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旱作农业土壤矿质态氮随地表径流迁移特征研究
引用本文:赵亮,张自军,唐泽军,冯绍元.旱作农业土壤矿质态氮随地表径流迁移特征研究[J].环境科学学报,2010,30(10):1977-1984.
作者姓名:赵亮  张自军  唐泽军  冯绍元
作者单位:1. 中国农业大学水利与土木工程学院,北京,100083
2. 河北工程大学水电学院,邯郸,056021
3. 中国农业大学水利与土木工程学院,北京,100083;中国农业大学中国农业水问题研究中心,北京,100083
摘    要:为了了解旱作农业土壤中氮素随地表径流的流失水平及规律,于野外夏玉米试验田中进行了模拟降雨与自然降雨条件下的对比试验,并通过对水量和水质的同步监测,研究了不同施肥水平下氮素的流失效应.其中,模拟降雨采用的两个降雨强度分别为40和70mm.h-1,3个尿素施肥水平分别为287、431和575kg.hm-2(以N计),每次自然降雨的试验小区布置相同.试验期间,共有20次降雨事件(包括模拟降雨),其中,4次降雨过程中产生了地表径流并有氮素流失.结果表明,次降雨径流过程中硝态氮流失浓度先迅速增大后逐步降低,而铵态氮流失浓度变化平稳,且流失浓度较低.次降雨间氮素流失平均浓度相差较大,尤其体现在硝态氮浓度上更为明显.此外,研究发现,次降雨径流过程地表氮素流失初期效应明显,且受降雨强度影响显著.通过氮素流失水平的计算发现,研究区大于25mm的降雨类型会有明显的地表径流产生及氮素流失.

关 键 词:降雨  平均流失浓度  初期效应  氮素流失
收稿时间:1/31/2010 6:26:05 PM
修稿时间:5/19/2010 8:00:05 PM

Migration characteristics of mineral nitrogen with surface runoff in dry farmland soil
ZHAO Liang,ZHANG Zijun,TANG Zejun and FENG Shaoyuan.Migration characteristics of mineral nitrogen with surface runoff in dry farmland soil[J].Acta Scientiae Circumstantiae,2010,30(10):1977-1984.
Authors:ZHAO Liang  ZHANG Zijun  TANG Zejun and FENG Shaoyuan
Institution:College of Water Conservancy and Civil Engineering, China Agricultural University, Beijing 100083,College of Water Conservancy and Hydropower Engineering, Hebei University of Engineering, Handan 056021,1. College of Water Conservancy and Civil Engineering, China Agricultural University, Beijing 100083; 2. Center of Agricultural Water Research in China, China Agricultural University, Beijing 100083 and 1. College of Water Conservancy and Civil Engineering, China Agricultural University, Beijing 100083; 2. Center of Agricultural Water Research in China, China Agricultural University, Beijing 100083
Abstract:To understand the process of nitrogen loss with runoff in dry farming land, the field experimental study of nitrogen loss under different fertilization level at Summer Maize was conducted. In order to investigate degree of soil nitrogen loss with surface runoff in dry farmland, the water quantity and quality were monitored simultaneously. Simulated rainfall was conducted at 2 rainfall intensity: 40mm•h-1,70mm•h-1 and 3 urea fertilizer level: 287kgN•hm-2,431 kgN•hm-2,575 kgN•hm-2, and also had same treatments for natural rainfall trial. During the experiment period, there were four runoff and nitrogen loss events happened among all of twenty rainfall events (including the simulated rainfall). The results showed in the rainfall runoff process the concentration of nitrate loss increased rapidly in first, and then decreased gradually, whereas the loss of ammonium nitrogen concentration stable, and the loss of lower concentration during a rainstorm event. It also showed big difference comparison among different rainfalls in event mean concentration, especially in nitrate. In addition, first flush effect of nitrogen loss with runoff presented obviously and was found to be affected by rainfall intensity significantly. It was proved that the runoff and nitrogen loss always appeared above 25mm rainfall event in study area according to nitrogen loss calculated.
Keywords:Rainfall  Event mean concentration  First flush effect  Nitrogen loss
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