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Laboratory study of trace element release and environmental risks from shale-fracturing fluid interactions
Alison R Keimowitz1, George L Diehl2, Ryan N Farley3
1Chemistry Department, Vassar College, 124 Raymond Avenue, Poughkeepsie, NY 12601, United States.
Journal of Hazardous Materials
|September 17, 2025
Summary
Hydraulic fracturing fluid alters shale geochemistry, mobilizing hazardous trace elements. These elements can enter water sources, posing environmental risks as extraction sites age.
Area of Science:
- Geochemistry
- Environmental Science
- Earth Science
Background:
- Hydraulic fracturing (fracking) is a key natural gas extraction method.
- Black shales, like the Marcellus, are targeted for extraction.
- Fracking fluid interacts with shale, altering mineralogy and mobilizing trace elements.
Purpose of the Study:
- Investigate trace element release and redistribution during fracking.
- Analyze geochemical reactions between fracking fluid and shale.
- Assess long-term environmental mobility of mobilized elements.
Main Methods:
- Laboratory experiments simulating fracking stages (shut-in, flowback, production, closure).
- Analysis of geochemical reactions and mineralogical changes in shale.
- Monitoring of trace element mobilization and redistribution.
Main Results:
- Acid additions during shut-in dissolve carbonates and sulfides, leading to sulfide oxidation and mineral transformations.
- Trace elements are released via acid dissolution during initial production.
- Some elements (lanthanides, Zn, Sr) are lost from the solid phase.
- Elements like As, Mo, and U are converted to more mobile mineral forms.
Conclusions:
- Fracking processes significantly alter shale geochemistry.
- Mobilized trace elements, particularly As, Mo, and U, pose risks for long-term environmental mobility.
- Potential for drinking water contamination increases with aging well networks.
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