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长期施肥对中国东北棕壤土壤微生物生物量、脱氢酶活性以及细菌和真菌群落结构的影响

Influence of long-term fertilization on soil microbial biomass, dehydrogenase activity, and bacterial and fungal community structure in a brown soil of northeast China.

作者信息

Luo Peiyu, Han Xiaori, Wang Yan, Han Mei, Shi Hui, Liu Ning, Bai Hongzhi

机构信息

College of Land and Environment, Shenyang Agricultural University, Dongling Road 120, Shenyang, 110866 Liaoning China ; National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources, Dongling Road 120, Shenyang, 110866 Liaoning China.

Foreign Language Teaching Department, Shenyang Agricultural University, Dongling Road 120, Shenyang, 110866 Liaoning China.

出版信息

Ann Microbiol. 2015;65(1):533-542. doi: 10.1007/s13213-014-0889-9. Epub 2014 Apr 22.

DOI:10.1007/s13213-014-0889-9
PMID:25705148
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC4331610/
Abstract

In this study, the effect of mineral fertilizer and organic manure were evaluated on soil microbial biomass, dehydrogenase activity, bacterial and fungal community structure in a long-term (33 years) field experiment. Except for the mineral nitrogen fertilizer (N) treatment, long-term fertilization greatly increased soil microbial biomass carbon (SMBC) and dehydrogenase activity. Organic manure had a significantly greater impact on SMBC and dehydrogenase activity, compared with mineral fertilizers. Bacterial and fungal community structure was analyzed by polymerase chain reaction (PCR)-denaturing gradient gel electrophoresis (DGGE). Long-term fertilization increased bacterial and fungal ribotype diversity. Total soil nitrogen (TN) and phosphorus (TP), soil organic carbon (SOC) and available phosphorus (AP) had a similar level of influence on bacterial ribotypes while TN, SOC and AP had a larger influence than alkali-hydrolyzable nitrogen (AHN) on fungal ribotypes. Our results suggested that long-term P-deficiency fertilization can significantly decrease soil microbial biomass, dehydrogenase activity and bacterial diversity. N-fertilizer and SOC have an important influence on bacterial and fungal communities.

摘要

在本研究中,通过一项长期(33年)田间试验,评估了矿物肥料和有机肥对土壤微生物生物量、脱氢酶活性、细菌和真菌群落结构的影响。除矿物氮肥(N)处理外,长期施肥显著增加了土壤微生物生物量碳(SMBC)和脱氢酶活性。与矿物肥料相比,有机肥对SMBC和脱氢酶活性的影响显著更大。采用聚合酶链反应(PCR)-变性梯度凝胶电泳(DGGE)分析细菌和真菌群落结构。长期施肥增加了细菌和真菌核糖型多样性。土壤全氮(TN)和全磷(TP)、土壤有机碳(SOC)和有效磷(AP)对细菌核糖型的影响程度相似,而TN、SOC和AP对真菌核糖型的影响大于碱解氮(AHN)。我们的结果表明,长期缺磷施肥会显著降低土壤微生物生物量、脱氢酶活性和细菌多样性。氮肥和SOC对细菌和真菌群落有重要影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/fdff7c800a2b/13213_2014_889_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/13e36c1eaaaa/13213_2014_889_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/c3e1d342297f/13213_2014_889_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/4b303634bcce/13213_2014_889_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/c1962d438913/13213_2014_889_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/fdff7c800a2b/13213_2014_889_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/13e36c1eaaaa/13213_2014_889_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/c3e1d342297f/13213_2014_889_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/4b303634bcce/13213_2014_889_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/c1962d438913/13213_2014_889_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a490/4331610/fdff7c800a2b/13213_2014_889_Fig5_HTML.jpg

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