COMSOL Multiphysics优化多孔涂层顶空固相微萃取干燥土壤样品中挥发性有机化合物

IF 0.3 Q4 CHEMISTRY, MULTIDISCIPLINARY Chemical Bulletin of Kazakh National University Pub Date : 2022-10-19 DOI:10.15328/cb1300
B. Kenessov, A. Kapar
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引用次数: 1

摘要

顶空固相微萃取(HSSPME)是测定土壤中挥发性有机物(VOCs)最简单、成本效益高的样品制备方法之一。本研究旨在开发使用COMSOL Multiphysics(CMP)通过多孔涂层对干燥土壤样品中挥发性有机化合物的HSSPME进行数值优化的模型稀释物种在多孔介质中的传输物理被用于建模。利用该模型研究了样品质量、压力、纤维顶部空间和土壤顶部空间分布常数对萃取剖面和95%平衡时间的影响。在大气压(1个大气压)下的平衡提取可能需要长达97分钟,而在真空(0.0313个大气压,2.3分钟)下。在所有研究的分布常数和样品质量下,真空下的平衡时间比1个大压力下低42-43倍。利用“稀释物种运输”物理学对开发的模型进行了修改,以优化预孵育时间。根据获得的曲线图,95%的平衡时间可以达到13.3分钟,这取决于样品质量和分析物的土壤顶部空间分布常数。当纤维顶部空间和土壤顶部空间分布常数、土壤孔隙度和密度已知时,所开发的模型可用于优化压力、预培养和提取时间。
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Optimization of headspace solid-phase microextraction of volatile organic compounds from dry soil samples by porous coatings using COMSOL Multiphysics
Headspace solid-phase microextraction (HSSPME) is one of the simplest and cost-efficient sample preparation approaches for determination of volatile organic compounds (VOCs) in soil. This study was aimed at the development of the model for numerical optimization of HSSPME of volatile organic compounds from dry soil samples by porous coatings using COMSOL Multiphysics (CMP). ‘Transport of Diluted Species in Porous Medium’ physics was used for modeling. Effect of sample mass, pressure, fiber-headspace and soil-headspace distribution constants on extraction profiles and time of 95% equilibrium has been studied using the developed model. Equilibrium extraction under atmospheric pressure (1 atm) can take up to 97 min, while under vacuum (0.0313 atm) – 2.3 min. Equilibration time under vacuum was 42-43 times lower than under 1 atm at all studied distribution constants and sample masses. The developed model was modified for optimization of pre-incubation time using ‘Transport of Diluted Species’ physics. According to the obtained plots, 95% equilibration time can reach 13.3 min and depends on both sample mass and soil-headspace distribution constant of the analyte. The developed model can be recommended for optimization of pressure, preincubation and extraction time when fiber-headspace and soil-headspace distribution constants, soil porosity and density are known.
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