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Hyperspectral Imaging as a Tool to Study Optical Anisotropy in Lanthanide-Based Molecular Single Crystals
Published on: April 14, 2020
EPR and optical absorption spectral studies on sphalerite mineral
K Seshamaheswaramma1, G Udayabhaskara Reddy, A Varada Reddy
1Dept. of Chemistry, Tirupati 517 502, India.
Summary
This study characterizes sphalerite (Zn,Fe)S using spectroscopy, identifying iron and manganese impurities within its crystal lattice. These impurities substitute into the lattice, with iron present in higher concentrations than manganese.
Area of Science:
- Mineralogy
- Materials Science
- Spectroscopy
Background:
- Sphalerite (Zn,Fe)S is a significant zinc sulfide mineral.
- Understanding impurity incorporation is crucial for its properties.
Purpose of the Study:
- To characterize sphalerite (Zn,Fe)S using advanced spectroscopic techniques.
- To identify and quantify iron and manganese impurities within the mineral lattice.
- To elucidate the structural environment of these impurities.
Main Methods:
- X-ray diffraction (XRD) for structural analysis.
- Electron Paramagnetic Resonance (EPR) spectroscopy to detect and characterize paramagnetic impurities.
- Near-Infrared (NIR) spectroscopy for vibrational analysis and identification of molecular species.
Main Results:
- Optical absorption and EPR spectra confirmed the presence of iron (Fe) and manganese (Mn(II)) impurities.
- Iron was identified in a distorted octahedral environment, with higher concentrations than manganese.
- Manganese (Mn(II)) was also found in a distorted octahedral environment.
- NIR spectroscopy indicated the presence of water and sulfide fundamentals, supporting the sphalerite formula and absence of sulfates.
Conclusions:
- Iron and Mn(II) impurities substitute into the sphalerite lattice.
- The mineralogical characterization confirms the presence and structural state of key impurities.
- The findings contribute to a deeper understanding of sphalerite composition and formation conditions.
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