4.7 Article

Runoff characteristics and nutrient loss mechanism from plain farmland under simulated rainfall conditions

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 468, 期 -, 页码 1069-1077

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2013.09.035

关键词

Non-point source pollution; Plain farmland; Soil nutrients; Loss mechanism; Rainfall simulation

资金

  1. National Natural Science Foundation of China [41001352]
  2. Fundamental Research Funds for the Central Universities
  3. Open Research Foundation of Pearl River Hydraulic Research Institute, PRWRI [[2010] KJ01]
  4. Water Specific Project of China [2008ZX07209-007]

向作者/读者索取更多资源

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 5.1 mm, a rainfall intensity of 50 mm/h, and an antecedent soil moisture of approximately 29.6%. (C) 2013 Elsevier B.V. All rights reserved.

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