Interlaboratory comparison of humic substances compositional space as measured by Fourier transform ion cyclotron resonance mass spectrometry (IUPAC Technical Report)

Author:

Zherebker Alexander12,Kim Sunghwan3,Schmitt-Kopplin Philippe4,Spencer Robert G. M.5,Lechtenfeld Oliver6ORCID,Podgorski David C.7,Hertkorn Norbert4,Harir Mourad4,Nurfajin Nissa3,Koch Boris8,Nikolaev Eugene N.1,Shirshin Evgeny A.9,Berezin Sergey A.10,Kats Dmitry S.10,Rukhovich Gleb D.2,Perminova Irina V.2

Affiliation:

1. Skolkovo Institute of Science and Technology , Skolkovo , Russia

2. Lomonosov Moscow State University , Department of Chemistry , Moscow , Russia

3. Kyungpook National University , Department of Chemistry , Daegu , South Korea

4. Helmholtz Zentrum-Muenchen, Research Unit Analytical Biogeochemistry , Munich , Germany

5. Florida State University , Earth, Ocean & Atmospheric Science , Tallahassee , FL , USA

6. Helmholtz Zentrum-Leipzig , Leipzig , Germany

7. University of New Orleans , Pontchartrain Institute for Environmental Sciences , Department of Chemistry, New Orleans , LA , USA

8. Alfred Wegener Institute for Marine and Arctic Research , Bremerhaven , Germany

9. Lomonosov Moscow State University , Department of Physics , Moscow , Russia

10. Lomonosov Moscow State University , Department of Computing Mathematics , Moscow , Russia

Abstract

Abstract Interlaboratory comparison on the determination of the molecular composition of humic substances (HS) was undertaken in the framework of IUPAC project 2016-015-2-600. The analysis was conducted using high resolution mass spectrometry, nominally, Fourier transform ion cyclotron resonance mass spectrometry (FTICR MS) with electrospray ionization. Six samples of HS from freshwater, soil, and leonardite were used for this study, including one sample of humic acids (HA) from coal (leonardite), two samples of soil HA (the sod-podzolic soil and chernozem), two samples of soil fulvic acids (FA) (the sod-podzolic soil and chernozem), and one sample of freshwater humic acids (the Suwannee River). The samples were analyzed on five different FTICR MS instruments using the routine conditions applied in each participating laboratory. The results were collected as mass lists, which were further assigned formulae for the determination of molecular composition. The similarity of the obtained data was evaluated using appropriate statistical metrics. The results have shown that direct comparison of discrete stoichiometries assigned to the mass lists obtained by the different laboratories yielded poor results with low values of the Jaccard similarity score – not exceeding 0.56 (not more than 56 % of the similar peaks). The least similarity was observed for the aromatics-rich HA samples from leonardite (coal) and the chernozem soil, which might be connected to difficulties in their ionization. The reliable similarity among the data obtained in this intercomparison study was achieved only by transforming a singular point (stoichiometry) in van Krevelen diagram into a sizeable pixel (a number of closely located stoichiometries), which can be calculated from the population density distribution. The conclusion was made that, so far, these are descriptors of occupation density distribution, which provide the metrics compliant with the data quality requirements, such as the reproducibility of the data measurements on different instruments.

Funder

International Union of Pure and Applied Chemistry

Russian Foundation for Basic Research

Russian Science Foundation

Publisher

Walter de Gruyter GmbH

Subject

General Chemical Engineering,General Chemistry

Reference44 articles.

1. P. MacCarthy. Soil Sci.166, 738 (2001).

2. F. Stevenson. Humus Chemistry: Genesis, Composition, Reactions, p. 512, Wiley, New York, 2nd ed. (1994).

3. D. S. Orlov. Humic Substances of Soil and General Theory of Humification, p. 266, CRC Press, USA, 1st ed. (1995).

4. W. Ziechmann. Huminstoffe, p. 408 S, Verlag Chemie, Weinheim (1980).

5. A. Piccolo. Soil Sci.166, 810 (2001).

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