Analytical and Bioanalytical Chemistry

, Volume 408, Issue 2, pp 651–655 | Cite as

Application of 13C ramp CPMAS NMR with phase-adjusted spinning sidebands (PASS) for the quantitative estimation of carbon functional groups in natural organic matter

Note

Abstract

The composition of carbon (C) functional groups in natural organic matter (NOM), such as dissolved organic matter, soil organic matter, and humic substances, is frequently estimated using solid-state 13C NMR techniques. A problem associated with quantitative analysis using general cross polarization/magic angle spinning (CPMAS) spectra is the appearance of spinning side bands (SSBs) split from the original center peaks of sp 2 hybridized C species (i.e., aromatic and carbonyl C). Ramp CP/phase-adjusted side band suppressing (PASS) is a pulse sequence that integrates SSBs separately and quantitatively recovers them into their inherent center peaks. In the present study, the applicability of ramp CP/PASS to NOM analysis was compared with direct polarization (DPMAS), another quantitative method but one that requires a long operation time, and/or a ramp CP/total suppression side band (ramp CP/TOSS) technique, a popular but non-quantitative method for deleting SSBs. The test materials were six soil humic acid samples with various known degrees of aromaticity and two fulvic acids. There were no significant differences in the relative abundance of alkyl C, O-alkyl C, and aromatic C between the ramp CP/PASS and DPMAS methods, while the signal intensities corresponding to aromatic C in the ramp CP/TOSS spectra were consistently less than the values obtained in the ramp CP/PASS spectra. These results indicate that ramp CP/PASS can be used to accurately estimate the C composition of NOM samples.

Keywords

Solid-state 13C NMR Phase-adjusted side band suppressing (PASS) Cross polarization/magic angle spinning (CPMAS) Direct polarization (DPMAS) Carbon functional groups Humic substances 

Notes

Acknowledgments

This research was supported by a Grant-in-Aid for Scientific Research (No. 20380043) from the Japan Society for the Promotion of Science. The authors thank Dr. T. Nakai, JEOL RESONANCE, for his great support in acquiring PASS sequence and technical official, Y. Maeda, Nagoya University, for his kind support in using an NMR spectrometer ECA 700. The authors thank Dr. Z. Zhong and Dr. P. G. Hatcher, Old Dominion University, for their great support in the measurement of 13C DPMAS NMR spectra. The authors also thank two anonymous reviewers for providing critical comments and valuable suggestions.

Compliance with ethical standards

Conflict of interest

The authors declare that they have no competing interests.

References

  1. 1.
    Cook RL (2004) Coupling NMR to NOM. Anal Bioanal Chem 378:1484–1503CrossRefGoogle Scholar
  2. 2.
    Smernik RJ, Olk DC, Mahieu N (2004) Quantitative solid-state 13C NMR spectroscopy of organic matter fractions in lowland rice soils. Eur J Soil Sci 55:367–379CrossRefGoogle Scholar
  3. 3.
    Mao JD, Chen N, Cao X (2011) Characterization of humic substances by advanced solid state NMR spectroscopy: demonstration of a systematic approach. Org Geochem 42:891–902CrossRefGoogle Scholar
  4. 4.
    Cook RL, Langford C, Yamdagni R, Preston CM (1996) A modified cross-polarization magic angle spinning 13C NMR procedure for the study of humic materials. Anal Chem 68:3979–3986CrossRefGoogle Scholar
  5. 5.
    Berns AE, Conte P (2011) Effect of ramp size and sample spinning speed on CPMAS 13C NMR spectra of soil organic matter. Org Geochem 42:926–935CrossRefGoogle Scholar
  6. 6.
    Mets G, Wu X, Smith SO (1994) Ramped-amplitude cross polarization in magic-angle-spinning NMR. J Magn Reson 110:219–227CrossRefGoogle Scholar
  7. 7.
    Johnson RL, Schmidt-Rohr K (2014) Quantitative solid-state 13C NMR with signal enhancement by multiple cross polarization. J Magn Reson 239:44–49CrossRefGoogle Scholar
  8. 8.
    Dixon WT (1982) Spinning-sideband-free and spinning-sideband-only NMR spectra in spinning samples. J Chem Phys 77:1800–1809CrossRefGoogle Scholar
  9. 9.
    Antzutkin ON (1999) Sideband manipulation in magic-angle-spinning nuclear magnetic resonance. Prog Nucl Mag Res Sp 35:203–266CrossRefGoogle Scholar
  10. 10.
    Antzutkin ON, Shekar SC, Levitt MH (1995) 2-dimensional side-band separation in magic-angle-spinning NMR. J Magn Reson 115:7–19CrossRefGoogle Scholar
  11. 11.
    Kuwatsuka S, Watanabe A, Itoh K, Arai S (1992) Comparison of two methods of preparation of humic and fulvic acids, IHSS method and NAGOYA method. Soil Sci Plant Nutr 38:23–30CrossRefGoogle Scholar
  12. 12.
    Watanabe A, Itoh K, Arai S, Kuwatsuka S (1994) Comparison of the composition of humic and fulvic acids prepared by the IHSS method and NAGOYA method. Soil Sci Plant Nutr 40:601–608CrossRefGoogle Scholar
  13. 13.
    Watanabe A, Maie N, Hepburn A, McPhail D, Abe T, Ikeya K, Ishida Y, Ohtani H (2004) Chemical characterization of Japanese Humic Substances Society standard soil humic and fulvic acids by spectroscopic and degradative analyses. Humic Sub Res 1:18–28Google Scholar
  14. 14.
    Mao JD, Hu WG, Schmidt-Rohr K, Davies G, Ghabbour EA, Xing B (2000) Quantitative characterization of humic substances by solid-state carbon-13 nuclear magnetic resonance. Soil Sci Soc Am J 64:873–884CrossRefGoogle Scholar
  15. 15.
    Monteil-Rivera F, Brouwer EB, Masset S, Deslandes Y, Dumonceau J (2000) Combination of X-ray photoelectron and solid-state 13C nuclear magnetic resonance spectroscopy in the structural characterisation of humic acids. Anal Chim Acta 424:243–255CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2015

Authors and Affiliations

  1. 1.Graduate School of Bioagricultural SciencesNagoya UniversityNagoyaJapan
  2. 2.Graduate School of Environmental StudiesNagoya UniversityNagoyaJapan

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