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灌溉与非灌溉条件下黄淮冬麦区不同追氮时期农田土壤氨挥发损失研究
引用本文:翟学旭,王振林,戴忠民,刘霞,王平,刘海涛,尹燕枰,曹丽,徐彩龙.灌溉与非灌溉条件下黄淮冬麦区不同追氮时期农田土壤氨挥发损失研究[J].植物营养与肥料学报,2013,19(1):55-67.
作者姓名:翟学旭  王振林  戴忠民  刘霞  王平  刘海涛  尹燕枰  曹丽  徐彩龙
作者单位:1. 山东农业大学作物生物学国家重点实验室,山东泰安,271018
2. 德州学院,山东德州,253023
3. 山东省农业科学院,山东济南,250100
4. 山东省泰安市农科院,山东泰安,271000
5. 中国农业大学资源与环境学院,北京,100094
基金项目:国家重点基础研究发展计划(973计划)项目(2009CB118602);国家公益性行业(农业)科研专项(201203100);国家自然科学基金项目(30871477);山东省自然科学基金项目(ZR2010CM044)资助
摘    要:采用通气法研究了灌溉与非灌溉条件下黄淮冬麦区农田氨挥发损失.结果表明,非灌溉条件下,麦田追肥氮的氨挥发主要发生在施肥后的5~25d内,追氮时期由起身期(SE,GS30)推迟到拔节期(JT,GS32),追肥氮的氨挥发速率峰值增大且出现时间提前;继续推迟至孕穗期(BT,GS41),氨挥发速率峰值减小.SE、JT和BT三个追氮时期的氨挥发损失量分别占追肥氮的24.84%~25.32%、25.42%~25.50%和14.77%~16.62%.灌溉(60mm)条件,不论何时追氮,麦田追肥氮氨挥发速率均变化较小,氨挥发损失量在N 0.40~0.55 kg/hm2之间,仅占追肥氮的0.36%~0.49%.非灌溉条件,氨挥发速率与0-10 cm土层土壤铵态氮浓度呈极显著的正相关关系;灌溉条件,氨挥发速率与10-20 cm土壤浓度呈极显著的正相关关系.土壤温度和降水是影响氨挥发的重要因素.此外,氨挥发还与农田土壤表面的通气状况有关,多穗型小麦品种更有利于减少麦田氨挥发的损失.

关 键 词:追氮时期  灌溉  氨挥发  通气法  铵态氮浓度
收稿时间:2012-03-30

Ammonia volatilization loss in Huang Huai winter wheat cultivation areas under irrigated and rainfed conditions
ZHAI Xue-xu,WANG Zhen-lin,DAI Zhong-min,LIU Xia,WANG Ping,LIU Hai-tao,YIN Yan-ping,CAO Li,XU Cai-long,CUI Zheng-yong,WU Guang-lei.Ammonia volatilization loss in Huang Huai winter wheat cultivation areas under irrigated and rainfed conditions[J].Plant Nutrition and Fertilizer Science,2013,19(1):55-67.
Authors:ZHAI Xue-xu  WANG Zhen-lin  DAI Zhong-min  LIU Xia  WANG Ping  LIU Hai-tao  YIN Yan-ping  CAO Li  XU Cai-long  CUI Zheng-yong  WU Guang-lei
Institution:1(1 Shandong Agricultural University/State Key Laboratory of Crop Biology,Shandong,Tai’an 271018,China; 2 Dezhou University,Shandong,Dezhou 253023,China;3 Shandong Academy of Agricultural Sciences,Shandong,Jinan 250100,China;4 Tai’an Academy of Agricultural Science,Shandong,Tai’an 27100,China;5 College of Resources and Environmental Sciences,China Agricultural University,Beijing 100094,China)
Abstract:A venting method was adopted to determine the effect of nitrogen topdressing stages on ammonia volatilization (AV) from topdressing fertilization in irrigated and rainfed wheat fields. The results show that under rainfed conditions, the AV from topdressing fertilization in wheat fields is mainly in the period from 5 to 25 days after the fertilization. With the delay of nitrogen topdressing stage from the pseudo stem erection stage (SE, GS30) to the jointing stage (JT, GS32), the peak value of the AV rate is increased and the occurrence time of the peak is ahead. With the delay of nitrogen topdressing stage to the booting (BT, GS41), the peak value of the AV rate is reduced. The rates of AV loss are 24.84%-25.32%, 25.42%-25.50% and 14.77%-16.62% in the SE, JT and BT treatments, respectively. Under 60 mm irrigation amount, the nitrogen fertilization stage has less effect on the AV, the AV rates from the topdressing fertilization are not changed significantly, and the N loss from the accumulated AV is N 0.40 to 0.55 kg/ha, only accounting for 0.36% to 0.49% of topdressing N. Under the rainfed conditions, there is a significant positive correlation between 0-10 cm layer soil NH4+-N concentration and the AV rate, and under irrigated conditions there is a significant positive correlation between 10-20 cm layer soil NH4+-N  concentration and the AV rate. Soil temperature and rainfall are the important influence factors of AV. In addition, AV is connected with aeration status of field soil surface. Multiple spike type wheat is helpful to reduce wheat field AV loss.
Keywords:nitrogen topdressing stage  irrigation  ammonia volatilization  venting method  NH4 -N concentration
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