Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6409956 | Journal of Hydrology | 2016 | 15 Pages |
â¢Explore reasons for failure of large diameter wells when used for irrigation.â¢Detailed field information leads to conceptual and computational models.â¢Computational models allow the preparation of water balances.â¢Seepage faces limit the volume of water pumped from the shallow aquifer.â¢Recommendation that dry season crop over only half of land holding.
SummaryLarge diameter wells in shallow weathered aquifers provide a valuable source of water for domestic and agricultural purposes in many locations including the Indian subcontinent. However, when used for irrigation, these wells often fail towards the end of the dry season. By considering two case studies in the dry and intermediate rainfall zones of Sri Lanka, reasons for the limited yield of these wells are identified. The first case study is concerned with a sloping catchment; a significant proportion of the precipitation during the rainy season either becomes runoff or passes down-gradient through the aquifer and is discharged at the ground surface. Furthermore, during the dry season, groundwater discharge continues. In the second case study the topography is generally flat but, even though the aquifer fills most years during the rainy season, there is often only sufficient water to irrigate about half of each farmer's holding. These investigations are based on field information and the development of conceptual and computational models. Of critical importance in assessing the long term yield of a well is the formation of a seepage face on the side of the well, with the water table a significant distance above the pumping water level. Consequently the water table may only be lowered to about half the depth of the well. The paper concludes with recommendations for the exploitation of groundwater from shallow weathered aquifers to minimise the risk of failure during the dry season.