Progress in isotope tracer hydrology in Canada

被引:252
作者
Gibson, JJ [1 ]
Edwards, TWD
Birks, SJ
St Amour, NA
Buhay, WM
McEachern, P
Wolfe, BB
Peters, DL
机构
[1] Univ Victoria, Natl Water Res Inst, Water & Climate Impacts Res Ctr, Victoria, BC, Canada
[2] Univ Waterloo, Dept Earth Sci, Waterloo, ON N2L 3G1, Canada
[3] Univ Winnipeg, Dept Geog, Winnipeg, MB R3B 2E9, Canada
[4] Alberta Environm, Air & Water Branch, Sci & Stand Div, Edmonton, AB, Canada
[5] Wilfrid Laurier Univ, Dept Geog & Environm Studies, Waterloo, ON N2L 3C5, Canada
关键词
isotope hydrology; isotope mass balance; oxygen-18; deuterium; deuterium excess; surface water; groundwater; river basin hydrology;
D O I
10.1002/hyp.5766
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
An overview of current research in isotope hydrology, focusing on recent Canadian contributions, is discussed under the headings: precipitation networks, hydrograph separation and groundwater studies, river basin hydrology, lake and catchment water balance, and isotope palaeohydrology from lake sediment records. Tracer-based techniques, relying primarily on the naturally occurring environmental isotopes, have been integrated into a range of hydrological and biogeochemical research programmes, as they effectively complement physical and chemical techniques. A significant geographic focus of Canadian isotope hydrology research has been on the Mackenzie River basin, forming contributions to programmes such as the Global Energy and Water Cycle Experiment. Canadian research has also directly supported international efforts such as the International Atomic Energy Agency's (IAEA) Global Network for Isotopes in Precipitation and IAEAs Coordinated Research Project on Large River Basins. One significant trend in Canadian research is toward sustained long-term monitoring of precipitation and river discharge to enable better characterization of spatial and temporal variability in isotope signatures and their underlying causes. One fundamental conclusion drawn from previous studies in Canada is that combined use of delta(18)O and delta(2)H enables the distinction of precipitation variability from evaporation effects, which offers significant advantages over use of the individual tracers alone. The study of hydrological controls on water chemistry is one emerging research trend that stems from the unique ability to integrate isotope sampling within both water quality and water quantity surveys. Copyright (C) 2005 John Wiley Sons, Ltd.
引用
收藏
页码:303 / 327
页数:25
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