Temporal variation in surface and subsoil abundance and function of the soil microbial community in an arable soil

被引:131
作者
Kramer, Susanne [1 ]
Marhan, Sven [1 ]
Haslwimmer, Heike [1 ]
Ruess, Liliane [2 ]
Kandeler, Ellen [1 ]
机构
[1] Univ Hohenheim, Soil Biol Sect, Inst Soil Sci & Land Evaluat, D-70599 Stuttgart, Germany
[2] Humboldt Univ, Ecol Grp, Inst Biol, D-10115 Berlin, Germany
关键词
PLFA; Enzyme activity; Specific enzyme activity; Topsoil; Subsoil; Crop effect; Litter amendment; Agricultural field; Season; ORGANIC-MATTER; ENZYME-ACTIVITIES; ECOSYSTEM RESPONSE; CARBON; BIOMASS; DEPTH; MANAGEMENT; DYNAMICS; TILLAGE; DECOMPOSITION;
D O I
10.1016/j.soilbio.2013.02.006
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Many studies of the microbial ecology of agricultural ecosystems focus on surface soils, whereas the impacts of management practice and season on soil microbial community composition and function below the plough zone are largely neglected. Deep soils have a high potential to store carbon; therefore any management driven stimulation or repression of microorganisms in subsoil could impact biogeochemical cycling in agricultural sites. The aim of this study was to understand whether soil management affects microbial communities in the topsoil (0-10 cm), rooted zone beneath the plough layer (40-50 cm), and the unrooted zone (60-70 cm). In a field experiment with different crops [wheat (Triticum aestivum L.) and maize (Zea mays L.)] and agricultural management strategies (litter amendment) we analysed microbial biomass as phospholipid fatty acids (PLFAs) and enzyme activities involved in the C-cycle (beta-glucosidase, N-acetyl-beta-D-glucosaminidase, beta-xylosidase, phenol- and peroxidase) across a depth transect over a period of two years. Wheat cultivation resulted in higher bacterial and fungal biomass as well as higher enzyme activities at most sampling dates in comparison to maize cultivated plots, and this effect was visible to 50 cm depth. Litter application increased bacterial and fungal biomass as well as hydrolytic enzyme activities but effects were apparent only in the topsoil. In winter high microbial biomass and enzyme activities were measured in all soil layers, possibly due to increased mobilization and translocation of organic matter into deeper soil. Hydrolytic enzyme activities decreased with depth, whereas oxidative enzyme activities showed no decrease or even an increase with depth. This could have been due to differing sorption mechanisms of hydrolytic and oxidative enzymes. Specific enzyme activities (enzyme activity per microbial biomass) were higher in the deeper layers and possible reasons are discussed. (C) 2013 Elsevier Ltd. All rights reserved.
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页码:76 / 85
页数:10
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