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Study on water-rock interactions of trace elements in groundwater with leaching experiments
1Department of Geoscience, University of Nevada Las Vegas, Las Vegas, NV 89154.
Trace element analysis of aquifer rocks reveals groundwater origins and flowpaths. Understanding host rock mineralogy and leaching helps identify water sources and mixing patterns in Southern Nevada.
Area of Science:
- Geochemistry
- Hydrogeology
- Environmental Science
Background:
- Trace elements leached from host rocks act as fingerprints for groundwater sources.
- Understanding groundwater flowpaths and mixing is crucial for water resource management.
- Aquifer geochemistry plays a vital role in contaminant transport and remediation.
Purpose of the Study:
- To investigate the leaching characteristics of trace elements from Southern Nevada aquifer host rocks.
- To determine the influence of experimental conditions (time, pH, grain size, mineralogy) on trace element leaching.
- To correlate host rock mineralogy with leachate composition for groundwater source identification.
Main Methods:
- Leaching experiments were conducted on three Southern Nevada aquifer host rocks.
- 13 trace elements were analyzed under varying experimental conditions.
- Geochemical modeling was used to simulate solute speciation and saturation indices.
Main Results:
- The fraction of leached trace elements varied significantly based on host rock type and experimental conditions.
- Host rock mineralogy was found to be a key factor influencing leachate composition.
- Geochemical modeling provided insights into trace element redistribution and leaching mechanisms.
Conclusions:
- Trace element leaching from aquifer rocks provides valuable information on groundwater origin and flow.
- Host rock mineralogy is a critical determinant of groundwater chemistry.
- This study enhances the understanding of water-rock interactions in arid environments.
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