Quantitative aspects of solid-state 13C-NMR spectra of humic substances from soils of volcanic systems

被引:77
作者
Conte, P [1 ]
Piccolo, A
Van Lagen, B
Buurman, P
de Jager, PA
机构
[1] Univ Naples Federico II, Dipartimento Sci Chim Agr, I-80055 Portici, Na, Italy
[2] Agr Univ Wageningen, Dept Soil Sci & Geol, NL-6700 AA Wageningen, Netherlands
[3] Wageningen Univ Agr, Dept Mol Phys, NL-6700 ET Wageningen, Netherlands
关键词
humic substances; CPMAS C-13-NMR; contact time; cross-polarisation; volcanic soils;
D O I
10.1016/S0016-7061(97)00058-X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Cross-Polarisation Magic Angle Spinning Carbon-13 Nuclear Magnetic Resonance spectroscopy (CPMAS C-13-NMR) represents one of the most powerful tools to investigate soil organic matter (SOM) mainly because of its inherent capacity to provide a semi-quantitative evaluation of carbon distribution. A critical parameter during acquisition of CPMAS C-13-NMR spectra is the contact time required to obtain the cross-polarisation between proton and carbon nuclei. The procedure to evaluate the best contact time for the acquisition of a quantitative CPMAS C-13-NMR spectrum is to perform Variable Contact Time (VCT) experiments. In this work the structural features of a number of purified humic substances from Italian and Costarican volcanic soils were investigated by CPMAS C-13-NMR spectroscopy after having performed preliminary VCT experiments. The VCT experiments showed that the average contact times vary according to the origin and chemical structure of the humic material. The optimal contact times (OCT) for nine humic samples were between 250 and 800 mu s. These values were different from the time of 1000 mu s that is commonly applied as the best average contact time for humic materials. Moreover, by comparing the NMR data to those obtained by elemental analysis (C/H ratio), it appeared that the efficiency of the cross-polarisation between protons and carbons, and hence the contact time, is affected not only by the number of protons, but also by their distribution over the molecules. The evaluation of errors in quantitative estimation of the different carbons revealed that the use of OCT generally reduced by half the loss of signals occurring when the average contact time of 1000 mu s is used in CPMAS C-13-NMR spectra of humic substances. (C) 1997 Elsevier Science B.V.
引用
收藏
页码:327 / 338
页数:12
相关论文
共 19 条
  • [1] CROSS POLARIZATION AND MAGIC ANGLE SAMPLE SPINNING NMR-SPECTRA OF MODEL ORGANIC-COMPOUNDS .1. HIGHLY PROTONATED MOLECULES
    ALEMANY, LB
    GRANT, DM
    PUGMIRE, RJ
    ALGER, TD
    ZILM, KW
    [J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1983, 105 (08) : 2133 - 2141
  • [2] CROSS POLARIZATION AND MAGIC ANGLE SAMPLE SPINNING NMR-SPECTRA OF MODEL ORGANIC-COMPOUNDS .2. MOLECULES OF LOW OR REMOTE PROTONATION
    ALEMANY, LB
    GRANT, DM
    PUGMIRE, RJ
    ALGER, TD
    ZILM, KW
    [J]. JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1983, 105 (08) : 2142 - 2147
  • [3] CHEMICAL-COMPOSITION OF HUMIC ACIDS - A COMPARISON WITH PRECURSOR LIGHT FRACTION LITTER FROM DIFFERENT VEGETATIONS USING SPECTROSCOPIC TECHNIQUES
    AMALFITANO, C
    QUEZADA, RA
    WILSON, MA
    HANNA, JV
    [J]. SOIL SCIENCE, 1995, 159 (06) : 391 - 401
  • [4] THE CONTRIBUTION OF LIGNIN TO THE COMPOSITION OF HUMIC ACIDS FROM A WHEAT-STRAW AMENDED SOIL DURING 3 YEARS OF INCUBATION IN POTS
    AMALFITANO, C
    PIGNALOSA, V
    AURIEMMA, L
    RAMUNNI, A
    [J]. JOURNAL OF SOIL SCIENCE, 1992, 43 (03): : 495 - 504
  • [5] [Anonymous], 1994, HUMUS CHEM GENESIS C
  • [6] [Anonymous], HUMIC SUBSTANCES TER
  • [7] ATTEMPTS TO IMPROVE SOLID-STATE C-13 NMR-SPECTRA OF WHOLE MINERAL SOILS
    ARSHAD, MA
    RIPMEESTER, JA
    SCHNITZER, M
    [J]. CANADIAN JOURNAL OF SOIL SCIENCE, 1988, 68 (03) : 593 - 602
  • [8] CHEMICAL CHARACTERISTICS OF HUMIC ACIDS FROM 5 SOILS IN KENYA
    ARSHAD, MA
    SCHNITZER, M
    [J]. ZEITSCHRIFT FUR PFLANZENERNAHRUNG UND BODENKUNDE, 1989, 152 (01): : 11 - 16
  • [9] DETERMINATION OF THE FRACTION OF ORGANIC-CARBON OBSERVABLE IN COALS AND COAL DERIVATIVES MEASURED BY HIGH-RESOLUTION SOLID-STATE C-13 NUCLEAR-MAGNETIC-RESONANCE SPECTROMETRY
    HAGAMAN, EW
    CHAMBERS, RR
    WOODY, MC
    [J]. ANALYTICAL CHEMISTRY, 1986, 58 (02) : 387 - 394
  • [10] C-13 NMR-STUDIES OF ORGANIC-MATTER IN WHOLE SOILS .1. QUANTITATION POSSIBILITIES
    KINCHESH, P
    POWLSON, DS
    RANDALL, EW
    [J]. EUROPEAN JOURNAL OF SOIL SCIENCE, 1995, 46 (01) : 125 - 137