State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, No. 19, Xinjiekouwai Street, Beijing 100875, China.
Sci Total Environ. 2014 Jan 15;468-469:1069-77. doi: 10.1016/j.scitotenv.2013.09.035. Epub 2013 Oct 4.
In recent years, nonpoint source (NPS) pollution has become the main contributor to water quality problems. Research on nitrogen (N) and phosphorus (P) losses from farmland and the factors that influence these losses is very meaningful both for increasing the crop yield and for improving environmental water quality. To explore the mechanism by which N and P are lost from farmland in the North China Plain (NCP), 16 simulated rainfalls were conducted in 14 experimental fields (each of which had different conditions) in the NCP from July to August in 2010. The results showed that the rainfall intensity, the antecedent soil moisture content, and the vegetation cover status were the main factors that affected the surface runoff in the NCP. The runoff volume increased with the increasing rainfall intensity and the increasing soil moisture content, and decreased with the increasing vegetation cover. These factors also significantly affected the losses of P and N. The losses of P and N were positively correlated with the rainfall intensity and the antecedent soil moisture content, and negatively correlated with the vegetation cover. A longer and more intense rainfall resulted in a higher loss of N and P. Dissolved nitrogen was the predominant form of N loss. For phosphorous, the predominant loss form was greatly influenced by the rainfall intensity, the vegetation cover, and the antecedent soil moisture content. Most of phosphorus existed as dissolved phosphorus in Baizhuang (BZ) and as particulate phosphorus in Tangcheng (TC) and Fentai (FT). The minimum requirements for runoff occurrence in experimental regions were a rainfall depth of 5.1mm, a rainfall intensity of 50mm/h, and an antecedent soil moisture of approximately 29.6%.
近年来,非点源(NPS)污染已成为水质问题的主要成因。研究农田氮(N)磷(P)流失及其影响因素,对于提高作物产量和改善环境水质都具有重要意义。为了探究华北平原农田氮磷流失的机理,于 2010 年 7-8 月在该地区 14 个实验农田(每个农田的条件均不同)中进行了 16 次模拟降雨。结果表明,降雨强度、前期土壤含水量和植被覆盖状况是影响华北平原地表径流的主要因素。径流量随降雨强度和土壤含水量的增加而增加,随植被覆盖度的增加而减少。这些因素也显著影响 P 和 N 的流失。P 和 N 的流失与降雨强度和前期土壤含水量呈正相关,与植被覆盖度呈负相关。较长且强烈的降雨会导致 N 和 P 的更高流失。溶解态氮是 N 流失的主要形态。对于磷,主要流失形式受降雨强度、植被覆盖和前期土壤含水量的影响较大。大部分磷以溶解态磷的形式存在于柏庄(BZ),以颗粒态磷的形式存在于唐城(TC)和范台(FT)。实验区发生径流的最低要求为降雨深度 5.1mm、降雨强度 50mm/h 和前期土壤含水量约 29.6%。