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Heavy metals distribution in the soils of Peshawar valley, Northern-Pakistan

机译:巴基斯坦北部白沙瓦河谷土壤中的重金属分布

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Information about metals concentrations in soil profiles of Peshawar-Pakistan in relation to their parent material is in scarcity. The study was aimed to identify the source of metals in soils and to determine the level of depletion and enrichment. Twenty two soil profiles derived from alluvium, piedmont alluvium, loess and re-deposits loess underlain by quaternary sediments with their respective parent materials were sampled and analyzed for metals by AAS. The average value of Ca, Fe, K, Mg, Na was significantly greater (p&0.05) in piedmont soils than red Murree shales. Cadmium was found to be high in all soils than the parent material. There was no significant difference in total content of Cu in all soils. Total content of Cd, Cr, Mn and Zn was found to be significantly greater (p&0.05) in piedmont soils than alluvium and loess soils, similarly Ni and Pb were significantly greater (p&0.05) in loess soils than piedmont and alluvium soils. The concentrations of Cr, Pb and Zn were significantly greater (p&0.05) in the A horizon of piedmont and alluvium soils than B horizon. The total content of all trace elements except for Cd and Ni was found to be significantly greater (p&0.05) than the reported mean for world soils. There was no significant difference between total trace elements content except for Cd and Ni between soils and parent materials. Data suggested no depletion or enrichment in all metals. All metals were evenly distributed and derived from similar parent material of sedimentary origin. These values could be considered as baseline levels for comparison with soils contaminated due to anthropogenic activities.
机译:缺乏关于白沙瓦-巴基斯坦土壤剖面中金属浓度与其母体材料有关的信息。该研究旨在确定土壤中的金属来源,并确定其消耗和富集水平。对二十二种土壤沉积物进行了取样,并利用原子吸收光谱法对来源于冲积层,山前冲积层,黄土和再沉积黄土的第四纪沉积物及其各自母体的土壤剖面进行了分析。在山前土壤中,Ca,Fe,K,Mg,Na的平均值明显大于红色的Murree页岩(p <0.05)。发现所有土壤中的镉含量都高于母体材料。在所有土壤中,铜的总含量没有显着差异。在山前土壤中Cd,Cr,Mn和Zn的总含量被发现比冲积土和黄土土壤显着更高(p <0.05),同样,在黄土土壤中,Ni和Pb的显着高于山麓土壤和冲积土(p <0.05)。 。山前土壤和冲积土的A层中的Cr,Pb和Zn的浓度显着高于B层(p <0.05)。发现除了Cd和Ni以外的所有微量元素的总含量明显大于所报道的世界土壤平均值(p <0.05)。除土壤和母体材料中的镉和镍外,总微量元素含量之间没有显着差异。数据表明所有金属均未消耗或富集。所有金属均分布均匀,并源自相似的沉积母体。这些值可被视为与人为活动污染的土壤进行比较的基准水平。

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