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- W765859100 abstract "Groundwater level changes in coastal aquifers occur due to oceanic tides, where the properties of oceanic tides can be applied to estimate hyadraulic parameters. Hydraulic parameters of coastal aquifers located in eastern part of Jeju island were estimated using the tidal response technique. Groundwater level data from a saltwater intrusion monitoring well system was used which showed tidal effects from 3 to 5 km. The hydraulic gradient was assessed by utilizing the filtering method from 71 consecutive hourly water-level observations. Calculated hydraulic diffusivity ranged from 2.94 to 4.36 . The hydraulic gradient of the coastal aquifer area was found to be ~, whereas the gradient of the area between wells Handong-1 and 2 was found to be ~, which is very low comparatively. Analysis of groundwater monitoring data showed that groundwater levels are periodically higher near coastal areas compared to that of inner land areas due to oceanic tide influences. When assessing groundwater flow direction in coastal aquifers it is important to consider tidal fluctuation." @default.
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- W765859100 date "2005-01-01" @default.
- W765859100 modified "2023-09-24" @default.
- W765859100 title "Analysis of Hydraulic Gradient at Coastal Aquifers in Eastern Part of Jeju Island" @default.
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