生态与农村环境学报 ›› 2018, Vol. 34 ›› Issue (4): 349-355.doi: 10.11934/j.issn.1673-4831.2018.04.008

• 污染控制与修复 • 上一篇    下一篇

减肥措施对稻田田面水氮、磷动态变化特征的影响

吕亚敏1, 吴玉红2, 李洪达1, 雷同1, 吕家珑1   

  1. 1. 西北农林科技大学资源环境学院/农业部西北植物营养与农业环境重点实验室, 陕西 杨凌 712100;
    2. 汉中市农业科学研究所, 陕西 汉中 723000
  • 收稿日期:2017-08-31 出版日期:2018-04-25 发布日期:2018-04-17
  • 通讯作者: 吕家珑 E-mail:ljlll@nwsuaf.edu.cn
  • 作者简介:吕亚敏(1992-),女,山东青岛人,硕士生,主要从事氮磷面源污染的研究。E-mail:Lyuyaminsunshine@163.com
  • 基金资助:

    陕西省科技统筹创新工程计划(2016KTZDNY03-01);陕西省水利科技项目(2016slkj-15)

Effects of Dynamic Changes of Nitrogen and Phosphorus Concentrations in Surface Water of Paddy Field Under Different Fertilizer Rate

LÜ Ya-min1, WU Yu-hong2, LI Hong-da1, LEI Tong1, LÜ Jia-long1   

  1. 1. College of Natural Resources and Environment, Northwest A & F University/Key Laboratory of Plant Nutrition and the Agri-Environment in Northwest China, Ministry of Agriculture, Yangling 712100, China;
    2. Hanzhong Agricultural Science Institute, Hanzhong 723000, China
  • Received:2017-08-31 Online:2018-04-25 Published:2018-04-17

摘要:

我国水稻种植面积大,过量施肥后稻田氨挥发、氮磷径流和渗漏等途径会引起农业面源污染等问题,而水稻淹水阶段田面水中氮、磷浓度是关键控制因子。通过设置田间小区隔板,开展肥料减量试验,研究稻季田面水不同形态氮、磷动态变化特征,同时探讨其潜在的环境效应。结果表明,磷肥施入后田面水总磷(TP)、总可溶性磷(TDP)和颗粒态磷(PP)浓度均呈先升高后降低趋势,9 d内下降迅速;基肥施入9 d,当氮、磷水平分别为214、90 kg·hm-2时,TP、TDP和PP质量浓度分别为0.76、0.71和0.03 mg·L-1;晒田结束后,田面水中TP和TDP浓度出现1次回升。各处理铵态氮和硝态氮浓度分别在基肥施入后第2天和第5天达到峰值;当施氮量为214、182和162 kg·hm-2时,田面水铵态氮浓度分别为对照的15.83、9.16和7.86倍,5 d内铵态氮浓度下降迅速且不同施肥处理间差异趋同。此外,增施氮磷肥料并不能显著增加水稻产量,当氮、磷水平分别为214、90 kg·hm-2时,水稻产量反而降低。因此,提出施磷后9 d内和晒田复水后是控制田面水磷流失的关键时期,而控制氮损失的关键时期是施肥后5 d内。综合水稻产量和肥料农学效率,证实试验田氮肥或磷肥减量25%是可行的,但仍需进一步通过大田试验验证其产量的持续性。

关键词: 田面水, 氮形态, 磷形态, 氮减量, 磷减量

Abstract:

Rice is broadly planted in China. Ammonia volatilization, nitrogen (N) and phosphorus (P) runoff and leakage have caused agricultural non-point source pollution and other issues due to excessive fertilization. The concentration of N and P in surface water during the flooding period is the key control factor. The dynamic characteristics of N and P in surface water of paddy field and their potential environmental impact were studied by field experiment with different P and N application. The results show that the concentration of total P (TP), total dissolved P (TDP) and particulate P (PP) all increased rapidly within 9 days after P application and then decreased. The concentrations of TP, TDP, and PP reached 0.76, 0.71 and 0.03 mg·L-1 with 214 and 90 kg·hm-2 N and P application, respectively. Besides, the concentration of TP and TDP showed an obvious rise after the soil-drying period. The concentration of ammonium nitrogen and nitrate in all treatments reached to maximum in 2 and 5 days, respectively, after the application of basal fertilizer. The concentration of ammonium nitrogen with 214,182 and 162 kg·hm-2 of N application were 15.83, 9.16 and 7.86 times of that in control treatment. N concentration decreased rapidly after 5 days and the differences between treatments became much smaller. In addition, increasing N and P application amount did not significantly increase the rice yield, but inversely, rice yield decreased with 214 and 90 kg·hm-2 of N and P application, respectively. Therefore, 9 days after P application and the stage after rewetting were the key periods for controlling P losses through runoff in surface water from paddy field, while 5 days following N application is the vital period for controlling N losses. By considering both rice yield and fertilizer agronomic efficiency, it is feasible to reduce 25% of N and P application. However, this should be further investigated for high yield consistency through field experiment.

Key words: surface water, nitrogen form, phosphorus form, reduction of nitrogen application rate, reduction of phosphorus application rate

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