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Impact of long term drainage on summer groundwater flow patterns in the Mer Bleue peatland, Ontario, Canada

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Figure

Fig. 1.31vegetation between both sides of the transect. The 60 m Forest sitesupported on average 4900 g mthe 200 m Bog site only supported 690 g mwater level and the peat–clay interface
Table 1. Porosity and hydraulic conductivity estimates for each layer implemented in the steady-state and transient MODFLOW models.
Fig. 2. Figure 2  Pollen records of important trees at the site and testateamoeba-based water table reconstructions from peat cores sampledon each side of the drainage ditch (approx
Table 2. Estimates of the horizontal hydraulic conductivities across the transect determined by slug tests after Hvorslev (1951).
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