TY - JOUR
T1 - Raman spectroscopy study of manganese oxides
T2 - Tunnel structures
AU - Post, Jeffrey E.
AU - McKeown, David A.
AU - Heaney, Peter J.
N1 - Funding Information:
We are grateful for the invaluable assistance provided by Rob Wardell with operation of the Raman laboratory in the Smithsonian Department of Mineral Sciences. Funding for this work was provided by NSF Grant EAR-1925903.
Publisher Copyright:
© 2020 De Gruyter. All rights reserved.
PY - 2020/8/26
Y1 - 2020/8/26
N2 - Raman spectra were collected for an extensive set of well-characterized tunnel-structure Mn oxide mineral species employing a range of data collection conditions. Using various laser wavelengths, such as 785, 633, and 532 nm at low power levels (30-500 µW), as well as the comprehensive database of standard spectra presented here, it is generally possible to distinguish and identify the various tunnel structure Mn oxide minerals. The Raman mode relative intensities can vary significantly as a function of crystal orientation relative to the incident laser light polarization direction as well as laser light wavelength. Consequently, phase identification success is enhanced when using a standards database that includes multiple spectra collected for different crystal orientations and with different laser light wavelengths. For the hollandite-group minerals, the frequency of the Raman mode near 630 cm-1 shows a strong linear correlation with the fraction of Mn3+ in the octahedral Mn sites. With the comprehensive Raman database of well-characterized Mn oxide standards provided here (and available online as Supplemental Materials1), and use of appropriate data collection conditions, micro-Raman is a powerful tool for identification and characterization of biotic and abiotic Mn oxide phases from diverse natural settings, including on other planets.
AB - Raman spectra were collected for an extensive set of well-characterized tunnel-structure Mn oxide mineral species employing a range of data collection conditions. Using various laser wavelengths, such as 785, 633, and 532 nm at low power levels (30-500 µW), as well as the comprehensive database of standard spectra presented here, it is generally possible to distinguish and identify the various tunnel structure Mn oxide minerals. The Raman mode relative intensities can vary significantly as a function of crystal orientation relative to the incident laser light polarization direction as well as laser light wavelength. Consequently, phase identification success is enhanced when using a standards database that includes multiple spectra collected for different crystal orientations and with different laser light wavelengths. For the hollandite-group minerals, the frequency of the Raman mode near 630 cm-1 shows a strong linear correlation with the fraction of Mn3+ in the octahedral Mn sites. With the comprehensive Raman database of well-characterized Mn oxide standards provided here (and available online as Supplemental Materials1), and use of appropriate data collection conditions, micro-Raman is a powerful tool for identification and characterization of biotic and abiotic Mn oxide phases from diverse natural settings, including on other planets.
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U2 - 10.2138/am-2020-7390
DO - 10.2138/am-2020-7390
M3 - Article
AN - SCOPUS:85101132560
SN - 0003-004X
VL - 105
SP - 1175
EP - 1190
JO - American Mineralogist
JF - American Mineralogist
IS - 8
ER -