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Assessing sequestration of selected polycyclic aromatic hydrocarbons by use of adsorption modeling and temperature-programmed desorption

机译:使用吸附模型和程序升温脱附技术评估选定的多环芳烃的螯合

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Sequestration of phenanthrene and pyrene was investigated in two soils-a sandy soil designated SBS and a silt-loam designated LHS-by combining long-term batch sorption studies with thermal desorption and pyrolysis of amended soil samples. The Polanyi-based adsorption volume and the adsorbed solute mass increased with aging for both soils, thus demonstrating the mechanism for observed sequestration. Despite rigorous thermal analysis, 30-62% (SBS sand) and 8-30% (LHS silt-loam) of phenanthrene could not be recovered after 30-270 days of sorption, with the increase in desorption resistance showing greater significance in SBS sand. For both soils, these values were 20-65% of adsorbed phenanthrene mass. Activation energies estimated from the temperature-programmed desorption (TPD) of sorbed phenanthrene at <= 375 degrees C were 51-53 kJ/mol, consistent with values derived for desorption of organic compounds from humic materials. The activated first-order model fitting of observed TPD data supports the conclusion that the desorption-resistant fraction of phenanthrene has become sequestered onto condensed organic domains and requires temperatures exceeding 600 degrees C to be released. The work demonstrates the use of thermal analysis in complementing the Polanyi-based adsorption modeling approach for assessing the mechanistic basis for sequestration of organic contaminants in soils.
机译:通过将长期分批吸附研究与修正后的土壤样品的热脱附和热解相结合,研究了两种土壤中的菲和quest的螯合情况(一种称为SBS的沙土和一种名为LHS的粉质壤土)。对于两种土壤,基于波兰尼的吸附量和吸附的溶质均随老化而增加,从而证明了观察到的螯合机理。尽管进行了严格的热分析,但在吸附30-270天后仍无法回收30-62%(SBS砂)和8-30%(LHS淤泥壤土)的菲,而抗吸附性的提高在SBS砂中显示出更大的意义。 。对于两种土壤,这些值都是吸附的菲质量的20-65%。根据吸附的菲在375°C以下的程序升温解吸(TPD)估算的活化能为51-53 kJ / mol,与从腐殖质材料中解吸有机化合物得出的值一致。激活的对TPD数据进行的一阶模型拟合证明了菲的抗解吸分数已被隔离在缩合的有机区域中,并且需要释放超过600摄氏度的温度,这一结论得到了支持。这项工作证明了热分析在补充基于波兰尼的吸附建模方法方面的应用,以评估土壤中有机污染物的固存机理。

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