2007Unpublished venueRequires access

Spatial Informations of Underground Water Level Based on Applied Geostatistics

Weiguang Wang

Open publisher page 1 citations

Abstract

The statistical method is one of most effective tools to describe many phenomena qualitatively or quantitatively from sampling. However,the information containing in spatial locations of samples is not considered and used in most of statistical procedures. In geostatistics, the traditional statistical method is utilized and the spatial information is taken into account. Geostatistical methods have been expanded to many other scientific fields for their unique statistical and interpolating advantages. In this paper, we applied ordinary kriging technique, one of the geostatistical methods, to analyze the spatial variability and gain the spatial informations of annual underground water level at 203 observation wells for Yellow River watershed during the period from 1997~2001.The result revealed that the semi-variograms of water level were best described by spherical variogram model. The final parameters attained indicated that the range of every year presented geometry anisotropy. Underground water level is one most important factor of water balance. So gaining the spatial informations of underground water level accurately is invaluable for understanding water cycle process.

About this research paper

What this paper is about

The statistical method is one of most effective tools to describe many phenomena qualitatively or quantitatively from sampling. However,the information containing in spatial locations of samples is not considered and used in most of statistical procedures. In geostatistics, the traditional statistical method is utilized and the spatial information is taken into account. Geostatistical methods have been expanded to many other scientific fields for their unique statistical and interpolating advantages. In this paper, we applied ordinary kriging technique, one of the geostatistical methods, to analyze the spatial variability and gain the spatial informations of annual underground water level at 203 observation wells for Yellow River watershed during the period from 1997~2001.The result revealed that the semi-variograms of water level were best described by spherical variogram model. The final parameters attained indicated that the range of every year presented geometry anisotropy. Underground water level is one most important factor of water balance. So gaining the spatial informations of underground water level accurately is invaluable for understanding water cycle process.

Why it matters

OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The statistical method is one of most effective tools to describe many phenomena qualitatively or quantitatively from sampling. However,the information containing in spatial locations of samples is not considered and used in most of statistical procedures. In geostatistics, the traditional statistical method is utilized and the spatial information is taken into account. Geostatistical methods have been expanded to many other scientific fields for their unique statistical and interpolating advantages. In this paper, we applied ordinary kriging technique, one of the geostatistical methods, to analyze the spatial variability and gain the spatial informations of annual underground water level at 203 observation wells for Yellow River watershed during the period from 1997~2001.The result revealed that the semi-variograms of water level were best described by spherical variogram model. The final parameters attained indicated that the range of every year presented geometry anisotropy. Underground water level is one most important factor of water balance. So gaining the spatial informations of underground water level accurately is invaluable for understanding water cycle process.

Key concepts: Geostatistics, Variogram, Kriging, Spatial analysis, Sampling (signal processing), Spatial variability, Range (aeronautics), Spatial dependence

Related papers

Back to paper searchBrowse research topicsOriginal source
Spatial Informations of Underground Water Level Based on Applied Geostatistics — Research Paper | ScholarLens