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Type-Curve Solution to Aquifer Tests under Water-Table Conditions   总被引:3,自引:0,他引:3  
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The Rainfall/Water-Table Level Relationship of an Unconfined Aquifer   总被引:1,自引:0,他引:1  
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Dimensionless Time-Drawdown Plots of Late Aquifer Test Data   总被引:1,自引:0,他引:1  
Zekâi &#;en 《Ground water》1988,26(5):615-618
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In order to understand the flow pattern around a pumping well partially penetrating a vertically extensive aquifer, a specially designed pumping test was carried out in Pakistan. In this paper salient features of the test have been described. The spatial distributions of drawdown have been shown graphically. Some of the preliminary conclusions made from the drawdown pattern include:
  • • The distance beyond which the flow is likely to be horizontal increases with decrease in the degree of aquifer penetration.
  • • In equidistant observation wells open at different depths, (1) the drawdowns tend to merge at larger times, provided the observation point is located within the screened section of the aquifer; (2) the less the depth of penetration is, the earlier the drawdowns start merging; and (3) the initial rate of drawdown near the aquifer top is slow but catches up with time to exceed those at deeper points.
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Pumping Test Analysis for a Tidally Forced Aquifer   总被引:3,自引:0,他引:3  
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Aquifer Test Analysis in Fractured Rocks with Linear Flow Pattern   总被引:2,自引:0,他引:2  
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