Yang Li-Xia, Yang Gui-Shan, Yuan Shao-Feng, Wu Ye
Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.
Huan Jing Ke Xue. 2007 Aug;28(8):1763-9.
Experiments of field runoff plots, which were conducted at vegetable plots in Hongsheng town of Wuxi city--the typical region of Taihu Basin, were designed to assess the effects of different rainfall intensities on soil phosphorus runoff loss from vegetable plots by artificial rainfall simulations. Results showed that there was a relationship of power function between initial runoff-generation time and rainfall intensity. Runoff amount slowly increased under small rainfall intensity, but rapidly increased with rainfall intensity increase. The concentrations of total phosphorus (TP) and particulate phosphorus (PP) were higher at the early stage, then gradually decreased with time and finally reached a comparative steady stage under 0.83, 1.17 and 1.67 mm x min(-1). However they indicated no obvious trend except wavy undulation under 2.50 mm x min(-1). In the course of rainfall-runoff, dissolved phosphorus (DP) gently varied and accounted for 20% - 32% of TP. PP was 68% - 80% of TP and its change trend was consistent with TP. Therefore, PP was main loss form of soil phosphorus runoff. Comparison of different phosphorous loss rate under different rainfall intensities suggested that loss rate of TP and DP under 2.50 mm x min(-1) was 20 times and 33 times higher than that under 0.83 mm x min(-1), which showed that loss rate of PP and DP increased with the increase of rainfall intensities. Results indicated that lots of inorganic dissolved phosphorus (DIP) of phosphorous fertilizer was discharged into water environment by using fertilizer in soil surface before rainfall, which increased loss of DP and greatly aggravated degree of water eutrophication.
在太湖流域典型地区无锡市鸿声镇的蔬菜地开展了田间径流小区试验,通过人工模拟降雨来评估不同降雨强度对蔬菜地土壤磷素径流流失的影响。结果表明,初始产流时间与降雨强度之间存在幂函数关系。在小降雨强度下径流总量缓慢增加,但随降雨强度增加而迅速增加。在0.83、1.17和1.67毫米×分钟⁻¹降雨强度下,总磷(TP)和颗粒态磷(PP)浓度在初期较高,随后随时间逐渐降低,最终达到相对稳定阶段。然而,在2.50毫米×分钟⁻¹降雨强度下,它们除了呈波浪状起伏外无明显趋势。在降雨径流过程中,溶解态磷(DP)变化平缓,占TP的20% - 32%。PP占TP的68% - 80%,其变化趋势与TP一致。因此,PP是土壤磷素径流的主要流失形态。不同降雨强度下不同磷素流失率的比较表明,2.50毫米×分钟⁻¹降雨强度下TP和DP的流失率分别比0.83毫米×分钟⁻¹降雨强度下高20倍和33倍,这表明PP和DP的流失率随降雨强度增加而增大。结果表明,降雨前在土壤表层施肥导致大量无机溶解态磷(DIP)排入水环境,增加了DP的流失,极大地加剧了水体富营养化程度。