首页> 外文会议>First International Conference on Remediation of Contaminated Sediments S1-1, Oct 10-12, 2001, Venice Italy >A DIFFERENTIAL HYSTERESIS COEFFICIENT FOR CHARACTERIZING THE ADSORPTIVE-DESORPTIVE BEHAVIOUR OF CONTAMINANTS IN SEDIMENTS
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A DIFFERENTIAL HYSTERESIS COEFFICIENT FOR CHARACTERIZING THE ADSORPTIVE-DESORPTIVE BEHAVIOUR OF CONTAMINANTS IN SEDIMENTS

机译:表征污染物在污染物中的吸附-去吸附行为的微分滞回系数

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In this work, a new hysteresis coefficient is proposed and its usefulness for determining the adsorption-desorption behavior of pollutants on sediments and soils is examined. In sediment pollution and remediation, the adsorption and desorption play a key role on pollutants availability and transport. For several pollutants and solid matrices such as sediments, the desorption pathway is different from that of the adsorption. This phenomenon is known as hysteresis. Here, we define a hysteresis coefficient CH as the ratio of the slope (derivative) of the adsorption curve and the slope of the desorption curve in a given point (C_j, q_j) of interest. We demonstrate that: ⅰ) CH is dimensionless; ⅱ) when hysteresis is not important, CH=1, i.e., the adsorption is reversible; ⅲ) when hysteresis is important, CH>1, i.e., the adsorption is irreversible; ⅳ) the greater the hysteresis, the greater the CH; ⅴ) the CH can be determined at any convenient point (C_j, q_j) of interest of the adsorption curve, peforming a few consecutive desorption steps, and there is no need to determine the full adsorption-desorption cycle; ⅵ) the CH is consistent (i.e. C_H ≥1) for the most common isotherm models (linear, Freundlich and Langmuir); ⅶ) there exist also analytical, particular, simple equations for finding CH for the linear, Freundlich and Langmuir isotherm models; ⅷ) the CH shows several advantages over the well known hysteresis indices defined by Huang and Weber (1997) and Ma et al. (1993). Using experimental data from refereed literature, we also show that the CH provides a quantitative basis for ⅰ) comparing the irreversibility of the adsorption of different individual pollutants on a given soil; ⅱ) comparing the irreversibility of the adsorption of a given pollutant on different soils; ⅲ) determining the effect of aging and weathering on adsorption irreversibility. Overall, the CH allows for the quantitative determination of pollutant availability and this, in turn, could be a valuable tool for estimating the remediation potential of polluted sediments.
机译:在这项工作中,提出了一个新的滞后系数,并研究了其在确定污染物在沉积物和土壤上的吸附-解吸行为的实用性。在沉积物污染和修复中,吸附和解吸对污染物的利用和运输起着关键作用。对于几种污染物和固体基质(如沉淀物),其解吸途径与吸附途径不同。这种现象称为磁滞现象。在此,我们将磁滞系数CH定义为感兴趣的给定点(C_j,q_j)上吸附曲线的斜率(导数)与解吸曲线的斜率之比。我们证明:ⅰ)CH是无量纲的; ⅱ)当磁滞不重要时,CH = 1,即吸附是可逆的; ⅲ)当磁滞很重要时,CH> 1,即吸附是不可逆的; ⅳ)磁滞越大,CH越大; ⅴ)可以在吸附曲线上感兴趣的任何方便点(C_j,q_j)上确定CH,执行几个连续的解吸步骤,而无需确定整个吸附-解吸循环; ⅵ)对于最常见的等温模型(线性,Freundlich和Langmuir),CH是一致的(即C_H≥1); ⅶ)还有线性的,Freundlich和Langmuir等温线模型的寻找CH的解析的,特别的简单方程; ⅷ)CH显示出优于Huang和Weber(1997)和Ma等人所定义的众所周知的磁滞指数的几个优点。 (1993)。使用参考文献中的实验数据,我们还表明CH为ⅰ)比较了给定土壤上不同污染物的吸附的不可逆性提供了定量基础。 ⅱ)比较给定污染物在不同土壤上的吸附的不可逆性; ⅲ)确定老化和风化对吸附不可逆性的影响。总体而言,CH可以定量确定污染物的可利用量,这反过来又可以成为估算污染沉积物修复潜力的有价值的工具。

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