Contribution of primary organic matter to the fatty acid pool in agricultural soils

被引:73
作者
Jandl, G
Leinweber, P
Schulten, HR
Ekschmitt, K
机构
[1] Univ Rostock, Inst Land Use, D-18051 Rostock, Germany
[2] Univ Giessen, Dept Anim Ecol, Inst Zool, D-35390 Giessen, Germany
关键词
fatty acids; farmyard manure; plant material; soil organisms; decomposition;
D O I
10.1016/j.soilbio.2004.10.018
中图分类号
S15 [土壤学];
学科分类号
0903 [农业资源与环境]; 090301 [土壤学];
摘要
Fatty acids as major compounds of soil lipids may affect many soil properties, but the input and turnover rates in soil are largely unknown. The objective of this study was to identify and quantify fatty acids in soils as a result of input from primary sources such as plant residues, farmyard manure and soil organisms, and to evaluate the corresponding turnover- and stabilization processes. The concentrations of n-C-10:0 to n-C-34:0 fatty acids were determined in the Ap horizon of a Phaeozem with long-term cropping of rye and maize and the treatments 'Unfertilized' ('U') and fertilized with 'Farmyard manure' ('FYM'). The most important primary sources of fatty acids such as rye and maize stubble and roots, soil micro- and mesofauna, and the applied FYM were also investigated. The quantification of fatty acids by gas chromatography/mass spectrometry (GC/MS) showed that long-term FYM application led to larger concentrations of n-alkyl fatty acids in the plots grown with rye ('U': 48.1 mu g g(-1), 'FYM': 57.7 mu g g(-1), **P <= 0.01, n = 3) and maize ('U': 17.0 mu g g(-1), 'FYM': 23.4 mu g g(-1), ***P <= 0.001, n=3). The observed bimodal fatty acid distribution in soils from n-C-10:0 to n-C-21:0 and from n-C-21:0 to n-C-34:0 with a predominance at n-C-16:0 and at n-C-28:0 was apparently due to input from crop residues, soil organisms and FYM. The short-chain lengths may have originated from the investigated primary sources. The major contributors to the long-chain lengths, with a maximum at n-C-28:0, were rye stubble and FYM. A change in mono-culture from rye to maize, 38 years prior to sampling, led to a decrease in fatty acid concentrations by factors of about 2.8 ('U') and 2.5 ('FYM'). Therefore, rye-derived fatty acids and soil tillage had a larger impact on fatty acid pools than the input of primary organic matter. The changes in fatty acid distributions and pools under the consideration of the quantified input of primary organic matter led to the conclusion that the short-chained fatty acids were more rapidly decomposed than the long-chains. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1033 / 1041
页数:9
相关论文
共 35 条
[1]
Ambles A, 1998, AGROCHIMICA, V42, P158
[2]
[Anonymous], ARCH AGRON SOIL SCI
[3]
BRADY NC, 1990, NATURE PROPERTIES
[4]
Organic geochemical studies of soils from the Rothamsted Classical Experiments - II, Soils from the Hoosfield Spring Barley Experiment treated with different quantities of manure [J].
Bull, ID ;
Van Bergen, PF ;
Poulton, PR ;
Evershed, RP .
ORGANIC GEOCHEMISTRY, 1998, 28 (1-2) :11-26
[5]
Fatty acid composition and dynamics of selected fungal-feeding nematodes and fungi [J].
Chen, J ;
Ferris, H ;
Scow, KM ;
Graham, KJ .
COMPARATIVE BIOCHEMISTRY AND PHYSIOLOGY B-BIOCHEMISTRY & MOLECULAR BIOLOGY, 2001, 130 (02) :135-144
[6]
Cobb NA., 1918, AGR TECH CIR US DEP, V1, P48
[7]
A review of some important families of refractory macromolecules: Composition, origin, and fate in soils and sediments [J].
Derenne, S ;
Largeau, C .
SOIL SCIENCE, 2001, 166 (11) :833-847
[8]
Dinel H., 1990, Soil biochemistry. Volume 6., P397
[9]
Changes in soil microbial community structure with tillage under long-term wheat-fallow management [J].
Drijber, RA ;
Doran, JW ;
Parkhurst, AM ;
Lyon, DJ .
SOIL BIOLOGY & BIOCHEMISTRY, 2000, 32 (10) :1419-1430
[10]
Dunger W., 1997, METHODEN BODENBIOLOG