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Created: | May 05, 2025 at 4:18 p.m. | |
Last updated: | May 05, 2025 at 4:27 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Discoverable |
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Abstract
This data contains major anion and cation analyses for shallow groundwater samples and irrigation water samples, taken following 1 irrigation event in July 2022 and 1 irrigation event in July 2024. Data is also plotted on Piper Diagrams for visualization as water chemistry evolves following an irrigation event. Preliminary results show that water becomes more Na Cl rich, from Ca-Mg-CaCO3. The irrigation water applied is much more dilute than any groundwater samples, suggesting that the change in chemistry comes from processes happening within the vadose zone as water percolates following irrigation - dissolving existing soluble salts (NaCl) and precipitating less soluble salts (CaCO3).
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Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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U.S. National Science Foundation | Collaborative Research: SitS: Development of multiple-scale sensor and remote sensing technology to quantify abiotic carbon dioxide emission in irrigated soils of aridlands | 2034312 |
U.S. National Science Foundation | Network Cluster: Patterns and controls of ecohydrology, CO2 fluxes, and nutrient availability in pedogenic carbonate-dominated dryland critical zones | 2012475 |
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This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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