The macromolecular organic composition of plant and microbial residues as inputs to soil organic matter

被引:1498
作者
Kögel-Knabner, I [1 ]
机构
[1] Tech Univ Munich, Wissensch Zentrum Weihenstephan Ernahrung Landnut, Lehrstuhl Bodenkunde, Dept Okol, D-85350 Freising Weihenstephan, Germany
关键词
litter; polysaccharides; lignin; lipids; biopolymers; nuclear magnetic resonance; plant residues; microbial residues; soil organic matter;
D O I
10.1016/S0038-0717(01)00158-4
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Plant litter and the microbial biomass are the major parent materials for soil organic matter (SOM) formation. Plant litter is composed of complex mixtures of organic components, mainly polysaccharides and lignin, but also aliphatic biopolymers and tannins. The composition and relative abundance of these components vary widely among plant species and tissue type. Whereas some components, such as lignin, are exclusively found in plant residues, specific products are formed by microorganisms, e.g. amino sugars. A wide variety of chemical methods is available for characterizing the chemical composition of these materials, especially the chemolytic methods, which determine individual degradation products and solid-state C-13 NMR spectroscopy, that gives an overview of the total organic chemical composition of the litter material. With the development of these techniques, an increasing number of studies are being carried out to investigate the changes during decay and the formation of humic substances. An overview is given on the amount of litter input, the proportion of various plant parts and their distribution (below-ground/above-ground), as well as the relative proportion of the different plant tissues. Major emphasis is on the organic chemical composition of the parent material for SOM formation and thus this paper provides information that will help to identify the changes occurring during biodegradation of plant litter in soils. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:139 / 162
页数:24
相关论文
共 124 条
[1]   LIGNIN CHEMISTRY - PAST, PRESENT AND FUTURE [J].
ADLER, E .
WOOD SCIENCE AND TECHNOLOGY, 1977, 11 (03) :169-218
[3]   Artifactual origin of mycobacterial bacteran. Formation of melanoidin-like artifact macromolecular material during the usual isolation process [J].
Allard, B ;
Templier, J ;
Largeau, C .
ORGANIC GEOCHEMISTRY, 1997, 26 (11-12) :691-703
[4]   Structure and origin of insoluble and non-hydrolyzable, aliphatic organic matter in a forest soil [J].
Augris, N ;
Balesdent, J ;
Mariotti, A ;
Derenne, S ;
Largeau, C .
ORGANIC GEOCHEMISTRY, 1998, 28 (1-2) :119-124
[5]   Assessing the extent of decomposition of natural organic materials using solid-state C-13 NMR spectroscopy [J].
Baldock, JA ;
Oades, JM ;
Nelson, PN ;
Skene, TM ;
Golchin, A ;
Clarke, P .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1997, 35 (05) :1061-1083
[6]   SOLID-STATE CP/MAS C-13 NMR ANALYSIS OF BACTERIAL AND FUNGAL CULTURES ISOLATED FROM A SOIL INCUBATED WITH GLUCOSE [J].
BALDOCK, JA ;
OADES, JM ;
VASSALLO, AM ;
WILSON, MA .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1990, 28 (02) :213-225
[7]   BIOSYNTHESIS AND FUNCTIONS OF FUNGAL MELANINS [J].
BELL, AA ;
WHEELER, MH .
ANNUAL REVIEW OF PHYTOPATHOLOGY, 1986, 24 :411-451
[8]   Litter decomposition and organic matter turnover in northern forest soils [J].
Berg, B .
FOREST ECOLOGY AND MANAGEMENT, 2000, 133 (1-2) :13-22
[9]   The macromolecular aromatic domain in suberized tissue: A changing paradigm [J].
Bernards, MA ;
Lewis, NG .
PHYTOCHEMISTRY, 1998, 47 (06) :915-+
[10]   MICROMORPHOLOGICAL, WET-CHEMICAL AND C-13 NMR SPECTROSCOPIC CHARACTERIZATION OF DENSITY FRACTIONATED FOREST SOILS [J].
BEUDERT, G ;
KOGELKNABNER, I ;
ZECH, W .
SCIENCE OF THE TOTAL ENVIRONMENT, 1989, 81-2 :401-408