The contribution of soil organic matter fractions to carbon and nitrogen mineralization and microbial community size and structure

被引:229
作者
Cookson, WR
Abaye, DA
Marschner, P
Murphy, DV
Stockdale, EA
Goulding, KWT
机构
[1] Univ Western Australia, Sch Earth & Geog Sci, Fac Nat & Agr Sci, Ctr Land Rehabil, Crawley, WA 6009, Australia
[2] Rothamsted Res, Agr & Environm, Harpenden AL5 2JQ, Herts, England
[3] Univ Adelaide, Sch Earth & Environm Sci, Fac Sci, Soil & Land Syst, Glen Osmond, SA 5064, Australia
基金
英国生物技术与生命科学研究理事会;
关键词
PLFA; N-15 pool dilution; hay and fertilizer application; N mineralization; N immobilization; nitrification; community structure; dissolved organic matter;
D O I
10.1016/j.soilbio.2005.02.007
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The aims of this study were to: (i) assess the impact of hay and fertilizer application on organic matter (OM) fractions (dissolved organic matter (DOM), light fraction organic matter (LFOM, < 1.0 g cm(-3)), heavy fraction OM (HFOM, < 1.7 g cm(-3))), carbon (C) and nitrogen (N) cycling processes and microbial community size and structure, and (ii) quantify the role of OM fractions to C and N cycling. Soil was collected in 2001 from a field experiment to which grass hay (1996) and/or fertilizer (1995 and 1999) had previously been applied. DOM-C (P < 0.05) and DOM-N (P = 0.07) were significantly higher in control and fertilized soil than hay and hay + fertilized soil. LFOM and HFOM C and N contents and C/N ratios were significantly (P < 0.05) higher in hay + fertilized and hay amended soil than in control and fertilized soil. Potentially mineralizable-N (PMN), microbial biomass-C (MB-C), microbial biomass-N (MB-N) and microbial respiration (CO2) were not affected by fertilizer and/or hay application. Gross N mineralization (Gross Min) and gross nitrification (Gross Nit) rates were significantly (P < 0.05) higher in fertilized, hay, hay + fertilized soil than control soil. However, there was no significant difference between treatments in gross N immobilization rates. Results reported here highlight the importance of a labile fraction of the DOM pool to N and C cycling as its removal significantly (P < 0.05) reduced PMN, MB-N, Gross Min and Gross Nit compared with whole soil in most or all treatments. In soil where DOM + LFOM were removed PMN was significantly (P < 0.05) lower, but MB-C, Gross Min and Gross Nit was significantly (P < 0.05) higher than in DOM removed soil. This suggests that LFOM plays an important role as a sink for mineral-N. Total soil phospholipid fatty acid (PLFA) concentration was significantly (P < 0.05) higher in hay amended than control, fertilized and hay + fertilized soil. Principal components analysis was able to clearly discriminate between control, fertilized, hay + fertilized and hay amended soil. Soil amended with hay or fertilizer had a microbial community structure which differed from that of the control or hay + fertilized soils. Redundancy analysis with Monte Carlo permutation tests revealed that PLFA profiles were strongly correlated to differences in Gross Min, Gross Nit, MB-N, MB-C, MB-C/N ratio, total soil C and total soil C/N ratio. The results of this research suggest that changes in microbial structure are related to aspects of soil C and N pools and cycling. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1726 / 1737
页数:12
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