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施氮水平对黄土旱塬区麦田土壤呼吸变化的影响
摘要点击 1874  全文点击 1910  投稿时间:2009-04-01  修订日期:2009-07-29
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中文关键词  施氮水平  土壤呼吸速率  土壤可溶性碳  微生物量碳  土壤碳氮比
英文关键词  nitrogen rates  soil respiration rate  soil dissolved organic carbon (DOC)  soil microbial biomass carbon (MBC)  C/N ratio
作者单位
高会议 中国科学院合肥智能机械研究所合肥230031 
郭胜利 西北农林科技大学资源环境学院杨凌712100 
刘文兆 西北农林科技大学资源环境学院杨凌712100 
车升国 西北农林科技大学资源环境学院杨凌712100 
中文摘要
      为评价土壤呼吸对施氮的响应,于2008年3月~2009年3月,监测了黄土旱塬区长期不同施氮水平条件下小麦连作系统中土壤呼吸日变化、季节变化以及不同生育期土壤可溶性碳(dissolved organic C,DOC)、微生物量碳(soil microbial biomass C,MBC)、土壤有机碳(soil organic C,SOC)和土壤全氮(soil total N,STN)的含量变化.研究涉及5个施氮水平(以N计)0(N0)、45(N45)、90(N
英文摘要
      To evaluate effects of nitrogen rates on soil respiration,we measured the diurnal and seasonal dynamic changes and the contents of the soil organic carbon (SOC),soil dissolved organic carbon (DOC),soil microbial biomass carbon (MBC),and total soil nitrogen (TSN) under different growing seasons of winter wheat under the continuous systems from March in 2008 to March in 2009 at Changwu ecological station of the Chinese Academy of Sciences. The experiment consists of five nitrogen rates: 0 (N0),45 (N45),90 (N90),135 (N135),and 180 (N180) kg/hm2. Soil respiration rate significantly enhanced with increasing nitrogen rate ranging from 0 to 90 kg/hm2 and increased little from 90 to 135 kg/hm2,but decreased with increasing nitrogen rate from 135 to 180 kg/hm2. At the seasonal change scale,there were an active phase of soil respiration from March to October and a weak phase of soil respiration from November to February. At the annual change scale,the fluctuate range of the treatments N0,N45,N90,N135,and N180 were 0.27-2.01 μmol/(m2·s),0.36-2.26 μmol/(m2·s) 0.58-2.56 μmol/(m2·s),0.65-2.94 μmol/(m2·s),and 0.58-2.6 μmol/(m2·s),respectively. Nitrogen fertilization significantly affected the dynamic changes of DOC and MBC. There were significant positive correlations between soil respiration rate and DOC and MBC,while significant negative correlations with the C/N ratio.

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