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Regressive modelling of soil water table fluctuations

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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.

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Chicago
Boucneau, Geert, Marc Van Meirvenne, J Desmet, and Georges Hofman. 1996. “Regressive Modelling of Soil Water Table Fluctuations.” Ed. RJL Hanus. Mathematics and Computers in Simulation 42 (2-3): 271–277.
APA
Boucneau, G., Van Meirvenne, M., Desmet, J., & Hofman, G. (1996). Regressive modelling of soil water table fluctuations. (R. Hanus, Ed.)MATHEMATICS AND COMPUTERS IN SIMULATION, 42(2-3), 271–277. Presented at the 1st IMACS/IFAC symposium on Mathematical Modelling and Simulation in Agriculture and Bio-Industries (M2SABI).
Vancouver
1.
Boucneau G, Van Meirvenne M, Desmet J, Hofman G. Regressive modelling of soil water table fluctuations. Hanus R, editor. MATHEMATICS AND COMPUTERS IN SIMULATION. 1996;42(2-3):271–7.
MLA
Boucneau, Geert, Marc Van Meirvenne, J Desmet, et al. “Regressive Modelling of Soil Water Table Fluctuations.” Ed. RJL Hanus. MATHEMATICS AND COMPUTERS IN SIMULATION 42.2-3 (1996): 271–277. Print.
@article{190729,
  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.},
  author       = {Boucneau, Geert and Van Meirvenne, Marc and Desmet, J and Hofman, Georges},
  editor       = {Hanus, RJL},
  issn         = {0378-4754},
  journal      = {MATHEMATICS AND COMPUTERS IN SIMULATION},
  language     = {eng},
  location     = {Brussels, Belgium},
  number       = {2-3},
  pages        = {271--277},
  title        = {Regressive modelling of soil water table fluctuations},
  url          = {http://dx.doi.org/10.1016/0378-4754(95)00125-5},
  volume       = {42},
  year         = {1996},
}

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