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A diagnosis of sub-surface water table dynamics in low hydraulic conductivity soils in the sugar cane fields of Pongola,South Africa
Institution:1. Department of Nanomedicine, Houston Methodist Research Institute, Houston, Texas 77030;2. Pain Therapy Service, University of Pavia‐Fondazione IRCCS Policlinico San Matteo, Pavia, Italy;3. Bioceramics and Bio‐Hybrid Materials, National Research Council of Italy – ISTEC, Faenza, Ravenna 48018, Italy;4. Department of Life and Environmental Sciences, Università Politecnica delle Marche, Ancona 60131, Italy;5. Department of Biomedical Engineering, University of Houston, Houston, Texas;6. Department of Surgery, Houston Methodist Hospital, Houston, Texas 77030;7. Department of Clinic Surgical Pediatric and Diagnostic Sciences, University of Pavia, Pavia, Italy
Abstract:Water and land are the two natural resources restraining crop production in South Africa. With the increasing demand for food, emphasis has shifted from the sole reliance on rain fed crop production, to irrigation. The deterioration in irrigation water quality from surface water sources is, however, posing a big challenge to the sustainability of irrigated crop production. This is because more water is required for leaching, resulting in shallow water tables in agricultural lands. The installation of well designed subsurface drainage systems alone is not enough; the provision of timely maintenance is also necessary. In this study, the extent and severity of problems as a consequence of shallow water tables and their possible causes were investigated at three sugarcane fields in Pongola, South Africa, having low hydraulic conductivity soils. Also investigated were soil salinity levels and the temporal variation in the salinity of the irrigation water. A water table map of a 32 ha sugarcane field was generated, using observed water table depth (WTD) data from 36 piezometers monitored from September 2011 to February 2012. Out of the total 32 ha under cultivation, 12% was found to be affected by shallow WTDs of less than the 1.0 m design WTD. The inability of natural drainage to cope with subsurface drainage needs and the poor maintenance of subsurface drainage systems contributed to the shallow water tables in the area. Furthermore, the currently adopted drainage design criteria also proved unsatisfactory with mean observed water table depth and drainage discharge (DD) of 20% and 50%, respectively, less than their respective design levels. The salinity of the irrigation water was, on average, 32% higher than threshold tolerance level of sugarcane. The root zone soil salinity levels at the three study sites were greater than the 1.7 dS m?1 threshold for sugar cane. The subsurface drainage design criteria adopted at the site needs to be revisited by ensuring that the slope of the land is taken into consideration in the drainage design in addition to adhering to a recommended maintenance schedule.
Keywords:Drainage design  Drain depth and spacing  Soil salinity  Sum of water table exceedance  Water table depth
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