Groundwater-surface water interaction between an esker aquifer and a drained fen

Pekka M. Rossi*, Pertti Ala-aho, Anna Kaisa Ronkanen, Bjørn Kløve, Pertti Otto Antero Ala-Aho

*Corresponding author for this work

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

Groundwater discharge from an esker aquifer to a fen was studied to understand relevant hydrological processes for groundwater-surface water interaction in an esker-peatland hillslope. Piezometric levels of the peat layer and esker sand layer were continuously monitored and compared to climate data. Groundwater exfiltration points were spatially mapped and related to peat depth. The study showed a clear interaction between fen surface water and sand esker groundwater although the hydraulic conductivity of peat was low and the peat depth thick. In the artesian aquifer beneath the fen, the piezometric head showed a clear response to precipitation and evapotranspiration. Wetting of the peat is rapidly seen as pressure increase in the confined aquifer. This provides new information on hydraulics of wetlands found in aquifer discharge areas. Groundwater exfiltrated through thick peat layers in vertical preferential point discharges demonstrating how double porosity provides flow through the peat layer with low hydraulic conductivity in the peat matrix. The " pipe flow" channels were found in the deep peat area in the transition zones from deep peat to shallow peat. Diffuse seepage through the ditch bottom was found where ditches cut into the sand layer. Increased discharge through the ditch bed reduced the flow resistance at the aquifer boundary which can lower the groundwater level in the esker. The results show new processes in the groundwater discharge zone that are useful for groundwater modelling and policy development for future groundwater protection.

Original languageEnglish
Pages (from-to)52-60
Number of pages9
JournalJournal of Hydrology
Volume432-433
DOIs
Publication statusPublished - 11 Apr 2012

Fingerprint

esker
groundwater-surface water interaction
fen
peat
aquifer
groundwater
sand
hydraulic conductivity
pipe flow
confined aquifer
policy development
hillslope
peatland
wetting
transition zone
seepage
evapotranspiration

Keywords

  • Esker
  • hillslope
  • land-use
  • peatland
  • preferential flow
  • spring

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

Rossi, P. M., Ala-aho, P., Ronkanen, A. K., Kløve, B., & Ala-Aho, P. O. A. (2012). Groundwater-surface water interaction between an esker aquifer and a drained fen. Journal of Hydrology, 432-433, 52-60. https://doi.org/10.1016/j.jhydrol.2012.02.026

Groundwater-surface water interaction between an esker aquifer and a drained fen. / Rossi, Pekka M.; Ala-aho, Pertti; Ronkanen, Anna Kaisa; Kløve, Bjørn; Ala-Aho, Pertti Otto Antero.

In: Journal of Hydrology, Vol. 432-433, 11.04.2012, p. 52-60.

Research output: Contribution to journalArticle

Rossi, PM, Ala-aho, P, Ronkanen, AK, Kløve, B & Ala-Aho, POA 2012, 'Groundwater-surface water interaction between an esker aquifer and a drained fen', Journal of Hydrology, vol. 432-433, pp. 52-60. https://doi.org/10.1016/j.jhydrol.2012.02.026
Rossi, Pekka M. ; Ala-aho, Pertti ; Ronkanen, Anna Kaisa ; Kløve, Bjørn ; Ala-Aho, Pertti Otto Antero. / Groundwater-surface water interaction between an esker aquifer and a drained fen. In: Journal of Hydrology. 2012 ; Vol. 432-433. pp. 52-60.
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