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Saline water tables are lowered by pumping or tile draining and the drainage water is stored in evaporation ponds.
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Currently, no model exists to simulate hormone fluxes from tile drains under field conditions.
Tile drains strongly influence the water cycle in agricultural catchment in terms of water quantity and quality.
Comparison of estimated tile drained areas from aerial image analysis shows a close agreement with estimated tile drained areas from previous studies (50% versus 46% drained area) which were based on GIS analysis and National Resource Inventory survey.
Implementing drainage water management at one of the subsurface tile drains decreased discharge (179 mm; 22%) and DOC loading (6.8 kg ha−1; 26%) compared to an adjacent free draining subsurface tile drain.
Subsurface tile drains influence watershed fluxes of nitrogen, phosphorus, and pesticides, but few studies have examined the role of subsurface tile drains and drainage water management practices on watershed dissolved organic carbon (DOC) export.
Mitigation of agricultural nitrogen (N) loss via tile drains using woodchip-based subsurface constructed wetlands seems promising.
We conclude that tile drains homogenize spatial patterns in hydrologic response by minimizing response differences between soil types.
Much of the water intercepted by the tile drains under the site was resident groundwater, rather than leachate from underneath the crops.
Tile drain NO3− concentrations were consistently elevated (4 38 mg l−1 N) relative to streamside soil and shallow groundwater exiting the same field (0.013 0.812 mg l−1 N).
Drainage water management (DWM) has received considerable attention as a potential best management practice (BMP) for improving water quality in tile drained landscapes.
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