Monitoring biomacromolecular degradation of Calluna vulgaris in a 23 year field experiment using solid state 13C-NMR and pyrolysis-GC/MS

被引:63
作者
Huang, Y
Stankiewicz, BA
Eglinton, G
Snape, CE
Evans, B
Latter, PM
Ineson, P
机构
[1] Univ Bristol, Dept Geol, Biogeochem Res Ctr, Bristol BS8 1RJ, Avon, England
[2] Univ Bristol, Sch Chem, Environm & Analyt Chem Sect, Bristol BS8 1TS, Avon, England
[3] Univ Strathclyde, Dept Pure & Appl Chem, Glasgow G1 1XL, Lanark, Scotland
[4] Inst Terr Ecol, Merlewood Res Stn, Grange Sands LA11 6JU, Cumbria, England
基金
英国自然环境研究理事会;
关键词
D O I
10.1016/S0038-0717(97)00234-4
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The qualitative and quantitative changes in lignin, polysaccharide, aliphatic, cutin and protein biomacromolecules in Calluna vulgaris shoots collected at three intervals (initial 0.5 y, 7 y and 23 y) in a field decomposition experiment have been investigated using quantitative solid slate C-13 nuclear magnetic resonance (NMR) spectroscopy and pyrolysis-gas chromatography/mass spectrometry (Py-GC/MS). Protein showed rapid decomposition with virtually none remaining after 7 y. The absolute weight losses of the other macromolecules after 23 y in the field show the sequence: polysaccharides > aliphatics/cutin > lignin. However, relative decomposition rates varied significantly during each interval, with polysaccharides and aliphatic/cutin being the highest in the first and second intervals, respectively, and polysaccharides being the lowest in the final interval. Py-GC/MS provided evidence that part of the remaining polysaccharides in the 23 y decomposed litter can be attributed to microbial production. Degradation of lignin is shown as progressive oxidation of alcoholic functions into the corresponding ketones or aldehydes and preferential degradation of syringyl over guaiacyl moieties. An unusual preferential removal of p-coumaric acid units over syringyl and guaiacyl units was observed, probably due to selective hydrolysis of its ester bond with lignin moieties either enzymatically by specific microorganisms or chemically. The specific soil environment with its low temperature, high rainfall and high acidity appears to limit microbial activities and leads to accumulation of carbon below ground. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:1517 / 1528
页数:12
相关论文
共 38 条
[1]  
ANDERSON JM, 1992, ADV ECOL RES, V22, P163, DOI 10.1016/S0065-2504(08)60136-1
[2]  
Boon J. J., 1989, Physico-chemical characterisation of plant residues for feed use., P25
[3]  
Boon J. J., 1986, Peat and Water. Aspects of Water Retention and Dewatering in Peat, P215
[4]   STRUCTURAL STUDIES ON CELLULOSE PYROLYSIS AND CELLULOSE CHARS BY PYMS, PYGCMS, FTIR, NMR AND BY WET CHEMICAL TECHNIQUES [J].
BOON, JJ ;
PASTOROVA, I ;
BOTTO, RE ;
ARISZ, PW .
BIOMASS & BIOENERGY, 1994, 7 (1-6) :25-32
[5]   PYROLYSIS MASS-SPECTROMETRY OF SOME SCIRPUS SPECIES AND THEIR DECOMPOSITION PRODUCTS [J].
BOON, JJ ;
WETZEL, RG ;
GODSHALK, GL .
LIMNOLOGY AND OCEANOGRAPHY, 1982, 27 (05) :839-848
[6]  
Cadisch G., 1997, Driven by nature. Plant litter quality and decomposition
[7]  
EWBANK G, 1993, ORGANIC GEOCHMISTRY, P519
[8]   SOLID-STATE C-13 NMR-STUDY OF PALM TRUNK CELL-WALLS [J].
GALLACHER, J ;
SNAPE, CE ;
HASSAN, K ;
JARVIS, MC .
JOURNAL OF THE SCIENCE OF FOOD AND AGRICULTURE, 1994, 64 (04) :487-491
[9]  
Galletti G.C., 1991, PREPRINTS AM CHEM SO, V36, P691
[10]  
HASLAM E, 1989, VEGETABLE TANNINS RE