首页 | 本学科首页   官方微博 | 高级检索  
     

秸秆分解对两种类型土壤无机氮和氧化亚氮排放的影响
引用本文:张学林,吴梅,何堂庆,张晨曦,田明慧,李晓立,侯小畔,郝晓峰,杨青华,李潮海. 秸秆分解对两种类型土壤无机氮和氧化亚氮排放的影响[J]. 中国农业科学, 2022, 55(4): 729-742. DOI: 10.3864/j.issn.0578-1752.2022.04.009
作者姓名:张学林  吴梅  何堂庆  张晨曦  田明慧  李晓立  侯小畔  郝晓峰  杨青华  李潮海
作者单位:河南农业大学农学院/省部共建小麦玉米作物学国家重点实验室/2011河南粮食作物协同创新中心,郑州 450002
基金项目:国家重点研发计划课题(2018YFD0200605);;河南省自然科学基金(182300410013);
摘    要:[目的]明确作物秸秆分解对土壤无机氮和氧化亚氮(N2O)排放的影响,为不同土壤类型采用合理的氮肥用量,促进秸秆分解、增加土壤可利用养分、减少N2O等温室气体排放提供理论依据.[方法]室内采用尼龙网袋法,设置秸秆类型(小麦和玉米)、土壤类型(潮土和砂姜黑土)和氮肥用量(N0:0,N1:180 kg N·hm-2,N2:3...

关 键 词:秸秆  潮土  砂姜黑土  温室气体  氮素矿化  全球变暖潜力
收稿时间:2021-01-11

Effects of Crop Residue Decomposition on Soil Inorganic Nitrogen and Greenhouse Gas Emissions from Fluvo-Aquic Soil and Shajiang Black Soil
ZHANG XueLin,WU Mei,HE TangQing,ZHANG ChenXi,TIAN MingHui,LI XiaoLi,HOU XiaoPan,HAO XiaoFeng,YANG QingHua,LI ChaoHai. Effects of Crop Residue Decomposition on Soil Inorganic Nitrogen and Greenhouse Gas Emissions from Fluvo-Aquic Soil and Shajiang Black Soil[J]. Scientia Agricultura Sinica, 2022, 55(4): 729-742. DOI: 10.3864/j.issn.0578-1752.2022.04.009
Authors:ZHANG XueLin  WU Mei  HE TangQing  ZHANG ChenXi  TIAN MingHui  LI XiaoLi  HOU XiaoPan  HAO XiaoFeng  YANG QingHua  LI ChaoHai
Affiliation:Agronomy College, Henan Agricultural University/State Key Laboratory of Wheat and Maize Crop Science/Collaborative Innovation Center of Henan Grain Crops for 2011, Zhengzhou 450002
Abstract:【Objective】The purpose of this study was to examine the effects of crop residue decomposition on soil available nitrogen (N) and nitrous oxide (N2O) emissions, and provide a theoretical basis for reasonable N fertilizer rate in agricultural soils to promote residue decomposition, to increase soil available nutrients, and to reduce N2O emissions. 【Method】The indoor soil incubations with nylon decomposition bag were conducted to study the effects of crop residue types (wheat and maize), soil types (fluvo-aquic soil: AS and Shajiang black soil: LS) and N fertilizer rates (N0: 0; N1: 180 kg N·hm-2; N2: 360 kg N·hm-2) on soil N2O emission. A control (CK) without residue addition and N fertilizer input was also established for the two soil types. Inorganic N content, N2O and CO2 flux, and soil enzyme activity were measured in incubated soil. 【Result】Compared with CK, soil inorganic N content under N0 decreased significantly, which was decreased by 0.8 mg·g-1 for 1 g wheat residue addition or 0.4 mg·g-1 for 1 g maize residue addition. Compared with AS, soil inorganic N content in LS reduced by 16% with wheat residue addition, by 41% with maize residue addition. Compared with wheat residue addition, soil inorganic N content in AS and LS increased by 111% and 252% with maize residue addition, respectively. Compared with CK, both soil N2O and CO2 flux increased with wheat residue or maize residue addition, and the total accumulation of soil N2O flux under N0 treatment increased by 70% and 47% with wheat residue and maize residue addition, by 346% and 154% for CO2 accumulation, and by 53% and 71% for global warming potential, respectively. Compared with AS, soil N2O flux in LS reduced by 38% and 61% with wheat residue and maize residue addition, by 12% and 51% for the accumulation of N2O flux, and by 28% and 16% for the accumulation of CO2 flux, respectively. And the global warming potential in LS increased by 13% with the wheat residue addition in comparison with that in AS, while declined by 44% with maize residue addition. Compared with wheat residue addition, the accumulation of soil N2O flux with maize residue addition increased by 88% in AS, and by 6% in LS, and reduced by 21% and 6% for the accumulation of soil CO2 flux in AS and LS, respectively. And the global warming potential with maize residue addition was 91% higher than that of wheat residue addition under the conditions of different N fertilizer rates and soil types. Compared with N0 and N2, soil N2O flux and their global warming potential under N1 treatment reduced significantly with wheat residue or maize residue addition in LS. Compared with CK, soil invertase activity increased with wheat residue or maize residue addition in both AS and LS, while which declined for soil Catalase and O2 content. Compared with wheat residue addition, soil urease activity, Catalase, and invertase activities declined with maize residue addition. Compared with AS, soil urease and catalase activities in LS reduced with wheat residue or maize residue addition, while soil O2 content increased. The catalase activities and O2 content was significantly and negatively related with soil N2O flux. 【Conclusion】The decomposition of wheat residue and maize residue reduced soil inorganic N content while increasing soil N2O flux. Soil inorganic N content and N2O flux with maize residue addition were higher than that of wheat residue. Emissions of N2O from Fluvo-aquic soil with wheat or maize residue addition was higher than that from Shajiang black soil. When combined with suitable N fertilizer rate, neither residues additions in Shajiang black soil increased N2O flux and global warming potential. These results suggested that, in the field, comprehensive management methods by returning residue to soil should consider the residue type, soil type and rate of N fertilization.
Keywords:crop residue  fluvo-aquic soil  Shajiang black soil  greenhouse gas  soil nitrogen mineralization  global warming potential  
点击此处可从《中国农业科学》浏览原始摘要信息
点击此处可从《中国农业科学》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号