生态与农村环境学报 ›› 2018, Vol. 34 ›› Issue (9): 788-796.doi: 10.11934/j.issn.1673-4831.2018.09.004

• 农业面源污染监测与估算方法研究专题 • 上一篇    下一篇

稻田氮、磷损失与过程监测方法研究进展

胡冰涛1,2, 张龙江1, 杨士红2, 陈玉东1, 周慧平1   

  1. 1. 环境保护部南京环境科学研究所, 江苏 南京 210042;
    2. 河海大学水利水电学院, 江苏 南京 210098
  • 收稿日期:2017-10-11 出版日期:2018-09-25 发布日期:2018-10-25
  • 通讯作者: 陈玉东,E-mail:dongzi1225@sina.com;周慧平,E-mail:zhp@nies.org E-mail:dongzi1225@sina.com;zhp@nies.org
  • 作者简介:胡冰涛(1993-),男,安徽安庆人,硕士生,研究方向为农业面源污染控制。E-mail:huqiansiyi@yeah.net
  • 基金资助:

    国家重点研发计划(2016YFD0801106,2017YFD0801300);中央级公益性科研院所基本科研业务专项;国家水体污染控制与治理科技重大专项(2014ZX07101-012)

Research Advances on Process and Monitoring Methods of Nitrogen and Phosphorus Loss in Paddy Fields

HU Bing-tao1,2, ZHANG Long-jiang1, YANG Shi-hong2, CHEN Yu-dong1, ZHOU Hui-ping1   

  1. 1. Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing 210042, China;
    2. College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210098, China
  • Received:2017-10-11 Online:2018-09-25 Published:2018-10-25

摘要:

水稻是我国主要的粮食作物之一。水稻生产过程中土壤和肥料中的部分氮磷元素以溶质或颗粒形态通过淋溶、径流迁移至周围水体,造成地下水污染和水体富营养化。稻田土壤中氨挥发产生的氨气和反硝化反应产生的氧化亚氮气体进入大气,加剧了温室效应。笔者围绕稻田氮磷的气体挥发、径流和淋溶3个流失途径介绍了国内外常用的监测方法,并进一步讨论了针对径流和淋溶这2种流失途径的监测指标、监测频率和监测深度等问题,总结了2种流失途径的主要氮磷流失形态,根据产流特征和施肥时间确定监测时间节点,综合考虑植物吸收和地下水深度确定淋溶监测深度,以期为稻田氮磷流失监测提供相关技术支持和科学依据。

关键词: 稻田, 氮磷, 监测方法

Abstract:

Rice is one of the major cereal crops in China. During the rice production process, part of the nitrogen and phosphorus in the soil and fertilizer migrates to the surrounding water body through leaching and runoff in the form of solutes or particles, causing groundwater pollution and eutrophication of water bodies. Ammonia produced by ammonium volatilization in paddy soil and nitric oxide produced by denitrification reactions enter the atmosphere, aggravating the greenhouse effect. The commonly used monitoring methods of gas volatilization, runoff, and leaching in paddy fields from domestic and international studies are introduced, and the monitoring indicators, monitoring frequency, and monitoring depth in the pathways are further discussed; the main nitrogen and phosphorus forms in runoff loss and leaching loss are summarized; the monitoring frequency is determined by the characteristics of runoff and the fertilization; plant absorption and depth of groundwater should be considered to determine the depth of leaching monitoring. This study provides a reference for further monitoring of nitrogen and phosphorus losses in paddy fields.

Key words: paddy field, nitrogen and phosphorus, monitoring method

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