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Updated: Jul 1, 2025

Fluid-cell Raman Spectroscopy for operando Studies of Reaction and Transport Phenomena during Silicate Glass Corrosion
Published on: May 9, 2025
Predicting Silicate Glass Geochemistry Using Raman Spectroscopy and Supervised Machine Learning: Partial Least Square
Blake O LaDouceur1, Molly McCanta1, Bhavya Sharma2
1Department of Earth and Planetary Sciences, University of Tennessee at Knoxville, Knoxville, Tennessee, USA.
Raman spectroscopy quantifies geochemistry in silicate glasses using partial least squares (PLS) calibration. This method accurately predicts major oxides, offering a foundation for analyzing amorphous silicates.
Area of Science:
- Geochemistry
- Spectroscopy
- Materials Science
Background:
- Accurate geochemical analysis of silicate glasses is crucial for various scientific disciplines.
- Traditional methods can be time-consuming and destructive.
- Raman spectroscopy offers a rapid, non-destructive analytical technique.
Purpose of the Study:
- To develop a quantitative geochemical analysis method for silicate glasses using Raman spectroscopy and partial least squares (PLS) calibration.
- To establish oxide-specific models for predicting major element concentrations (wt%) in synthetic and natural silicate glasses.
- To investigate the efficacy of multivariate analysis for Raman spectroscopic data in geochemistry.
Main Methods:
- Utilized Raman spectroscopy to collect spectral data from synthetic and natural silicate glass samples.
- Developed univariate partial least squares (PLS) calibration models for quantifying eight major oxides (SiO2, Na2O, K2O, CaO, TiO2, Al2O3, FeOT, MgO).
- Trained PLS models on 48 samples and validated on 21 held-out samples, also testing on an external set of 11 natural basaltic glasses.
Main Results:
- Achieved accurate predictions for major oxides with average root mean square errors for calibration, cross-validation, and prediction around 2.4-2.9 wt%.
- Identified key Raman spectral channels crucial for the regression of specific oxides.
- Demonstrated that Raman band shifts correlate with oxidation state and silica concentration, influenced by Fe3+/Fe2+ ratios and SiO2 content.
Conclusions:
- Partial least squares (PLS) calibration combined with Raman spectroscopy provides a robust method for quantitative geochemical analysis of silicate glasses.
- The developed models show potential for analyzing amorphous silicates, with preliminary validation on natural samples indicating suitability for specific applications.
- This study establishes a foundational approach for future advancements in Raman spectroscopy for geochemical analysis of silicate materials.
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