Raman spectroscopy study of manganese oxides: Tunnel structures

被引:95
作者
Post, Jeffrey E. [1 ]
McKeown, David A. [2 ]
Heaney, Peter J. [3 ]
机构
[1] Smithsonian Inst, Natl Museum Nat Hist, Dept Mineral Sci, Washington, DC 20013 USA
[2] Catholic Univ Amer, Vitreous State Lab, Washington, DC 20064 USA
[3] Penn State Univ, Dept Geosci, 540 Deike Bldg, University Pk, PA 16802 USA
关键词
Manganese oxide; Raman spectroscopy; todorokite; hollandite; X-RAY-DIFFRACTION; ROCK COATINGS; CS-EXCHANGE; BIRNESSITE; MECHANISMS; ADSORPTION; OXIDATION; BEHAVIOR; SPECTRA; METALS;
D O I
10.2138/am-2020-7390
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 mu W), 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.
引用
收藏
页码:1175 / 1190
页数:16
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