Why strontium baselines should be based on pristine areas only: The disturbing effect of agricultural lime revisited
- 1Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade 2, 8000, Aarhus C, Denmark.
- 0Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade 2, 8000, Aarhus C, Denmark.
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View abstract on PubMed
Summary
This summary is machine-generated.Agricultural lime lowers groundwater 87Sr/86Sr ratios in farmland. Pristine areas retain higher ratios, indicating lime
Area Of Science
- Geochemistry
- Environmental Science
- Hydrogeology
Background
- The 87Sr/86Sr ratio in groundwater is a key geochemical tracer.
- Understanding anthropogenic impacts on natural strontium isotope signatures is crucial for environmental monitoring.
Purpose Of The Study
- To investigate the impact of agricultural practices on groundwater 87Sr/86Sr ratios.
- To differentiate between natural and anthropogenic sources of strontium in meltwater plain environments.
Main Methods
- Analysis of 87Sr/86Sr ratios in groundwater and vadose zone sand from boreholes.
- Comparison of isotope ratios in pristine (heath/forest) and agricultural (farmland) areas.
- Evaluation of potential strontium sources, including agricultural lime and carbonate clasts.
Main Results
- Groundwater and vadose zone sand exhibit significantly lower 87Sr/86Sr ratios in farmland compared to pristine areas.
- The observed decrease in 87Sr/86Sr ratios in farmland is attributed to the application of agricultural lime.
- Strontium from agricultural lime is mobile and not retained in topsoil.
Conclusions
- Agricultural lime application demonstrably alters groundwater strontium isotope signatures.
- Pristine areas serve as a better reference for natural strontium baselines.
- Groundwater and surface water in contact with farmland are unsuitable for establishing natural strontium baselines.
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