首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >Characteristics and Distribution of Organic Phosphorus Fractions in the Surface Sediments of the Inflow Rivers around Hongze Lake China
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Characteristics and Distribution of Organic Phosphorus Fractions in the Surface Sediments of the Inflow Rivers around Hongze Lake China

机译:洪泽湖附近入流河流表层沉积物中有机磷组分的特征与分布

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摘要

In this study, the characteristics and distribution of the organic phosphorus (Po) fractions in the surface sediments of seven inflow rivers around Hongze Lake in China were analyzed with a soil Po fraction method, as used by Ivanoff. The relationships between the Po fractions and physiochemical features of sediments were also discussed. The results showed that, the sediments of the rivers had been moderately pollution with certain ecological risk effects except the Waste Yellow River. The relative contribution order of the Po fractions in the sediments was residual Po > HCl-Po > fulvic acid-Po > humic acid-Po > labile organic phosphorus (LOP). Moderately labile organic phosphorus (MLOP) was the main part of the Po forms in the whole sediments. The risk of phosphorus released from river sediments was the highest in the western region, followed by the southwestern region, and finally the northwestern region. There were significant correlations between Po forms and total phosphorus (TP), inorganic phosphorus (Pi), and Po. Non labile organic phosphorus (NLOP) had the strongest correlation with TP. The distribution of Po forms in each region was different due to the impact of human activities, industrial and agricultural production and the land types; the heaver polluted sediments with higher Po fractions. It is suggested that most of the sediments of the inflow rivers in the regions have certain ecological risk effects and P of them have an important contributions on the eutrophication of Hongze Lake. Po forms can provide a reliable theoretical basis for dealing with the change of water quality and should be paid more attention in the lake eutrophication investigation. There was reciprocal transformation between different Po forms, especially non-bioavailable fraction can change into bio-available ones. The results can provide a basis for the earth cycle of phosphorus and a new perspective of eutrophication control of shallow lakes.
机译:本研究采用伊万诺夫(Ivanoff)的土壤Po分数法,分析了中国洪泽湖周围7条入江河流表层沉积物中有机磷(Po)的特征和分布。还讨论了Po含量与沉积物理化特征之间的关系。结果表明,除废黄河外,河流沉积物已受到中度污染,具有一定的生态风险作用。沉积物中Po组分的相对贡献顺序为:残余Po> HCl-Po>黄腐酸-Po>腐殖酸-Po>不稳定有机磷(LOP)。中度不稳定的有机磷(MLOP)是整个沉积物中Po形态的主要部分。从河流沉积物中释放磷的风险在西部地区最高,其次是西南地区,最后是西北地区。 Po形式与总磷(TP),无机磷(Pi)和Po之间存在显着相关性。非活性有机磷(NLOP)与TP的相关性最强。由于人类活动,工农业生产和土地类型的影响,每个地区的Po形态分布都不同。重金属污染了具有较高Po含量的沉积物。建议该地区入流河流的大部分沉积物具有一定的生态风险效应,其中P对洪泽湖的富营养化有重要贡献。 Po形式可以为处理水质变化提供可靠的理论基础,在湖泊富营养化调查中应引起更多重视。在不同的Po形式之间存在相互转化,特别是非生物可利用的部分可以转变为生物可利用的部分。研究结果可为磷的地球循环和浅水湖泊富营养化控制提供新的依据。

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