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土耳其西南部萨勒恰伊河流域痕量金属的来源与分布

Sources and distribution of trace metals in the Saricay Stream basin of southwestern Turkey.

作者信息

Tuna A Levent, Yilmaz F, Demirak A, Ozdemir N

机构信息

Department of Biology, Faculty of Science and Arts, Mugla University, Mugla, Turkey.

出版信息

Environ Monit Assess. 2007 Feb;125(1-3):47-57. doi: 10.1007/s10661-006-9238-1. Epub 2006 Aug 5.

Abstract

Seasonal variation of the concentrations of trace metals (Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb and Zn) were measured by ICP-AES in the water and sediment from the Saricay Stream, Geyik Dam and Ortakoy Well in the same basin. Comparisons between trace metal concentrations in water and sediment in three sources (Stream, Dam and Well) were made. The concentrations of a large number of trace metals in the water and sediment were generally higher in the Stream than in the Well and Dam, particularly in summer. Trace metal concentration ranges in sediments of the Saricay Stream and its sources showed very wide ranges (as mass ratio): Co: 5-476 microg g(-1), Cr: 15-1308 microg g(-1), Cu: 7-128 microg g(-1), Fe: 1120-13210 microg g(-1), Mn: 150-2613 microg g(-1), Ni: 102-390 microg g(-1), Pb: 0.7-31.3 microg g(-1) and Zn: 18-304 microg g(-1), whereas Cd was not detected. Trace metal concentration ranges found in waters were: Co: 9.5-20.7 microg L(-1), Cr: 20.3-284 microg L(-1), Cu: 170-840 microg L(-1), Fe: 176-1830 microg L(-1), Mn: 29.3-387 microg L(-1), and Ni: 4.3-21.9 microg L(-1). Among the trace metals studied, Cd and Zn in two seasons and Pb in winter were usually not detected or in the recommended levels. In addition, Cd was not detected in the sediment during the winter season. The analysis of variance (one-way ANOVA) and correlation matrix was employed for the sediment and water samples of the two field surveys (summer and winter) comparison. The three sources showed differences in metal contents. The metal levels in sediments displayed marked seasonal and regional variations, which were attributed to anthropogenic influences and natural processes. In the Saricay Stream, high values of metals during the dry season showed an anthropological effect from small industry firms, e.g.: an olive mill and a dairy farm or water dilution during summer seasons. Finally, the pollution in this basin probably originated from small industrial, low quality coal-burned thermal power plants, and particularly agricultural and domestic waste discharges.

摘要

采用电感耦合等离子体发射光谱法(ICP-AES)测定了同一流域内萨勒恰伊河、盖伊克大坝和奥尔塔科伊井的水和沉积物中痕量金属(镉、钴、铬、铜、铁、锰、镍、铅和锌)浓度的季节变化。对三个水源(河流、大坝和水井)水和沉积物中的痕量金属浓度进行了比较。河流中水体和沉积物中大量痕量金属的浓度通常高于水井和大坝,尤其是在夏季。萨勒恰伊河及其水源沉积物中的痕量金属浓度范围(质量比)非常宽:钴:5 - 476微克/克,铬:15 - 1308微克/克,铜:7 - 128微克/克,铁:1120 - 13210微克/克,锰:150 - 2613微克/克,镍:102 - 390微克/克,铅:0.7 - 31.3微克/克,锌:18 - 304微克/克,而未检测到镉。水体中痕量金属浓度范围为:钴:9.5 - 20.7微克/升,铬:20.3 - 284微克/升,铜:170 - 840微克/升,铁:176 - 1830微克/升,锰:29.3 - 387微克/升,镍:4.3 - 21.9微克/升。在所研究的痕量金属中,两个季节的镉和锌以及冬季的铅通常未被检测到或处于推荐水平。此外,冬季沉积物中未检测到镉。采用方差分析(单因素方差分析)和相关矩阵对两次实地调查(夏季和冬季)的沉积物和水样进行比较。三个水源的金属含量存在差异。沉积物中的金属含量显示出明显的季节和区域变化,这归因于人为影响和自然过程。在萨勒恰伊河中,旱季金属含量较高显示出小型工业企业(如橄榄油厂和奶牛场)的人为影响,或者夏季的水体稀释作用。最后,该流域的污染可能源于小型工业、低质量燃煤热电厂,特别是农业和生活污水排放。

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