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Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
Published on: September 12, 2017
Application and evaluation of kriging and cokriging methods on groundwater depth mapping
Seyed Hamid Ahmadi1, Abbas Sedghamiz
1Agricultural Research and Education Organization, Agricultural Engineering Research Institute, P.O. Box 73415-111, Zarghan, Iran. seyedhamid.ahmadi@gmail.com
Geostatistical methods like kriging and cokriging effectively map groundwater depth variations in arid regions. Cokriging offers slightly improved accuracy for water resource management under diverse climatic conditions.
Area of Science:
- Environmental Science
- Hydrogeology
- Geostatistics
Background:
- Sustainable water resources management is crucial for arid and semi-arid regions.
- Understanding groundwater depth fluctuations is vital for conserving water resources.
- Geostatistical techniques can reveal critical water resource conditions.
Purpose of the Study:
- To evaluate kriging and cokriging methods for mapping groundwater depth.
- To analyze spatial variations in groundwater depth across different climatic conditions (dry, wet, normal).
- To assess the accuracy of geostatistical approaches for water resource management.
Main Methods:
- Geostatistical analysis using kriging and cokriging.
- Mapping groundwater depth over a 12-year period with significant climatic variations.
- Calculating Root Mean Square Error (RMSE) to compare method accuracy.
Main Results:
- Groundwater depth exhibits spatial variability influenced by climatic conditions.
- Cokriging demonstrated slightly higher accuracy than kriging in mapping groundwater depth.
- Both methods showed underestimation, with cokriging providing less biased results across different climate types.
Conclusions:
- Geostatistical approaches, particularly cokriging, are reliable for mapping groundwater depth.
- Farming in dry conditions requires careful management due to high groundwater depth variability.
- These methods aid water resource managers in allocating groundwater under varying environmental conditions.
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