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  FeMnOx-1: A new microanalytical reference material for the investigation of Mn-Fe rich geological samples

Jochum, K. P., Wilson, S. A., Becker, H., Garbe-Schonberg, D., Groschopf, N., Kadlag, Y., et al. (2016). FeMnOx-1: A new microanalytical reference material for the investigation of Mn-Fe rich geological samples. Chemical Geology, 432, 34-40. doi:10.1016/j.chemgeo.2016.03.026.

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 Creators:
Jochum, K. P.1, Author           
Wilson, S. A.2, Author
Becker, H.2, Author
Garbe-Schonberg, D.2, Author
Groschopf, N.2, Author
Kadlag, Y.2, Author
Macholdt, D. S.1, Author           
Mertz-Kraus, R.2, Author
Otter, L. M.1, Author           
Stoll, B.1, Author           
Stracke, A.2, Author
Weis, U.1, Author           
Haug, Gerald H.1, Author           
Andreae, M. O.3, Author           
Affiliations:
1Climate Geochemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_2237635              
2external, ou_persistent22              
3Biogeochemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826286              

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 Abstract: Suitable Mn-Fe rich microanalytical reference materials (MRMs) as calibration material for laser ablation-inductively coupled plasma mass spectrometry (LA-ICPMS) have not been available. The United States Geological Survey (USGS) in collaboration with the Max Planck Institute for Chemistry has prepared a synthetic MRM, FeMnOx-1, with elevated mass fractions of MnO (25 g/100 g), Fe2O3 (8.5 g/100 g) and high mass fractions of 25 trace elements varying between 200 and 5000 mg/kg. This new MRM has been designed as calibration material for a wide range of different Mn-Fe deposits, such as desert/rock varnish, ocean crusts and nodules as well as Mn accumulations in soils and lakes. Small-scale and large-scale homogeneity of FeMnOx-1 were tested with three LA systems (200 nm femtosecond, and 193 nm and 213 nm nanosecond lasers) using different spot sizes and fluences. Our results demonstrate that FeMnOx-1 is homogeneous in the pg to mu g and nm to mu m range and therefore well suited for microanalytical applications. The relative standard deviation (RSD) values obtained from repeated measurements are about 2-3% for test portion masses of 5-100 ng, and are comparable to those of the homogeneous NIST SRM610 and USGS GSE-1G reference glasses. Homogeneity of FeMnOx-1 was also verified for a test portion of 0.1 ng. Seven laboratories using five different bulk and microanalytical techniques were involved in the characterization of FeMnOx-1. Small amounts of this MRM can be obtained on request from the authors. (C) 2016 Elsevier B.V. All rights reserved.

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Language(s): eng - English
 Dates: 2016
 Publication Status: Issued
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Title: Chemical Geology
  Other : Chem. Geol.
Source Genre: Journal
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Publ. Info: Amsterdam : Elsevier
Pages: - Volume / Issue: 432 Sequence Number: - Start / End Page: 34 - 40 Identifier: ISSN: 0009-2541
CoNE: https://pure.mpg.de/cone/journals/resource/954925389240