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The dynamics of a shallow perched watertable on a heavy soil in the Lower Herbert Valley

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The duration and dynamics of a shallow perched watertable was measured, and modelled and the amount of subsurface flow (interflow) from the watertable to the in-field drains (water furrows) was quantified. A watertable model was used to test the robustness of the measured soil hydraulic propelties and to predict the relative duration of waterlogging between a field with and without water furrows. The presence and duration of the shallow perched watertable agreed with other observations. The amount of inter±1ow was calculated and was found to be only a small component of the water balance (9%). The presence of the water furrows in the field design was found to decrease the length of waterlogging by II days over a ISO-day period.
File Name: 2001_pa_ag26.pdf
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