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首页> 外文期刊>Ground Water Monitoring & Remediation >Batch and Column Experiments to Support Heavy Metals (Cu, Zn, and Mn) Transport Modeling in Alluvial Sediments Between the Mogan Lake and the Eymir Lake, Goelbasi, Ankara
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Batch and Column Experiments to Support Heavy Metals (Cu, Zn, and Mn) Transport Modeling in Alluvial Sediments Between the Mogan Lake and the Eymir Lake, Goelbasi, Ankara

机译:分批和柱实验支持在Mogan湖和Eymir湖之间的冲积沉积物中重金属(Cu,Zn和Mn)迁移模型,Goalbasi,安卡拉

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摘要

This article describes laboratory batch sorption and column transport experiments that were conducted using heterogeneous alluvial sediments with a wide physical characteristic from wells, located between Lake Mogan and Lake Eymir, Golbasi, Ankara. The batch sorption experiment was conducted in two separate systems, that is, single and multicomponents. Single batch experiment was performed to determine equilibrium condition between the heavy metal ions and the soil adsorption sites. The sorption isotherms data from multibatch experiments were used to calculate the sorption parameters. Single batch experiment indicated that equilibrium was attained within 9 days from the start of the sorption test. As a result of multicomponents batch experiments, for Zn and Mn, the sorption process was well described by the Freundlich or Langmuir isotherm model, whereas sorption of Cu was better described by the linear isotherm model. The K_d of Cu were found to be highest in soil 1 (32550.350 L kg~(-1)) and lowest in soil 5 (18170.76 L kg~(-1))- The maximum and minimum sorption capacity values for Zn were found to be in soil 1 (10985.148 mg kg~(-1)) and in soil 2 (8597.14 mg kg~(-1)) units, respectively. [Correction added after online publication 15 July, 2010: In the preceding sentence, the words "minimum" and "maximum" were initially switched.] Similarly, soil 1 (7587.391 mg kg~(-1)) and soil 5 (4908.695 mg kg~(-1)) units provided the maximum and minimum values for Mn. In the column experiments, flow and tracer transport was studied under saturated conditions using conservative tracer to determine the transport parameters. Transport parameter values were obtained by curve-fitting using the nonlinear least-squares optimization code CXTFIT. Results of the column experiments indicated that the dispersivity values obtained for soil samples were in the range of 0.024 to 1.13 cm.
机译:本文介绍了实验室批吸附和柱传输实验,这些实验是使用位于莫干湖和安卡拉Golbasi的Eymir湖之间的具有广泛物理特征的非均质冲积沉积物进行的。分批吸附实验在两个独立的系统中进行,即单组分和多组分。进行单批实验以确定重金属离子与土壤吸附位点之间的平衡条件。来自多批次实验的吸附等温线数据用于计算吸附参数。单批实验表明从吸附测试开始的9天内达到平衡。作为多组分批处理实验的结果,对于锌和锰,吸附过程可以通过Freundlich或Langmuir等温线模型很好地描述,而对铜的吸附可以通过线性等温线模型更好地描述。铜的K_d在土壤1中最高(32550.350 L kg〜(-1)),在土壤5中最低(18170.76 L kg〜(-1))-锌的最大和最小吸附容量值分别在土壤1(10985.148 mg kg〜(-1))和土壤2(8597.14 mg kg〜(-1))单位中。 [在在线发布于2010年7月15日之后添加的更正:在前面的句子中,单词“ minimum”和“ maximum”最初被切换。]同样,土壤1(7587.391 mg kg〜(-1))和土壤5(4908.695 mg kg〜(-1))单位提供了Mn的最大值和最小值。在柱实验中,使用保守示踪剂在饱和条件下研究了流动和示踪剂的运输,以确定运输参数。通过使用非线性最小二乘最优化代码CXTFIT进行曲线拟合获得运输参数值。柱实验的结果表明,土壤样品的分散度值为0.024至1.13 cm。

著录项

  • 来源
    《Ground Water Monitoring & Remediation》 |2010年第3期|P.125-139|共15页
  • 作者

    E.Disli;

  • 作者单位

    Environmental Engineering Department, Faculty of Engineering-Architecture, Yuezuencue Yil University, Zeve Campus, Van, Turkey;

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  • 正文语种 eng
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