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  • Articles  (7)
  • transient recharge  (7)
  • Springer  (7)
  • National Academy of Sciences
  • 1995-1999  (7)
  • 1975-1979
  • Architecture, Civil Engineering, Surveying  (7)
  • Information Science and Librarianship
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  • Articles  (7)
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  • Springer  (7)
  • National Academy of Sciences
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  • Architecture, Civil Engineering, Surveying  (7)
  • Information Science and Librarianship
  • Geography  (7)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 12 (1998), S. 199-208 
    ISSN: 1573-1650
    Keywords: phreatic aquifer ; ground water ; water table ; transient recharge ; analytical solution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract Understanding the dynamic response of phreatic aquifers due to recharge is most important for the proper management of ground-water systems. In this paper an analytical solution is developed to describe the water-table fluctuation in a finite aquifer system due to transient recharge from two parallel strip basins. Application of the solution in the prediction of spatiotemporal variation of the water table and in the sensitivity analysis of the effects of various controlling parameters on the water-table fluctuation is demonstrated with the help of an example problem.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 12 (1998), S. 467-475 
    ISSN: 1573-1650
    Keywords: unconfined aquifer ; transient recharge ; water table ; analytical solution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract A prior knowledge of the water table fluctuations, in response to the proposed recharge scheme, is essential to achieve the preset objectives of ground water resources management. In this paper an analytical solution of the linearised Boussinesq's equation is presented to predict the spatio-temporal variation of the water table in an aquifer system in response to time-varying recharge applied through a rectangular basin. The recharge function is approximated by introducing a number of line segments depending on its nature of variation. The solution is obtained by using finite Fourier sine transform and its application is demonstrated for a case of periodically applied recharge.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 12 (1998), S. 271-284 
    ISSN: 1573-1650
    Keywords: analytical solution ; ground-water ; recharge basin ; transient recharge ; water-table
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract An analytical solution of the linearized Boussinesq equation is developed to predict the formation of a ground-water mound in an aquifer system in response to localized time-varying recharge. The recharge is applied from a centrally located circular basin. The solution is obtained using an eigenvalue-eigenfunction method. The solution for a constant recharge rate is shown as a special case of the solution for a time-varying recharge rate. Application of the solution to predict ground-water mound formation is demonstrated by a numerical example. Effects of variation in the rate of reachrge, size of recharge basin and the saturated hydraulic conductivity on the growth of the water-table are also investigated.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 9 (1995), S. 127-138 
    ISSN: 1573-1650
    Keywords: Aquifer ; water table ; transient recharge ; drain ; analytical solution ; prediction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract Recharging of aquifers due to irrigation, seepage from canal beds and other sources leads to the growth of water table near to the ground surface causing problems like water logging and increase of salinity in top soils in many regions of the world. This problem can be alleviated if proper knowledge of the spatio — temporal variation of the water table is available. In this paper an analytical solution for the water table fluctuation is presented for a 2-D aquifer system having inclined impervious base with a small slope in one — direction and receiving time varying vertical recharge. Application of the solution in estimation of water table fluctuation is demonstrated with the help of an example problem.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 9 (1995), S. 27-37 
    ISSN: 1573-1650
    Keywords: Groundwater flow ; transient recharge ; strip basin ; analytical solution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract Two cases of water-table fluctuation in a finite aquifer in response to transient recharge from a strip basin are investigated. In the first case the aquifer is bounded by open water-bodies, whereas in second one the aquifer is bounded by impermeable boundaries on both sides. Analytical solutions are presented to predict the transient position of the water-table. The solutions are obtained by using finite Fourier sine and cosine transforms.
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 10 (1996), S. 189-198 
    ISSN: 1573-1650
    Keywords: aquifer ; transient recharge ; groundwater mound ; analytical solution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract Recharge to the aquifer leads to the growth of a groundwater mound. Therefore, for the proper management of an aquifer system, an accurate prediction of the spatio-temporal variation of the water table is very essential. In this paper, a problem of groundwater mound formation in response to a transient recharge from a rectangular area is investigated. An approximate analytical solution has been developed to predict the transient evolution of the water table. Application of the solution and its sensitivity to the variation of the recharge rate have been illustrated with the help of a numerical example.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Water resources management 11 (1997), S. 185-196 
    ISSN: 1573-1650
    Keywords: Unconfined aquifer ; transient recharge ; water table ; analytical solution
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Notes: Abstract An analytical solution is developed to predict spatio-temporal variation of the water table in a 2-D aquifer system which is receiving transient recharge from an overlying basin of rectangular shape. The transient recharge function is approximated by a number of line segments. Application of the solution is demonstrated with the help of an example problem.
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