Heat-based hyporheic flux calculations in heterogeneous salmon spawning gravels

Christian Birkel, Chris Soulsby, Dylan J. Irvine, Iain Malcolm, Laura K Lautz, Doerthe Tetzlaff

Research output: Contribution to journalArticle

13 Scopus citations

Abstract

Groundwater-surface water interactions in rivers are a critically important factor for fish spawning, as streamwater downwelling or upwelling of low-oxygen groundwater can affect egg survival. Assessing such dynamics at the reach scale using distributed temperature measurements as a tracer proved reliable in determining flux rates and directions in the hyporheic zone in a number of studies. Here, we report heat-based vertical flux rates from a heterogeneous gravel-bed stream reach used by spawning Atlantic salmon in the Scottish Highlands. Results showed mostly small downwelling fluxes (~0.3 m d−1), which were largely independent of discharge. Contrasting, and at times unusual flux-depth profiles (e.g., increasing flux with depth) were detected, consistent with the heterogeneous streambed material causing diverse hyporheic flow paths. This was tested in a numerical 2-D model setup attempting to reproduce such behavior with variable random hydraulic conductivity (K) fields. The 2-D model clearly demonstrated that strong deviations from the expected decrease of fluxes with depth can be explained by high heterogeneity coupled with relatively low K fields. This showed that using simple 1-D heat-based flux estimates in combination with 2-D models is a useful approach to testing hypotheses about the influence of variable streambed materials on groundwater–surface water exchange in an ecological context.

Original languageEnglish (US)
JournalAquatic Sciences
DOIs
StateAccepted/In press - Aug 19 2015

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Keywords

  • Ground water-surface water interaction
  • Heat tracer
  • Hyporheic zone
  • Numerical 2-D model
  • VFLUX

ASJC Scopus subject areas

  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Ecology, Evolution, Behavior and Systematics

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