栗方亮, 李忠佩, 刘明, 江春玉. 氮素浓度和水分对水稻土硝化作用和微生物特性的影响[J]. 中国生态农业学报(中英文), 2012, 20(9): 1113-1118. DOI: 10.3724/SP.J.1011.2012.01113
引用本文: 栗方亮, 李忠佩, 刘明, 江春玉. 氮素浓度和水分对水稻土硝化作用和微生物特性的影响[J]. 中国生态农业学报(中英文), 2012, 20(9): 1113-1118. DOI: 10.3724/SP.J.1011.2012.01113
LI Fang-Liang, LI Zhong-Pei, LIU Ming, JIANG Chun-Yu. Effects of different concentrations of nitrogen and soil moistures on paddy soil nitrification and microbial characteristics[J]. Chinese Journal of Eco-Agriculture, 2012, 20(9): 1113-1118. DOI: 10.3724/SP.J.1011.2012.01113
Citation: LI Fang-Liang, LI Zhong-Pei, LIU Ming, JIANG Chun-Yu. Effects of different concentrations of nitrogen and soil moistures on paddy soil nitrification and microbial characteristics[J]. Chinese Journal of Eco-Agriculture, 2012, 20(9): 1113-1118. DOI: 10.3724/SP.J.1011.2012.01113

氮素浓度和水分对水稻土硝化作用和微生物特性的影响

Effects of different concentrations of nitrogen and soil moistures on paddy soil nitrification and microbial characteristics

  • 摘要: 为了明确不同氮素浓度和水分对土壤硝化作用和微生物特性的影响, 特别是高氮素浓度下的响应特异性, 以红壤水稻土为供试土壤, 设置4个硫铵用量水平0(CK)、120 mg(N)·kg-1(A1)、600 mg(N)·kg-1(A2)、 1 200 mg(N)·kg-1(A3), 调节土壤水分为饱和持水量(WHC)的40%、60%和80%, 研究了短期内不同氮素浓度和不同水分条件下土壤硝化作用、微生物生物量碳和微生物功能多样性的变化。结果表明: 在40%、60%和80%WHC水分条件时, 硫铵A2、A3浓度处理土壤硝化率和硝化速率普遍较低, 硫铵A1浓度处理硝化率和硝化速率随土壤含水量的升高而升高; 同含水量时随硫铵用量的升高而显著降低。在40%、60%和80%WHC水分条件时, 微生物生物量碳随硫铵浓度的升高而降低; 同浓度硫铵用量水平时, 微生物生物量碳的变化基本表现为: 60%WHC>80% WHC>40%WHC。分析发现不同水分和硫铵处理之间存在交互作用。BIOLOG分析显示: 不同氮素浓度和不同水分处理, 60%WHC下A1处理的平均吸光值(AWCD)和Shannon、Simpson、McIntosh指数最大, 其次为60%WHC的硫铵CK处理, 而不同水分下硫铵A2、A3处理, 其AWCD值和Shannon、Simpson、McIntosh多样性指数都较低, 进一步说明过量施肥导致微生物活性降低。不同氮素浓度和水分条件下土壤微生物和生化性状不同, 过量施用化肥后将有可能造成土壤微生物性状和生化功能衰减。

     

    Abstract: To make clear the effects of different concentrations of nitrogen and soil moistures on soil nitrification and microbial characteristics, especially the responses to high nitrogen concentration, nitrification, microbial biomass carbon and microbial community diversity in red paddy soils were studied under four ammonium sulfate doses 0(CK), 120 mg(N)·kg-1 (A1), 600 mg(N)·kg-1 (A2), 1 200 mg(N)·kg-1 (A3) and adjusted soil moistures of 40%, 60% and 80% of water holding capacity (WHC). Nitrification ratios and rates of A2 and A3 treatments were generally low under 40%, 60% and 80% WHC. Nitrification ratios and rates of A1 treatments significantly increased with increasing soil moisture. Nitrification significantly decreased with decreasing ammonium sulfate at constant soil moisture. Soil microbial biomass carbon reduced with increasing ammonium sulfate from 40%, 60% to 80%WHC. The trend in microbial biomass carbon at constant ammonium sulfate concentration was 60%WHC > 80%WHC > 40%WHC. No interactive effects were noted in the soil moisture and ammonium sulfate treatments. For different concentrations of nitrogen and soil moistures, BIOLOG analysis showed that AWCD value and Shannon, Simpson, McIntosh indices were highest under A1 treatment at 60%WHC, followed by CK treatment at 60%WHC. For different soil moisture, excessive fertilization led to low microbial activity. AWCD value and Shannon, Simpson, McIntosh indices were low under A2 and A3 ammonium sulfate treatments. The findings suggested different soil biological and biochemical properties under different concentrations of nitrogen and soil moistures. Overuse of chemical fertilizers did no enhance soil biological properties and biochemical function.

     

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