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水热条件与土壤性质对农田土壤硝化作用的影响
摘要点击 3089  全文点击 1326  投稿时间:2008-01-25  修订日期:2008-03-25
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中文关键词  土壤硝化作用强度  硝化细菌  土壤类型  气温  降雨  交互作用  土壤置换试验
英文关键词  soil nitrification  nitrobacteria  soil type  temperature  rainfall  interaction  soil transplantation experiment
作者单位
孙波 中国科学院南京土壤研究所南京210008 
郑宪清 中国科学院南京土壤研究所南京210008 
胡锋 南京农业大学资源与环境科学学院南京210095 
李辉信 南京农业大学资源与环境科学学院南京210095 
孔滨 中国科学院南京土壤研究所南京210008 
王帘里 中国科学院南京土壤研究所南京210008 
隋跃宇 中国科学院东北地理与农业生态研究所哈尔滨150040 
中文摘要
      水热条件、土壤性质和耕作管理影响了土壤的硝化作用从而影响农田氮素循环和平衡.本试验选择中国东部3个气候带上的主要农田土壤:中温带黑龙江海伦的黑土、暖温带河南封丘的潮土和中亚热带江西鹰潭的红壤,在上述3个地点的生态试验站建立土壤置换试验,对比研究不同水热条件和土壤类型对玉米单作系统中土壤硝化作用的交互影响.2006~2007年的试验结果表明,在玉米抽雄期,从海伦到鹰潭(月均温由22.3℃上升到26.8℃,月降水由100.8 mm增加到199.6 mm),3种土壤的硝化作用强度均随着月均温和月降水的增加而下降,黑土、潮土和红壤分别下降了64.2%~67.2%、 52.1%~52.5%和41.7%~75.2%,土壤的硝化作用强度与气温(r=-0.354,p<0.01)和降水(r=-0.290,p<0.01)均呈极显著负相关.土壤类型也显著影响了土壤硝化细菌的数量和硝化强度,硝化细菌数和硝化强度的大小顺序为:潮土> 黑土> 红壤.土壤pH对土壤硝化强度有显著影响,其相关系数r=0.551(p<0.01).总体上,在玉米抽雄期,区域水热状况及土壤类型、施肥均影响了土壤的硝化强度,水热×土壤类型、水热×施肥、土壤类型×施肥、水热×土壤类型×施肥等对硝化强度有着极显著的交互作用.
英文摘要
      Climate conditions, soil properties and management practices control soil nitrification process which affects nitrogen cycling and balance in agro-ecosystems. The interaction of temperature, rainfall, soil type and fertilization on the soil nitrification process was studied by a soil transplantation experiment installed in 3 experiment stations of Chinese Ecological Research Network, i.e. Hailun, Fenqiu and Yingtan Agroecological Experiment Station, which represents middle temperature, warm temperature and middle subtropical zone, respectively. Three types of cropland soils were selected, i.e. neutral black soil (Phaeozem), alkaline Chao soil (Cambisol) and acidic red soil (Acrisol). Then one-meter depth soil profiles for each soil were transplanted in 3 stations to build the field experiment. The two-year experimental results (2006-2007) showed soil nitrification intensity (SNI) changed with the temperature and rainfall during the maize tasseling stage. From Hailun to Yingtan, with an increase of monthly average temperature from 22.3℃ to 26.8℃ and the monthly rainfall from 100.8 mm to 199.6 mm, SNI decreased by 64.2%-67.2% for black soil, 52.1%-52.5% for Chao soil, and 41.7%-75.2% for red soil, respectively. There were significant negative correlations between SNI and temperature and rainfall, with a correlation coefficient of r=-0.354 (p<0.01) and r=-0.290 (p<0.01), respectively. The total number of soil nitrobacteria and the intensity of soil nitrification was affected by soil types, which increased in a sequence of Chao soil > black soil > red soil. Among soil properties, pH affected SNI significantly, with a correlation coefficient of r=0.551 (p<0.01). In generally, climate condition (temperature and rainfall), soil type and fertilization present an integrated impact on soil nitrification process, and there were significant interactions of climate×soil type, climate×fertilization, soil type×fertilization, and climate×soil type×fertilization.

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