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Regressive modelling of soil water table fluctuations

Author

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  • Boucneau, G.
  • Van Meirvenne, M.
  • Desmet, J.
  • Hofman, G.

Abstract

Environmental and agricultural studies require spatial information on the soil water table level. Data collection based on dip-well measurements requires frequent measurements and a high number of dip-wells as the soil water table depth is varying strongly within short distances and time intervals. This paper presents a model based method, requiring a limited number of dip-wells and related mapped soil information, to describe water table depth fluctuations in time and space. A dip-well specific, regressive model was developed with meteorological data as input. This model described the fluctuations in time at the dip-well locations successfully. Based on the relationship between model parameters and mapped soil data, spatially extended models were created.

Suggested Citation

  • Boucneau, G. & Van Meirvenne, M. & Desmet, J. & Hofman, G., 1996. "Regressive modelling of soil water table fluctuations," Mathematics and Computers in Simulation (MATCOM), Elsevier, vol. 42(2), pages 271-277.
  • Handle: RePEc:eee:matcom:v:42:y:1996:i:2:p:271-277
    DOI: 10.1016/0378-4754(95)00125-5
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    References listed on IDEAS

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    1. Van der Sluijs, P. & De Gruijter, J. J., 1985. "Water table classes: A method to describe seasonal fluctuation and duration of water tables on Dutch soil maps," Agricultural Water Management, Elsevier, vol. 10(2), pages 109-125, September.
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