C-13-NMR SPECTRA AND CONTACT TIME EXPERIMENT FOR SKJERVATJERN FULVIC AND HUMIC ACIDS

被引:21
作者
MALCOLM, RL
机构
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D O I
10.1016/0160-4120(92)90028-3
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The T(CP) and T1p time constants for Skjervatjern fulvic and humic acids were determined to be short with T(CP) values ranging from 0.14 ms to 0.53 ms and T1p values ranging from 3.3 ms to 5.9 ms. T(CP) or T1p time constants at a contact time of 1 ms are favorable for quantification of C-13-NMR spectra. Because of the short T(CP) values, correction factors for signal intensity for various regions of the C-13-NMR spectra would be necessary at contact times greater than 1.1 ms or less than 0.9 ms. T(CP) and T1p values have a limited non-homogeneity within Skjervatjern fulvic and humic acids. A pulse delay or repeat time of 700 ms is more than adequate for quantification of these C-13-NMR spectra. Paramagnetic effects in these humic substances are precluded due to low inorganic ash contents, low contents of Fe, Mn, and Co, and low organic free-radical contents. The observed T(CP) values suggest that all the carbon types in Skjervatjern fulvic and humic acids are fully cross-polarized before significant proton relaxation occurs. The C-13-NMR spectra for Skjervatjern fulvic acid is similar to most aquatic fulvic acids as it is predominantly aliphatic, low in aromaticity (fa1 = 24), low in phenolic content, high in carboxyl content, and has no resolution of a methoxyl peak. The C-13-NMR spectra for Skjervatjern humic acid is also similar to most other aquatic humic acids in that it is also predominantly aliphatic, high in aromaticity (fa1 = 38), moderate in phenolic content, moderate in carboxyl content, and has a clear resolution of a methoxyl carbon region. After the consideration of the necessary C-13-NMR experimental conditions, these spectra are considered to be quantitative. With careful consideration of the previously determined C-13-NMR experimental conditions, quantitative spectra can be obtained for humic substances in the future from the HUMEX site. Possible changes in humic substances due to acidification should be determined from C-13-NMR data.
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页码:609 / 620
页数:12
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[1]  
Earl, NMR of humic substances and coal, NMR of humic substances in coal, pp. 167-187, (1987)
[2]  
Gillam, Wilson, Structural analysis of aquatic humic substances by NMR spectroscopy, American Chemical Society symposium series, no. 305 on organic marine geochemistry, pp. 128-141, (1986)
[3]  
Hatcher, Wilson, The effect of sample hydration on <sup>13</sup>C CPMAS NMR spectra of fulvic acids, Org. Geochem., 17, pp. 293-299, (1991)
[4]  
Malcolm, Evaluation of humic substances from Spodosols, Proc. fifth international soil correlation meeting (ISCOM), characterization, classification, and utilization of Spodosols in Main, Massachusetts, New Hampshire, New York, Vermont, and New Brunswick, pp. 200-210, (1990)
[5]  
Malcolm, Variations among humic substances from soils, stream waters, and ground waters, Humic substances in soils and agronomy, pp. 13-35, (1990)
[6]  
Malcolm, Factors to be considered in the isolation and characterization of aquatic humic substances, Humic substances in the aquatic and terrestrial environment, pp. 369-391, (1991)
[7]  
Senesi, Application of electron spin resonance (ESR) spectroscopy in soil chemistry, Adv. Soil Sci., 14, pp. 77-130, (1990)
[8]  
Vassallo, C NMR measurements of humic substances. An examination of factors affecting their reliable interpretation, pp. 211-223, (1987)
[9]  
Wilson, NMR techniques and applications in geochemistry and soil chemistry, (1987)
[10]  
Wilson, Pugmire, Grant, Nuclear magnetic resonance spectroscopy of soils and related materials. Relaxation of <sup>13</sup>C nuclei in cross-polarization nuclear magnetic response experiments, Org. Geochem., 5, pp. 121-129, (1983)