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长期定位有机物料还田对关中平原冬小麦-玉米轮作土壤N2O排放的影响
摘要点击 3256  全文点击 1065  投稿时间:2016-09-30  修订日期:2016-12-27
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中文关键词  N2O排放  秸秆还田  牛粪  直接排放系数  长期定位施肥  单位产量N2O排放量
英文关键词  N2 O emission  straw retention  cattle waste  direct emission factor  long-term fertilization  yield-scaled N2 O emission
作者单位E-mail
郝耀旭 西北农林科技大学资源环境学院, 杨凌 712100 haoyaoxu912@163.com 
刘继璇 西北农林科技大学资源环境学院, 杨凌 712100  
袁梦轩 西北农林科技大学资源环境学院, 杨凌 712100  
周应田 西北农林科技大学资源环境学院, 杨凌 712100  
杨学云 西北农林科技大学资源环境学院, 杨凌 712100  
顾江新 西北农林科技大学资源环境学院, 杨凌 712100 gujiangxin@nwsuaf.edu.cn 
中文摘要
      为定量研究有机物料还田对农田土壤N2O排放的影响,采用静态暗箱-气相色谱法对关中平原冬小麦-玉米轮作24 a长期定位施肥试验地土壤N2O排放速率和相关环境因子进行了周年观测,试验处理为对照(CK,0 kg·hm-2)、氮磷钾(NPK,353 kg·hm-2)、氮磷钾加秸秆还田[NPKS,(353+40)kg·hm-2]和氮磷钾加牛粪[NPKM,(238+115)kg·hm-2]4个处理.结果表明观测期内,CK处理N2O排放速率较小[<2.9 g·(hm2·d)-1];施肥处理在冬小麦季施肥和玉米季灌溉后均出现排放峰,最高值分别为NPKS[113.4 g·(hm2·d)-1]和NPKM[495.0 g·(hm2·d)-1]处理.各处理N2O排放通量与土壤湿度均呈显著正相关关系(r>0.28,P<0.05).CK、NPK、NPKS和NPKM处理N2O年排放总量分别为(0.1±0.0)、(2.6±0.1)、(3.4±0.7)和(2.9±0.3)kg·hm-2,施肥处理排放总量显著高于CK处理(P<0.05),但施肥处理之间差异不显著(P=0.06),说明施肥促进了N2O排放,但有机物料还田未能显著增加N2O排放.各施肥处理N2O直接排放系数分别为0.72%、0.83%和0.80%,均低于IPCC缺省值1%.施肥处理中,NPKM处理的单位产量N2O排放量最低.
英文摘要
      The primary aim of this study was to quantify the effects of long-term organic amendments on soil nitrous oxide (N2O) emissions. Using static chamber-gas chromatograph technique, we measured N2O fluxes from winter wheat-maize rotation system and related environmental factors in the Guanzhong Plain for one year (October 2014 to October 2015). Field experiments were based on the "Chinese National Loess Fertility and Fertilizer Effects Long-term Monitoring Experiment". Four treatments were control (CK, 0 kg·hm-2), NPK (NPK, 353 kg·hm-2), NPK combined with maize straw[NPKS, (353+40) kg·hm-2] and cattle waste[NPKM, (238+115) kg·hm-2]. During the experimental period, N2O fluxes from CK treatment were small[<2.9 g·(hm2·d)-1]; while emissions from fertilized treatments peaked after fertilization[up to 113.4 g·(hm2·d)-1 for NPKS] and irrigation[up to 495.0 g·(hm2·d)-1 for NPKM] during winter wheat and maize seasons, respectively. N2O flux was significantly correlated to soil water-filled pore space for all treatments (r>0.28,P<0.05). Annual N2O emissions were (0.1±0.0), (2.6±0.1), (3.4±0.7) and (2.9±0.3) kg·hm-2 for CK, NPK, NPKS and NPKM, respectively. The fertilized treatments released higher N2O emissions than CK treatment (P<0.05), indicating that fertilization stimulated N2O emissions. However, the differences in N2O emissions were not significant among the fertilized treatments (P=0.06), suggesting that organic amendments did not increase N2O emissions obviously. The direct emission factors were 0.72%, 0.83% and 0.80% for NPK, NPKS and NPKM, respectively, all of which were lower than the IPCC default of 1%. The yield-scaled N2O emission for NPKM was the lowest among the fertilized treatments.

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