Assessment of Geostatistical Methods for Determining Distribution Patterns of Groundwater Resources in Sari-Neka Coastal Plain, Northern Iran

Document Type : Research Paper

Authors

1 Department of Watershed Management, Sari Agricultural Sciences and Natural Resources University, Sari, I

2 Department of Watershed Management, Sari Agricultural Sciences and Natural Resources University, Sari, Iran

Abstract

This study aimed to evaluate the temporal change and accuracy of interpolation techniques
used for spatial zonation of two groundwater quantity parameters including water table and
depth to water table over 11 years. The study was conducted based on the data collected
from piezometric wells of Sari-Neka Plain in Mazandaran Province, Iran. The investigated
methods included a set of geostatistical approaches involving simple Kriging, ordinary
Kriging, Radial Basis Function (RBF), and a deterministic interpolation method called
Inverse Distance Weighting (IDW) with powers of 1 and 5. Subsequent to quality control
and data normalization, the most appropriate variogram was chosen based on low RSS and
high r2 while the most suitable interpolation technique was determined regarding the cross
validation, Mean Absolute Error (MAE), and Mean Bias Error (MBE). The results
demonstrated that Simple Kriging was the most suitable method for zoning the depth to
groundwater over the years 2001, 2006, and 2012. Meanwhile, the most suitable methods
for zoning the water table included IDW with a power of 1for the year 2001, RBF for the
year 2006, and IDW with a power of 5 for the year 2012. The important finding was that
the interpolation methods showed a lower error for estimating water table than estimating
depth to groundwater. This study also revealed a drop in water table in the study area over
the 11 years’ period. Meanwhile, new water table classes have been added and extended
between the years 2006 and 2012 that had not existed five years earlier. The highest water
table losses were observed in three points at 13m depth to water table in the middle and
northern parts of the study area.

Keywords


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