Combination of geostatistics and self-organizing maps for the spatial analysis of groundwater level variations in complex hydrogeological systems

Journal Article (2023)
Author(s)

Emmanouil A. Varouchakis (Technical University of Crete)

Dimitri P. Solomatine (TU Delft - Water Resources, IHE Delft Institute for Water Education)

Gerald Corzo Corzo Perez (IHE Delft Institute for Water Education)

Seifeddine Jomaa (Helmholtz Centre for Environmental Research - UFZ)

George P. Karatzas (Technical University of Crete)

Research Group
Water Resources
Copyright
© 2023 Emmanouil A. Varouchakis, D.P. Solomatine, Gerald A. Corzo Perez, Seifeddine Jomaa, George P. Karatzas
DOI related publication
https://doi.org/10.1007/s00477-023-02436-x
More Info
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Publication Year
2023
Language
English
Copyright
© 2023 Emmanouil A. Varouchakis, D.P. Solomatine, Gerald A. Corzo Perez, Seifeddine Jomaa, George P. Karatzas
Research Group
Water Resources
Issue number
8
Volume number
37
Pages (from-to)
3009-3020
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Abstract

Successful modelling of the groundwater level variations in hydrogeological systems in complex formations considerably depends on spatial and temporal data availability and knowledge of the boundary conditions. Geostatistics plays an important role in model-related data analysis and preparation, but has specific limitations when the aquifer system is inhomogeneous. This study combines geostatistics with machine learning approaches to solve problems in complex aquifer systems. Herein, the emphasis is given to cases where the available dataset is large and randomly distributed in the different aquifer types of the hydrogeological system. Self-Organizing Maps can be applied to identify locally similar input data, to substitute the usually uncertain correlation length of the variogram model that estimates the correlated neighborhood, and then by means of Transgaussian Kriging to estimate the bias corrected spatial distribution of groundwater level. The proposed methodology was tested on a large dataset of groundwater level data in a complex hydrogeological area. The obtained results have shown a significant improvement compared to the ones obtained by classical geostatistical approaches.