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Spatial analyses of groundwater levels using universal kriging
2007
Proceedings of the Indian Academy of Sciences, Earth and Planetary Sciences
For water levels, generally a non-stationary variable, the technique of universal kriging is applied in preference to ordinary kriging as the interpolation method. Each set of data in every sector can fit different empirical semivariogram models since they have different spatial structures. These models can be classified as circular, spherical, tetraspherical, pentaspherical, exponential, gaussian, rational quadratic, hole effect, K-bessel, J-bessel and stable. This study aims to determine
doi:10.1007/s12040-007-0006-6
fatcat:oqjgi4e33vc6noakatp2yhu25a