Lateral hyporheic zone chemistry in an artificially constructed gravel bar and a re-meandered stream channel, Southern Ontario, Canada

Tamao Kasahara, Alan R. Hill

Research output: Contribution to journalArticle

36 Citations (Scopus)

Abstract

The effect of stream restoration on hyporheic functions has been neglected, although channel rehabilitation projects have a potential to alter stream-ground-water interactions. The present study examined the effect of an artificially constructed gravel bar and re-meandered stream channel on lateral hyporheic exchange flow and chemistry in two lowland N-rich streams in southern Ontario, Canada. Nitrate concentrations were relatively high, ranging from 0.5 to 1.3 mg N/l in both streams during spring through fall months. However, nitrate concentrations showed a steep decline as stream water entered the gravel bar and the meander bends. Differences between observed and predicted nitrate concentrations based on conservative ion concentration patterns indicated that 40-100 and 68-98% of the nitrate entering the hyporheic zone was removed in the gravel bar and meanders, respectively. Rapid depletion of dissolved oxygen concentrations along lateral hyporheic flow paths and denitrifying potentials assayed by the acetylene block technique in hyporheic sediments suggests that denitrification was an important mechanism of nitrate depletion. Despite the high rate of nitrate removal, the flux of stream water laterally entering the constructed gravel bar and meander bends was very small, and hyporheic nitrate removal was <0.015% of the daily stream load during base-flow periods in summer and fall. The effects of restoration projects on hyporheic zone dynamics are often limited in lowland streams by low channel gradients and fine floodplain sediments with low interstitial flows that restrict the magnitude of the stream-hyporheic connection.

Original languageEnglish
Pages (from-to)1257-1269
Number of pages13
JournalJournal of the American Water Resources Association
Volume43
Issue number5
DOIs
Publication statusPublished - Oct 1 2007
Externally publishedYes

Fingerprint

hyporheic zone
stream channel
Gravel
Nitrates
gravel
nitrate
meander
Restoration
Sediments
Denitrification
Acetylene
Dissolved oxygen
Patient rehabilitation
Water
Groundwater
acetylene
baseflow
sediment
Fluxes
denitrification

All Science Journal Classification (ASJC) codes

  • Ecology
  • Water Science and Technology
  • Earth-Surface Processes

Cite this

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abstract = "The effect of stream restoration on hyporheic functions has been neglected, although channel rehabilitation projects have a potential to alter stream-ground-water interactions. The present study examined the effect of an artificially constructed gravel bar and re-meandered stream channel on lateral hyporheic exchange flow and chemistry in two lowland N-rich streams in southern Ontario, Canada. Nitrate concentrations were relatively high, ranging from 0.5 to 1.3 mg N/l in both streams during spring through fall months. However, nitrate concentrations showed a steep decline as stream water entered the gravel bar and the meander bends. Differences between observed and predicted nitrate concentrations based on conservative ion concentration patterns indicated that 40-100 and 68-98{\%} of the nitrate entering the hyporheic zone was removed in the gravel bar and meanders, respectively. Rapid depletion of dissolved oxygen concentrations along lateral hyporheic flow paths and denitrifying potentials assayed by the acetylene block technique in hyporheic sediments suggests that denitrification was an important mechanism of nitrate depletion. Despite the high rate of nitrate removal, the flux of stream water laterally entering the constructed gravel bar and meander bends was very small, and hyporheic nitrate removal was <0.015{\%} of the daily stream load during base-flow periods in summer and fall. The effects of restoration projects on hyporheic zone dynamics are often limited in lowland streams by low channel gradients and fine floodplain sediments with low interstitial flows that restrict the magnitude of the stream-hyporheic connection.",
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