首页 | 本学科首页   官方微博 | 高级检索  
   检索      

免耕稻田氮肥运筹对土壤NH3挥发及氮肥利用率的影响
引用本文:马玉华,刘兵,张枝盛,郑大,周亮,曹凑贵,李成芳.免耕稻田氮肥运筹对土壤NH3挥发及氮肥利用率的影响[J].生态学报,2013,33(18):5556-5564.
作者姓名:马玉华  刘兵  张枝盛  郑大  周亮  曹凑贵  李成芳
作者单位:农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070;农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070;农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070;农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070;农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070;农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070;农业部长江中游作物生理生态与耕作重点实验室, 武汉 430070;华中农业大学植物科技学院, 武汉 430070
基金项目:国家科技支撑计划:粮食丰产科技工程(2011BAD16B02); 国家自然科学基金(31100319); 中央高校基本科研业务费专项资金(2013PY106)
摘    要:通过大田试验,设置5种不同的施肥比例(基肥:分蘖肥:拔节肥:穗肥-2:2:3:3(R1)、3:2:2:3(R2)、4:2:2:2(R3)、4:3:1:2(R4)与0:0:0:0(CK)),研究氮肥运筹对稻田NH3挥发和氮肥利用率的影响。结果表明,(1)相对于不施肥,施肥显著提高了稻田NH3挥发量。氮肥施用后,NH3挥发损失量占施氮量的6.2%-8.5%,其中,以分蘖期NH3挥发损失量最大,齐穗期次之,苗期和拔节期最小。施肥处理间,处理R1稻田累积NH3挥发量最小,显著低于其它施肥处理,比处理R2、R3和R4分别低9.1%(P<0.05)、10.9%(P<0.05)和17.7%(P<0.05)。(2)相关分析表明,田面水NH4+、pH值和土壤NH4+和pH值均与稻田土壤NH3挥发通量呈显著或者极显著相关;(3)处理R1水稻氮肥利用率相对于处理R2、R3和R4增加了28.4%(P<0.05)、55.4%(P<0.05)和74.9%(P<0.05)。研究表明,氮肥后移能有效降低免耕稻田NH3挥发,提高水稻的氮肥利用率。

关 键 词:氮肥运筹  NH3  NH4+  氮肥利用效率
收稿时间:4/2/2013 12:00:00 AM
修稿时间:7/1/2013 12:00:00 AM

Effects of nitrogen management on NH3 volatilization and nitrogen use efficiency under no-tillage paddy fields
MA Yuhu,LIU Bing,ZHANG Zhisheng,ZHENG D,ZHOU Liang,CAO Cougui and LI Chengfang.Effects of nitrogen management on NH3 volatilization and nitrogen use efficiency under no-tillage paddy fields[J].Acta Ecologica Sinica,2013,33(18):5556-5564.
Authors:MA Yuhu  LIU Bing  ZHANG Zhisheng  ZHENG D  ZHOU Liang  CAO Cougui and LI Chengfang
Institution:Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China;Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China;Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China;Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China;Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China;Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China;Key Laboratory of Crop Ecophysiology and Farming System in the Middle Reaches of the Yangtze River, Ministry of Agriculture of China, Wuhan, Hubei 430070, China;College of Plant Science and Technology, Huazhong Agricultural University, Wuhan, Hubei 430070, China
Abstract:NH3 volatilization is an important process of N loss from fertilizer nitrogen (N) applied to no-tillage rice fields. It has been demonstrated that no-tillage promotes NH3 volatilization. However, few studies have been conducted to investigate the effects of N management on NH3 volatilization from no-tillage paddy fields. Therefore, a field experiment was conducted on a clay loam soil (Anthrosol, World Reference Base for Soil Resources) to study the effects of N management on NH3 volatilization and N use efficiency from no-tillage rice fields in the city of Wuxue in central China during the 2012 rice-growing season. In this study, five experimental treatments were arranged in a completely randomized design with three replications. Five treatments were applied including five application rates of N fertilizer in the seedling, mid-tillering, flowering and heading stages of rice: 2:2:3:3 (R1), 3:2:2:3 (R2), 4:2:2:2 (R3), 4:3:1:2 (R4) and 0:0:0:0 (CK). The NH3 volatilization fluxes were determined 20 times using a venting method during the 2012 rice growing season. NH4+ concentrations and pH of the soils and field surface water were also measured. The obtained results showed that application of N fertilizer significantly enhanced both NH4+ concentrations of the soils and field surface water and the soil pH. Compared with the other fertilized treatments (R2, R3 and R4), R1 significantly decreased NH4+ concentrations of the soils and field surface water. In the fertilized treatments, during the rice growing season, each application of N fertilizer led to NH3 volatilization fluxes peaking after 1-3 days, and then dropping rapidly to those in the unfertilized treatment levels within 1-2 weeks. The NH3 volatilization fluxes in the CK treatment were relatively low, and remained nearly unchanged. The NH3 volatilization fluxes ranged from 2.0 to 21.94 mg·m-2·d-1 for the CK treatment and from 2.21 to 209.6 mg·m-2·d-1 for the fertilized treatments. Mean NH3 volatilization fluxes in the R1, R2, R3 and R4 treatments were (13.8±2.0), (15.3±0.2), (15.8±0.1) and (14.2±0.1) mg·m-2·d-1, respectively, which were 1.57, 1.81, 1.88 and 1.69 times, respectively, that in the CK treatment. The cumulative amounts of NH3 volatilization were (8.52±0.20) (CK), (19.59±2.30) (R1), (21.85±0.68) (R2), (21.98±0.45) (R3) and (23.79±1.15) kg N/hm2 (R4). For fertilized treatments, the highest cumulative NH3 volatilization was observed at the mid-tillering stage (accounting for 11.9%-14.7% of the total), followed by the heading stage, with the minimum being found at the seeding and booting stages. Compared with no N fertilizer, application of N fertilizer significantly increased NH3 volatilization by 56.5%-64.2% from the no-tillage paddy fields. In fertilized treatments, N losses through NH3 volatilization accounted for 6.2%-8.5% of the applied N. Among the four fertilized treatments, the cumulative NH3 volatilization was significantly reduced by 9.1%-17.7% under R1 than under the other fertilized treatments. Linear correlation analysis indicated that NH4+ concentrations and pH in the soils and field surface water were significantly related to the NH3 volatilization fluxes. Application of N fertilizer significantly affected N uptake of rice, where, compared with the CK treatments, fertilized treatments significantly increased N uptake of rice by 46.5%-89.3%. Compared with the other fertilized treatments, R1 significantly enhanced N use efficiency by 28.4%-74.9%. Therefore, our results suggest that N application at the late growth stage of rice can decrease NH3 volatilization, thus improving N use efficiency of rice under no-tillage rice fields.
Keywords:nitrogen management  NH3  NH4+  nitrogen use efficiency
点击此处可从《生态学报》浏览原始摘要信息
点击此处可从《生态学报》下载免费的PDF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