Stable isotope tracers as diagnostic tools in upscaling flow path understanding and residence time estimates in a mountainous mesoscale catchment

P. J. Rodgers, Christopher Soulsby, S Waldron

Research output: Contribution to journalArticle

65 Citations (Scopus)

Abstract

delta(18)O measurements of precipitation and stream waters were used as a natural tracer to investigate hydrological pathways and residence times in the River Feshie, a complex mesoscale (231 km(2)) catchment in the Cairngorm Mountains of Scotland. Precipitation delta(18)O exhibited strong seasonal variation over the 2001-02 hydrological year, ranging from -6.9 parts per thousand in the summer, to -12.0 parts per thousand during winter snowfalls (mean delta(18)O -9-59 parts per thousand). Although damped, this seasonality was reflected in stream water outputs at seven sampling sites in the catchment, allowing delta(18)O variations to be used to infer hydrological source areas. Thus, stream water delta(18)O was generally controlled by a seasonally variable storm flow end member, mixing with groundwater of more constant isotopic composition. Periodic regression analysis allowed the differences in this mixing process between monitoring subcatchments to be assessed more quantitatively to provide a preliminary estimate of mean stream water residence time. This demonstrated the importance of responsive hydrological pathways associated with peat and shallow alpine soils in the headwater subcatchments in producing seasonally variable runoff with short mean residence times (33-113 days). In contrast, other tributaries with more freely draining soils and larger groundwater storage in shallow aquifers provided more effective mixing of variable precipitation inputs, resulting in longer residence time estimates (178-445 days). The mean residence time of runoff leaving the Feshie catchment reflected an integration of these contrasting influences (110-200 days). These insights from delta(18)O measurements extend the hydrological understanding of the Feshie catchment gained from other hydrochemical tracers, and demonstrate the utility of isotope tracers in investigating hydrological processes at the mesoscale. Copyright (c) 2005 John Wiley & Sons, Ltd.

Original languageEnglish
Pages (from-to)2291-2307
Number of pages17
JournalHydrological Processes
Volume19
Issue number11
Early online date14 Mar 2005
DOIs
Publication statusPublished - Jul 2005

Keywords

  • delta O-18
  • isotope
  • tracers
  • hydrology
  • mesoscale
  • residence times
  • runoff processes
  • models
  • Scotland
  • different spatial scales
  • Sub-Arctic catchment
  • Cairngorm mountains
  • hydrograph separations
  • hydrological pathways
  • Scottish catchment
  • event water
  • rainfall

Cite this

Stable isotope tracers as diagnostic tools in upscaling flow path understanding and residence time estimates in a mountainous mesoscale catchment. / Rodgers, P. J.; Soulsby, Christopher; Waldron, S .

In: Hydrological Processes, Vol. 19, No. 11, 07.2005, p. 2291-2307.

Research output: Contribution to journalArticle

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AB - delta(18)O measurements of precipitation and stream waters were used as a natural tracer to investigate hydrological pathways and residence times in the River Feshie, a complex mesoscale (231 km(2)) catchment in the Cairngorm Mountains of Scotland. Precipitation delta(18)O exhibited strong seasonal variation over the 2001-02 hydrological year, ranging from -6.9 parts per thousand in the summer, to -12.0 parts per thousand during winter snowfalls (mean delta(18)O -9-59 parts per thousand). Although damped, this seasonality was reflected in stream water outputs at seven sampling sites in the catchment, allowing delta(18)O variations to be used to infer hydrological source areas. Thus, stream water delta(18)O was generally controlled by a seasonally variable storm flow end member, mixing with groundwater of more constant isotopic composition. Periodic regression analysis allowed the differences in this mixing process between monitoring subcatchments to be assessed more quantitatively to provide a preliminary estimate of mean stream water residence time. This demonstrated the importance of responsive hydrological pathways associated with peat and shallow alpine soils in the headwater subcatchments in producing seasonally variable runoff with short mean residence times (33-113 days). In contrast, other tributaries with more freely draining soils and larger groundwater storage in shallow aquifers provided more effective mixing of variable precipitation inputs, resulting in longer residence time estimates (178-445 days). The mean residence time of runoff leaving the Feshie catchment reflected an integration of these contrasting influences (110-200 days). These insights from delta(18)O measurements extend the hydrological understanding of the Feshie catchment gained from other hydrochemical tracers, and demonstrate the utility of isotope tracers in investigating hydrological processes at the mesoscale. Copyright (c) 2005 John Wiley & Sons, Ltd.

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KW - hydrological pathways

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