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Spatial estimation of aquifer’s hydraulic parameters by a combination of borehole data and inverse solution

  • Mohammad-Mahdi Ansarifar
  • Meysam SalarijaziEmail author
  • Khalil Ghorbani
  • Abdol-Reza Kaboli
Original Paper
  • 51 Downloads

Abstract

A combination of borehole data interpretation and inverse solution method used to estimate the spatial distribution of hydraulic conductivity (K) and specific yield (Sy) for the Bandar-e Gaz unconfined aquifer located in Northern Iran considering no access to pumping test data. A numerical model used to simulate the behavior of the aquifer in two 12-month calibration and validation periods. The Nash-Sutcliffe criterion in calibration and validation periods indicates a completely appropriate accuracy and reliability of the combined method. The values of calibrated K and Sy by the inverse solution method are in accordance with their initial estimated values based on boreholes logs data. The estimated K and Sy are in the ranges of 5–15 and 0.024–0.036 m/day and their spatial distribution pattern shows a decreasing trend in the south-to-north direction, which is well suited to the spatial pattern of aquifer sediment’s type and size.

Keywords

Groundwater Hydraulic conductivity Specific yield Boreholes logs Numerical model 

Notes

Acknowledgments

This manuscript extracted from an MSc thesis at the Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran, and the authors are grateful to the University to provide the conditions for conducting this research.

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Department of Water Engineering, Faculty of Water and Soil EngineeringGorgan University of Agricultural Sciences and Natural ResourceGolestanIran
  2. 2.Abdol-Reza Kaboli Expert of HydrogeologyGolestan Regional Water CompanyGolestanIran

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