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Physical and Hydrological Characteristics of Ponds in Reclaimed Upland Landscape Settings and Their Impact on Agriculture Capability
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Pigot, M. E., Macyk, T. M., Moran, S. R., Trudell, M. R.
pond was perched above the water table. This pond was instrumented in September 1987 to monitor the subsurface water and salinity regime. Observations that continued throughout 1988 and 1989 provide the basis of this report. The closed basin responsible for the existence of pond S195 was formed by
produced a hydraulic barrier with sufficiently high density and low hydraulic conductivity that rapid downward drainage of the ponded water was prevented. The hydraulic conductivity was further reduced by sealing of the upper surface of the spoil as a result of structural collapse of sodic clay in