松花江、黑龙江水中可溶性铁与有机质含量的相关性

Correlation Between Total Dissolved Iron and Organic Matter in Songhua River and Heilongjiang River

  • 摘要: 以黑龙江和松花江为研究对象,分析了河水中可溶性铁含量的分布特征及其与有机质含量、pH值的关系。结果表明,黑龙江、松花江水体中可溶性铁质量浓度分别为0.10~0.62和0.11~0.73mg·L-1,Fe2+质量浓度分别为0.01~0.16和0.04~0.35mg·L-1。松花江水体中可溶性铁、Fe2+浓度平均值均略高于黑龙江。同一年份内水体可溶性铁含量峰值以平水期居多。黑龙江水体CODCr与Fe2+含量呈显著负相关,松花江水体CODCr与可溶性铁含量呈显著正相关。松花江水体中BOD5、pH值与Fe2+含量呈显著负相关。人为来源的难生物降解有机质的大量输入提高了河水中铁离子的络合容量,使水中可溶性铁和有机络合铁含量增加。

     

    Abstract: Characteristics of concentration distribution of total dissolved iron and its correlation with organic matter and pH value in Songhua River and Heilongjiang River were studied.Results show that the concentrations of total dissolved iron ranged in 0.10-0.62 mg·L-1 in Heilongjiang River,and in 0.11-0.73 mg·L-1 in Songhua River.The mean concentrations of both total dissolved iron and ferrous iron in Songhua River were slightly higher than that in Heilongjiang River.Within a year,the peak concentrations of dissolved iron appeared mostly in the moderate flow period.A significant negative linear relationship was observed between CODCr and ferrous iron in Heilongjiang River,but a significant positive linear relationship between CODCr and total dissolved iron and significant negative linear relationships of ferrous iron with BOD5 and pH were observed in Songhua River.Input of hard-to-biodegrade organic substances from anthropogenic sources increases the concentrations of both total dissolved iron and organic-chelated iron.

     

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