifer recharge. On the other hand, the paper explains how the water isotopes are used in the study of the Antarctic Ice Sheet as climatic archives as well as how they allow to understand the formation of more than 200 m of lake ice present above the liquid water of subglacial Lake Vostok in East Antarctica. This case study approach demonstrates that stable water isotopes can be an ideal tool to account for many processes active in the physical environment. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Unknown Antarctic East Antarctica Lake Vostok ENVELOPE(106.000,106.000,-77.500,-77.500) The Antarctic Belgeo 2 133 144
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
French
topic stable isotopes
hydrology
glaciology
climatic archives
Antarctica
arid environment
geo
envir
spellingShingle stable isotopes
hydrology
glaciology
climatic archives
Antarctica
arid environment
geo
envir
Roland Souchez
Réginald Lorrain
Jean-Louis Tison
Stable water isotopes and the physical environment
topic_facet stable isotopes
hydrology
glaciology
climatic archives
Antarctica
arid environment
geo
envir
description This paper presents the characteristics of the fractionation of water isotopes which occurs during evaporation and freezing of water. It shows how these characteristics can be used for studying some aspects of the physical environment, namely hydrological and glaciological issues. On the one hand, case studies regarding the hydrological cycle are considered. They deal with the relative contributions of runoff and groundwater to the discharge of rivers, of plant transpiration and direct evaporation in the arid regions atmosphere and of different water sources in aquifer recharge. On the other hand, the paper explains how the water isotopes are used in the study of the Antarctic Ice Sheet as climatic archives as well as how they allow to understand the formation of more than 200 m of lake ice present above the liquid water of subglacial Lake Vostok in East Antarctica. This case study approach demonstrates that stable water isotopes can be an ideal tool to account for many processes active in the physical environment.
format Article in Journal/Newspaper
author Roland Souchez
Réginald Lorrain
Jean-Louis Tison
author_facet Roland Souchez
Réginald Lorrain
Jean-Louis Tison
author_sort Roland Souchez
title Stable water isotopes and the physical environment
title_short Stable water isotopes and the physical environment
title_full Stable water isotopes and the physical environment
title_fullStr Stable water isotopes and the physical environment
title_full_unstemmed Stable water isotopes and the physical environment
title_sort stable water isotopes and the physical environment
publisher Société Royale Belge de Géographie and the Belgian National Committee of Geography
publishDate 2002
url https://doi.org/10.4000/belgeo.16199
https://doaj.org/article/2014b4923fbf4ce8b764b7a78219f043
long_lat ENVELOPE(106.000,106.000,-77.500,-77.500)
geographic Antarctic
East Antarctica
Lake Vostok
The Antarctic
geographic_facet Antarctic
East Antarctica
Lake Vostok
The Antarctic
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
op_source Belgeo, Vol 2, Pp 133-144 (2002)
op_relation 1377-2368
2294-9135
doi:10.4000/belgeo.16199
https://doaj.org/article/2014b4923fbf4ce8b764b7a78219f043
op_rights undefined
op_doi https://doi.org/10.4000/belgeo.16199
container_title Belgeo
container_issue 2
container_start_page 133
op_container_end_page 144
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