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Phosphorus characteristics, distribution, and relationship with environmental factors in surface sediments of river systems in Eastern China

机译:中国东部河流系统表层沉积物中磷的特征,分布及其与环境因子的关系

摘要

Phosphorus (P) is an essential nutrient for aquatic organisms. However, too much P discharged into limnetic ecosystems can induce eutrophication. The concentration of P in freshwater ecosystems has escalated in Eastern China due to overuse of fertilizer and excess emission of sewage, which is the result of the development of industry and agriculture in this area. However, little is known about the P characteristics and its environmental factors in river systems. Here, we present the results of P characterization and its relationships with environmental factors in Eastern China by applying SMT and P-31-NMR methods. The results showed that the concentrations of P in surface sediments varied with the river system, and more than 50 % of the samples had P concentrations exceeding 500 mg kg(-1). HCl-Pi was the dominant Pi in surface sediments, with the highest percentage (96.5 %) in the Yellow River System. Mono-P was the dominant Po in river sediments, followed by DNA-P. The PCA approach indicated that NaOH-Pi and ortho-P clustered in one group, with a second group including mono-P, diesters-P, and HCl-Pi. Phon-P and pyro-P belonged to different groups. On a regional scale, NaOH-Pi and Po showed a negative relationship with pH in sediments. Continuous eutrophication was induced by the presence of dams, and oxygen-consuming pollutants, such as NH3-N and CODcr, even when external P input was cut in heavily polluted rivers. The research revealed the characteristics of P in different river systems and proposed a conceptual model of P biogeochemical cycles in heavily polluted rivers. Results from this study may provide insight into P characteristics in Eastern China and would set a scientific basis for effective P management in developing countries.
机译:磷(P)是水生生物必需的营养素。然而,排放到限制生态系统中的磷过多会引起富营养化。由于化肥的过度使用和污水的过量排放,华东地区淡水生态系统中的P浓度已经升高,这是该地区工农业发展的结果。但是,对于河流系统中的磷特性及其环境因素知之甚少。在这里,我们通过应用SMT和P-31-NMR方法介绍了华东地区P表征的结果及其与环境因素的关系。结果表明,表层沉积物中磷的含量随河流系统的变化而变化,超过50%的样品中磷的含量超过500 mg kg(-1)。 HCl-Pi是表面沉积物中主要的Pi,在黄河系统中比例最高(96.5%)。 Mono-P是河流沉积物中的主要Po,其次是DNA-P。 PCA方法表明,NaOH-Pi和邻位P聚集在一组中,第二组包括mono-P,二酯-P和HCl-Pi。 Phon-P和pyro-P属于不同的组。在区域范围内,NaOH-Pi和Po与沉积物中的pH呈负相关。即使在污染严重的河流中切断了外部磷的输入,由于水坝和诸如NH3-N和CODcr之类的耗氧污染物的存在,也引起了持续的富营养化。研究揭示了不同河流系统中磷的特征,并提出了重度污染河流中磷生物地球化学循环的概念模型。这项研究的结果可能会提供有关中国东部磷素特征的见解,并为发展中国家有效磷素管理奠定科学基础。

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