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种植模式对喀斯特山地农田土壤可溶性氮含量、组分及迁移的影响
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  • 英文篇名:Effects of cropping patterns on the content,composition and migration of soluble nitrogen in cropland soil in karst region
  • 作者:杨成 ; 孟凡非 ; 彭艳 ; 崔丽 ; 刘涛泽 ; 罗绪强
  • 英文作者:YANG Cheng;MENG Fan-fei;PENG Yan;CUI Lifang;LIU Tao-ze;LUO Xu-qiang;College of Eco-Environmental Engineering,Guizhou Minzu University;State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences;School of Geography and Resources,Guizhou Education University;
  • 关键词:可溶性有机氮 ; 种植模式 ; 土壤 ; 喀斯特地区
  • 英文关键词:soluble organic nitrogen;;cropping pattern;;soil;;karst region
  • 中文刊名:生态学杂志
  • 英文刊名:Chinese Journal of Ecology
  • 机构:贵州民族大学生态环境工程学院;中国科学院地球化学研究所环境地球化学国家重点实验室;贵州师范学院地理与资源学院;
  • 出版日期:2019-06-04 16:38
  • 出版单位:生态学杂志
  • 年:2019
  • 期:10
  • 基金:国家自然科学基金项目(41563013、41563007和41571130042);; 贵州省科技厅科技计划项目(黔科合SY字〔2012〕3165、黔科合基础﹝2018)1074号);; 贵州省教育厅青年科技人才成长项目(黔教合KY字[2016] 161)资助
  • 语种:中文;
  • 页:125-133
  • 页数:9
  • CN:21-1148/Q
  • ISSN:1000-4890
  • 分类号:S153.6
摘要
以贵州喀斯特山地6种不同种植模式农田土壤为对象,研究种植模式对农田土壤可溶性氮含量、组分及迁移的影响。结果表明:6种不同种植模式农田土壤可溶性无机氮(SIN)、可溶性有机氮(SON)和可溶性总氮(TSN)含量分别为3.75~95.15、21.17~155.91和28.76~188.95 mg·kg-1,平均含量分别为26.49、59.76和86.25 mg·kg-1;不同种植模式中SIN含量表现为葱-姜轮作>葱-玉米轮作>葱-水淹休耕>葱-葱连作>葱-休耕>葱-水稻轮作,SON含量表现为葱-葱连作>葱-姜轮作>葱-玉米轮作>葱-水淹休耕>葱-休耕>葱-水稻轮作,TSN含量表现为葱-姜轮作>葱-葱连作>葱-玉米轮作>葱-水淹休耕>葱-休耕>葱-水稻轮作;土壤SON/TSN的比例占60%以上,最高可达82.4%,为农田土壤可溶性氮的主要组分; 6种不同种植模式农田土壤SIN和SON含量在0~60 cm土层中,表现为随着土层的增加而下降;种植模式对农田土壤可溶性氮含量和组分有着显著影响,SON为农田土壤氮流失的主要形态,应引起重视。
        We examined the effects of six different cropping patterns on the content,composition and migration of soluble nitrogen in cropland soils in Guizhou karst region. The results showed that the contents of soil soluble inorganic nitrogen( SIN),soluble organic nitrogen( SON) and soluble total nitrogen( TSN) ranged from 3.75 to 95.15 mg·kg-1,21.17 to 155.91 mg·kg-1 and 28.76 to 188. 95 mg · kg-1,with a mean value of 26.49,59.76 and 86.25 mg·kg-1,respectively. The contents of SIN under different cropping patterns were as the following order:chive-ginger rotation land > chive-maize rotation land > chive-waterlogged and fallowed land >chive-chive continuous cultivation land> chive-fallowed land> chive-rice rotation land. For SON,the order was: chive-chive continuous cultivation land> chive-ginger rotation land> chive-maize rotation land > chive-waterlogged and fallowed land > chive-fallowed land > chive-rice rotation land. For TSN,the order was: chive-ginger rotation land> chive-chive continuous cultivation land> chive-maize rotation land > chive-waterlogged and fallowed land > chive-fallowed land > chiverice rotation land. SON and NH4+-N were the main components of soil soluble nitrogen. The SON/TSN ratios were more than 60%,with the highest of 82.4%. The contents of SIN and SON decreased with soil depth at 0-60 cm layers. Our results indicate that cropping patterns have significant impacts on the content and composition of soluble nitrogen in cropland soil. SON is the major form of nitrogen loss from cropland soil,which should be paid attention to.
引文
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