TY - JOUR
T1 - Hydrous species in feldspars
T2 - A reassessment based on FTIR and SIMS
AU - Mosenfelder, Jed L.
AU - Rossman, George R.
AU - Johnson, Elizabeth A.
N1 - Publisher Copyright:
© 2015 by Walter de Gruyter Berlin/Boston.
PY - 2015/5/1
Y1 - 2015/5/1
N2 - Recent interest in hydrogen incorporation in feldspars has been driven by the potential of this common mineral species to record magmatic water contents. Accurate measurement of H concentrations in feldspars by Fourier transform infrared (FTIR) spectroscopy is hampered by the need to collect polarized spectra in three mutually perpendicular directions, which can be impractical for crystals characterized by small dimensions, polysynthetic twinning, and/or chemical zoning. SIMS is an attractive alternative to FTIR, offering high spatial resolution, high precision, and the feasibility of attaining low detection limits. In this study we compare FTIR and SIMS data for 19 feldspars, including plagioclase, anorthoclase, sanidine, microcline, and orthoclase. We present adjustments to previously published FTIR data on some of these samples. Our new SIMS and FTIR data are well correlated and we demonstrate the feasibility of quantitatively measuring H concentrations as low as 1-2 ppmw H2O using SIMS. Combination of the new data together with re-evaluation of the NMR calibration of Johnson and Rossman (2003) indicates that the IR absorption coefficients for hydrous species in feldspar increase with decreasing frequency of their O-H absorptions, in accord with theory. We derive new molar integral IR absorption coefficients (I) for feldspars with the following hydrous species as defined by Johnson and Rossman (2003): Type I and II H2O (microcline and orthoclase): I = 120 470 ± 11 360 L·mol-1 H2O cm-2 Type IIb OH (sanidine): I = 150 000 ± 15 000 L·mol-1 H2O cm-2 Type IIa OH (plagioclase and anorthoclase): I = 202 600 ± 20 260 L·mol-1 H2O cm-2 These absorption coefficients depend on critical assumptions with regards to SIMS matrix effects. If accurate, one important implication is that the H concentrations of plagioclase crystals estimated in the literature are too high by up to a factor of two, requiring revision of previously estimated plagioclasemelt H partitioning coefficients.
AB - Recent interest in hydrogen incorporation in feldspars has been driven by the potential of this common mineral species to record magmatic water contents. Accurate measurement of H concentrations in feldspars by Fourier transform infrared (FTIR) spectroscopy is hampered by the need to collect polarized spectra in three mutually perpendicular directions, which can be impractical for crystals characterized by small dimensions, polysynthetic twinning, and/or chemical zoning. SIMS is an attractive alternative to FTIR, offering high spatial resolution, high precision, and the feasibility of attaining low detection limits. In this study we compare FTIR and SIMS data for 19 feldspars, including plagioclase, anorthoclase, sanidine, microcline, and orthoclase. We present adjustments to previously published FTIR data on some of these samples. Our new SIMS and FTIR data are well correlated and we demonstrate the feasibility of quantitatively measuring H concentrations as low as 1-2 ppmw H2O using SIMS. Combination of the new data together with re-evaluation of the NMR calibration of Johnson and Rossman (2003) indicates that the IR absorption coefficients for hydrous species in feldspar increase with decreasing frequency of their O-H absorptions, in accord with theory. We derive new molar integral IR absorption coefficients (I) for feldspars with the following hydrous species as defined by Johnson and Rossman (2003): Type I and II H2O (microcline and orthoclase): I = 120 470 ± 11 360 L·mol-1 H2O cm-2 Type IIb OH (sanidine): I = 150 000 ± 15 000 L·mol-1 H2O cm-2 Type IIa OH (plagioclase and anorthoclase): I = 202 600 ± 20 260 L·mol-1 H2O cm-2 These absorption coefficients depend on critical assumptions with regards to SIMS matrix effects. If accurate, one important implication is that the H concentrations of plagioclase crystals estimated in the literature are too high by up to a factor of two, requiring revision of previously estimated plagioclasemelt H partitioning coefficients.
KW - FTIR
KW - SIMS
KW - calibration
KW - crust
KW - feldspar
KW - hygrometry
KW - nominally anhydrous minerals
KW - water
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U2 - 10.2138/am-2015-5034
DO - 10.2138/am-2015-5034
M3 - Article
AN - SCOPUS:84929620268
SN - 0003-004X
VL - 100
SP - 1209
EP - 1221
JO - American Mineralogist
JF - American Mineralogist
IS - 5-6
ER -