Sprinkler-based rainfall simulation experiments to assess nitrogen and phosphorus losses from a hillslope cropland of purple soil in China

Chunyan Luo , Yang Gao , Bo Zhu , Tao Wang
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引用次数: 14

Abstract

Currently, water eutrophication has become a serious environmental pollution problem in China due to large amounts of nutrients input into Chinese rivers every year. In order to better understand the mechanisms of nitrogen and phosphorus transport induced by agricultural non-point pollution, we conducted simulated rainfall experiment on a hilly cropland of purple soil under different levels of rainfall intensity and cropland gradient. The dimensions of the experimental plot are: length × width × depth = 4.5 m × 1.5 m × 0.6 m, wherein cropland gradient can be adjusted. The results showed that the discharge process of surface and subsurface runoff was significantly enhanced with the elevated cropland gradient and simulated rainfall intensity. The total phosphorus (TP) transported by runoff was significantly increased with the elevated cropland gradient and simulated rainfall intensity, and accompanied by irregular fluctuation. The discrepancy of TP transport caused by rainfall intensity and cropland gradient was smaller by subsurface runoff than by surface runoff. The transport concentration of total nitrogen (TN) was higher for the subsurface runoff than for surface runoff. Due to different rainfall intensity and cropland gradient, the discrepancy on TN transport was larger by subsurface runoff than by surface runoff. In current study, TN transport by surface runoff was observed between 3.5 and 5.5 mg/L, but the concentration of TP is close to 100 g P/L under rainstorm events, which is the threshold for P eutrophication. The large nutrients losses for local farmers would be an important non-point pollution source to the Three Gorges Reservoir area that receives runoff from the watershed.

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基于喷淋的降雨模拟试验评估中国紫色土壤坡耕地氮磷损失
目前,由于每年大量的营养物质进入中国河流,水体富营养化已成为中国严重的环境污染问题。为了更好地了解农业面源污染对土壤氮磷运移的影响机制,在不同降雨强度和农田梯度条件下,对紫色土丘陵农田进行了模拟降雨试验。试验田的尺寸为:长×宽×深= 4.5 m × 1.5 m × 0.6 m,其中耕地坡度可调。结果表明:随着农田坡度的升高和模拟降雨强度的增大,地表和地下径流的排放过程显著增强;径流输运总磷(TP)随农田坡度升高和模拟降雨强度增大而显著增加,并伴有不规则波动。降雨强度和农田坡度对总磷输运的影响差异,地表径流对总磷输运的影响小于地下径流。地下径流输运总氮(TN)浓度高于地表径流。由于降雨强度和农田坡度的不同,地下径流对全氮输运的影响大于地表径流。在目前的研究中,地表径流输运全氮在3.5 ~ 5.5 mg/L之间,而在暴雨条件下,总磷浓度接近100 g P/L,这是磷富营养化的阈值。当地农民的大量养分损失将成为三峡库区接收流域径流的重要非点源污染源。
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