文章摘要
杜世宇,薛飞,吴汉卿,邹洪涛,张玉玲,张玉龙,虞娜.水氮耦合对设施土壤温室气体排放的影响[J].农业环境科学学报,2019,38(2):476-484.
水氮耦合对设施土壤温室气体排放的影响
Interactive effect of irrigation and nitrogen fertilization on greenhouse gas emissions from greenhouse soil
投稿时间:2018-03-28  修订日期:2018-07-20
DOI:10.11654/jaes.2018-0408
中文关键词: 水氮耦合  设施土壤  温室气体  全球增温潜势
英文关键词: interactive effect of irrigation and nitrogen application  greenhouse soil  greenhouse gas emissions  global warming potential
基金项目:国家自然科学基金项目(41401322);国家重点研发计划项目(2016YFD0300807);国家科技支撑计划项目(2015BAD23B01);农业农村部东北耕地保育重点实验室开放基金项目(2015NYBKFT-01)
作者单位E-mail
杜世宇 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866  
薛飞 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866  
吴汉卿 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866  
邹洪涛 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866  
张玉玲 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866  
张玉龙 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866  
虞娜 沈阳农业大学土地与环境学院/农业农村部东北耕地保育重点实验室/土肥资源高效利用国家工程实验室, 沈阳 110866 sausoilyn@163.com 
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中文摘要:
      为探究水氮耦合对设施土壤温室气体排放的影响,基于连续5年的设施番茄水氮调控定位试验,比较分析了水氮耦合对土壤N2O、CO2和CH4排放通量和累积排放量的影响,并估算了温室气体的全球增温潜势(GWP)和温室气体排放强度(GHGI)的差异。田间小区试验设置不同灌水下限(W1:25 kPa、W2:35 kPa、W3:45 kPa)和施氮量(N1:75 kg N·hm-2、N2:300 kg N·hm-2、N3:525kg N·hm-2)组合共9个处理。结果表明:设施土壤N2O和CO2排放通量受灌水施肥时期的影响,施肥后N2O排放通量呈增加趋势,高灌水量(低灌水下限25 kPa)促进N2O和CO2排放。CH4的排放通量表现为中等和强变异的特点。除水氮交互对CO2累积排放总量和施氮量对CH4累积排放总量影响不显著外,灌水下限、施氮量和水氮交互作用对N2O、CO2、CH4累积排放总量、GWPGHGI和番茄产量的影响显著或极显著。随氮肥用量的增加,N2O累积排放总量增加。N2O和CO2累积排放总量与GWP之间均达到极显著正相关,且各处理N2O对GWP平均贡献率为5.25%,CO2为94.59%。适当减少氮肥用量和增加灌水下限能够有效地降低温室气体排放和减缓全球变暖。W2N1处理是本研究中减缓温室气体排放并提高番茄产量的最佳水氮管理措施。
英文摘要:
      This study conducted an experiment on greenhouse grown tomatoes to explore the interactive effect of irrigation and nitrogen application on the level of greenhouse gas emissions released from greenhouse soil, and to determine the impact of this effect on emission flux and total cumulative emission of greenhouse gases (N2O, CO2 and CH4). Furthermore, this study examined differences in global warming potential (GWP)and greenhouse gas intensity (GHGI)between the gases over a five-year experimental period. Nine treatments, comprised of a combination of three irrigation lower limits (W1:25 kPa, W2:35 kPa, W3:45 kPa)and three N application rates (N1:75 kg N·hm-2, N2:300 kg N·hm-2, N3:525 kg N·hm-2), were utilized in the experiment. Results showed that the effects of irrigation and fertilization time influenced the emission fluxes of N2O and CO2. N2O emission flux increased after fertilization, and the high irrigation rate (irrigation lower limit 25 kPa)raised the emission fluxes of both N2O and CO2. The variability coefficients of CH4 emission flux were in the middle to strong range. Except for the interactive effect of irrigation and nitrogen on the total cumulative emission of CO2, and the effect of nitrogen fertilization on the total cumulative emission of CH4, irrigation and nitrogen fertilizer rates and their interactions had a very significant effect on tomato yield, GWP, GHGI, and the total cumulative emission of N2O, CO2, and CH4. Additionally, as nitrogen fertilizer rates increased, the total cumulative emission of N2O also increased. The total cumulative emission of N2O and CO2 had a significant, positive correlation with GWP; the average contribution rate of N2O to GWP was 5.25% compared with a GWP of 94.59% for CO2. Ultimately, reducing the nitrogen fertilizer rate and increasing the irrigation lower limit could effectively reduce greenhouse gas emissions and ameliorate global warming. In this study, W2N1 treatment provided the optimal regulation of irrigation and nitrogen fertilization needed to increase tomato yield and mitigate greenhouse gas emissions.
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