首页> 外文期刊>Journal of Aerosol Science >Adsorption of nitrogen and water vapor by insoluble particles and the implication on cloud condensation nuclei activity
【24h】

Adsorption of nitrogen and water vapor by insoluble particles and the implication on cloud condensation nuclei activity

机译:不溶性颗粒对氮和水蒸气的吸附及其对云凝结核活性的影响

获取原文
获取原文并翻译 | 示例
           

摘要

The adsorption parameters of three insoluble species, black carbon, kaolinite and montmorillonite particles were measured using an accelerated surface area and porosimetry system with nitrogen and water molecules as adsorbates to estimate the ability of insoluble species to act as cloud condensation nuclei (CCN). The surface area of adsorbents was determined using the Brunauer-Emmett-Teller (BET) isotherm analysis and further incorporated in Frenkel-Halsey-Hill (FHH) isotherm analysis to illustrate the multilayer adsorption process at high saturation conditions. The derived BET adsorption parameters suggest a higher multilayer adsorption at surface coverage (theta)=1 for water adsorption than N-2 adsorption, i.e., 24 +/- 2% vs 8 +/- 3%. The water adsorption on carbon surface showed no consistent trend for the BET isotherm possibly due to the hydrophobic properties. However, for water saturation (S) in the range of 0.4-0.9, all three components followed a good FHH isotherm trend. The required supersaturation (SSc) to form CCN using the FHH-adsorption activation theory showed a lower criterion for montmorillonite by 0.05-03% than that for black carbon and kaolinite. The equivalent hygroscopicity parameters, kappa, was estimated as similar to 0.002 for montmorillonite and less than 0.001 for both black carbon and kaolinite at a dry diameter of 200 nm. The results suggested that montmorillonite is a better CCN than the other two species. In addition to the adsorption parameter determination, the surface coverage was revised using the original definition and showed a higher required supersaturation than the simplified formula which was applied in earlier studies. Such deviation is more significant for composition having higher hygroscopicity and suggests the possible overestimation of CCN activation using the simplified equation, commonly applied in most studies. (C) 2015 Elsevier Ltd. All rights reserved.
机译:使用氮和水分子作为被吸附物的加速表面积和孔隙率法测量了三种不溶物的吸附参数,即黑碳,高岭石和蒙脱土,以估算不溶物作为云凝结核(CCN)的能力。吸附剂的表面积使用Brunauer-Emmett-Teller(BET)等温线分析法确定,并进一步纳入Frenkel-Halsey-Hill(FHH)等温线分析法中,以说明在高饱和条件下的多层吸附过程。得出的BET吸附参数表明,水吸附的表面覆盖度(θ)= 1比N-2吸附的多层吸附更高,即24 +/- 2%对8 +/- 3%。碳表面上的水吸附对于BET等温线没有显示出一致的趋势,这可能是由于疏水性造成的。但是,对于0.4至0.9范围内的水饱和度(S),所有三个分量均遵循良好的FHH等温线趋势。根据FHH吸附活化理论,形成CCN所需的过饱和度(SSc)显示,蒙脱石的标准比黑碳和高岭石的标准低0.05-03%。在200 nm的干燥直径下,蒙脱石的等效吸湿参数kappa估计为0.002,黑碳和高岭石的吸湿参数均小于0.001。结果表明,蒙脱石比其他两种物种具有更好的CCN。除了确定吸附参数外,还使用原始定义修改了表面覆盖率,并显示出比早期研究中使用的简化公式更高的所需过饱和度。对于具有较高吸湿性的组合物而言,这种偏差更为显着,并表明使用大多数研究中普遍使用的简化公式可能会高估CCN的活化作用。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号