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FLOW REVERSALS IN PEATLANDS INFLUENCED BY LOCAL GROUNDWATER SYSTEMS
Author(s) -
DEVITO K. J.,
WADDINGTON J. M.,
BRANFIREUN B. A.
Publication year - 1997
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/(sici)1099-1085(199701)11:1<103::aid-hyp417>3.0.co;2-e
Subject(s) - peat , water table , groundwater , groundwater flow , hydrology (agriculture) , hydrogeology , drawdown (hydrology) , groundwater recharge , groundwater discharge , geology , environmental science , subsurface flow , aquifer , geography , geotechnical engineering , archaeology
Piezometric head data from various depths were examined at two peatlands in Ontario, Canada and one peatland in Sweden influenced by small‐scale, shallow groundwater systems. Data from different hydrogeological settings show reversals in groundwater flow leading to discharge in topographically high regions of peatlands in isolation from large‐scale groundwater flow. It is suggested that subsurface flow within peat can reverse in direction in response to water deficit and water‐table drawdown. The data presented here refute the assumption that local groundwater flow in peatlands is unidirectional and further illustrate the fact that measurable subsurface water flow can occur at depth in peat isolated from large‐scale groundwater flow systems. In the light of implicit assumptions made by many workers on water movement in peatlands, especially when connected to small‐scale groundwater systems, the consequences of such reversals are paramount in understanding the hydrology and biogeochemistry of peatlands. © 1997 by John Wiley & Sons, Ltd.