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Effect of solute size and mass transfer on transport of contaminants in porous media.

机译:溶质大小和传质对污染物在多孔介质中迁移的影响。

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摘要

Miscible displacement experiments were performed with solutes of different size and structure to examine their mass transfer, sorption, and transport in homogeneous and heterogeneous porous media. In homogeneous porous media, the contribution of axial diffusion becomes significant at pore-water velocities less than 0.1 cm/h, and the use of a tracer-derived dispersivity for solutes of different sizes would not be valid in this case. Comparison showed that dispersivities measured with a non-sorbing single-solute solution should be applicable to multi-component systems. Breakthrough curves exhibited both early breakthrough and tailing for solute transport in aggregated, stratified, and macroporous media. The extent of non-ideality was consistent with the impact of solute size on the relative degree of "non-equilibrium" experienced by solutes whose transport is constrained by diffusive mass transfer. Flow-interruption experiments with dual tracers of different size, performed for various interruption times, provided additional evidence regarding the effect of solute size on diffusive mass transfer. The relationship between sorbate structure and rate-limited sorption was examined using the QSAR (quantitative structure-activity relationship) approach for sorption of low-polarity compounds by two soils. The first-order valence molecular connectivity (¹xᵛ), accounting for the size and structure of the solutes, was found to be the best topological descriptor. This supports the contention that rate-limited sorption in these systems is analogous to the polymer diffusion model. Based on this model, the calculated diffusion-length ratios for two soils compare favorably to the values determined from the measured rate data. The synergistic effects of rate-limited sorption and mass transfer in heterogeneous porous media were examined. Independent predictions produced with the multiprocess non-equilibrium model (MPNE) provided very good descriptions of the experimental data for transport of several organic solutes with different solute structures in a saturated aggregated medium. The success of describing the mass transfer, rate-limited sorption, and transport of contaminants has important implications for understanding contaminant transport in the subsurface and for remediation practices of contaminated sites.
机译:用不同大小和结构的溶质进行了混溶驱替实验,以检查它们在均质和非均质多孔介质中的传质,吸附和迁移。在均质的多孔介质中,当孔隙水速度小于0.1 cm / h时,轴向扩散的作用变得显着,在这种情况下,对于不同大小的溶质使用示踪剂衍生的分散性将是无效的。比较表明,使用非吸附性单溶质溶液测得的分散度应适用于多组分系统。突破曲线显示了在聚集,分层和大孔介质中溶质的早期突破和拖尾现象。非理想程度与溶质尺寸对溶质所经历的“非平衡”相对程度的影响相一致,溶质的相对迁移程度受扩散传质的限制。在不同的中断时间使用不同大小的双示踪剂进行的流中断实验,提供了有关溶质大小对扩散传质影响的更多证据。使用QSAR(定量结构-活性关系)方法研究了两种土壤对低极性化合物的吸附情况,研究了吸附物结构与限速吸附之间的关系。发现溶质的大小和结构的一价化合价分子连接性(¹xᵛ)是最好的拓扑描述子。这支持了以下观点:在这些系统中限速吸附类似于聚合物扩散模型。基于该模型,计算出的两种土壤的扩散长度比与根据测得的速率数据确定的值相比具有优势。检查了异质多孔介质中限速吸附和传质的协同效应。用多过程非平衡模型(MPNE)产生的独立预测对饱和聚集介质中几种具有不同溶质结构的有机溶质的迁移提供了非常好的实验数据描述。描述污染物的传质,限速吸附和污染物转移的成功对理解地下污染物的转移以及污染场地的修复方法具有重要意义。

著录项

  • 作者

    Hu Qinhong.;

  • 作者单位
  • 年度 1995
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
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