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首页> 外文期刊>Environmental Science and Pollution Research >Distribution of phosphorous pools in western river sediments of the Urmia Lake basin, Iran
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Distribution of phosphorous pools in western river sediments of the Urmia Lake basin, Iran

机译:伊朗乌尔米湖盆地西部河流沉积物的分布

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Impact of anthropogenic loading of phosphorous (P) to an aquatic ecosystem can be qualitatively assessed by measuring the buildup and distribution of P in sediments and by differentiating bioavailable and recalcitrant P pools. Distribution of P pools in sediments is affected by the physico-chemical properties including specific elements, particle size distribution, pH, electrical conductivity (EC), and carbonate content. We applied X-ray fluorescence and scanning electron microscopy (SEM) methods to characterize sediments from western rivers in the Urmia Lake basin in Iran with a particular focus on properties that are relevant to P speciation. Phosphorous pools were sequentially extracted into operationally defined exchangeable (EXCH-P), iron and aluminum oxide-bound (Fe/Al-P), calcium-bound (Ca-P), and residual (RES-P) P pools. In river sediments, the size of P pool was found to be in the order of Ca-P > RES-P > Fe/Al-P > EXCH-P indicating small fraction of bioavailable P pool and Ca-P minerals being the most dominant P sink. Carbonate-related properties had an inverse relationship with bioavailable P pools in the river sediments studied. The principal component analysis (PCA) of the sequential extraction data with sediment properties revealed that four principal components described 82.7% of total variation. Similarly, particle size-related properties were found to have the highest eigenvalues in the first PC. Electron diffraction spectra (EDS) and X-ray fluorescence (XRF) analyses showed a largely uniform distribution of P in the upstream sediment. However, limited evidence of local enrichment of P with Fe, Al, and Ca contents was observed in the downstream river sediments. Correlation of Fe/Al-P pool size with Al~(2)O~(3)and SiO~(2)contents indicated that P was associated with Al oxide and clay minerals in the sediment matrix. Overall, the results from this study provide insights into the variability of upstream and downstream river processes and their relationship with P pools with regard to their bioavailability. These results are expected to be useful in assessing the potential impact of P loading on the aquatic ecosystem in the Urmia Lake basin.
机译:通过测量沉积物中P的累积和分布,可以定性评估磷(p)对水生生态系统的人为磷(p)的影响,并通过区分生物可利用和顽固的p池。沉积物中P池的分布受到物理化学性质的影响,包括特定元素,粒度分布,pH,电导率(EC)和碳酸酯含量。我们采用X射线荧光和扫描电子显微镜(SEM)的方法对相关为P形态特性尤其关注表征从伊朗湖乌尔米耶盆地西部的河流沉积物。依次提取磷池,进入可操作地定义的可更换的交换(Exch-P),氧化铝和氧化铝 - 结合(Fe / Al-P),钙结合(Ca-P)和残留(Res-P)P池。在河流沉积物中,发现P池的大小为Ca-P> RES-P> Fe / Al-P> Exch-p,表明少量生物可利用的P池和Ca-P矿物质是最占主导地位的P水槽。碳酸酯相关性质与研究的河沉积物中的生物可利用P池具有反比关系。沉积物特性的连续提取数据的主要成分分析(PCA)显示,四个主要成分描述了总变化的82.7%。类似地,发现粒子尺寸相关性质具有第一PC中的最高特征值。电子衍射光谱(EDS)和X射线荧光(XRF)分析在上游沉积物中显示出P的P均匀分布。然而,在下游河沉积物中观察到具有Fe,Al和Ca含量的P局部富集P的有限证据。用Al〜(2)O〜(3)和SiO〜(2)含量的Fe / Al-P池尺寸的相关性表明P与沉积物基质中的Al氧化物和粘土矿物质相关。总的来说,本研究的结果为上游和下游河流过程的变化以及与P池的关系提供了洞察力的洞察力。这些结果预计可用于评估P加载对乌尔米湖盆地水生生态系统的潜在影响。

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