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首页> 外文期刊>Journal of the Atmospheric Sciences >Predicting particle critical supersaturation from hygroscopic growth measurements in the humidified TDMA. Part II: Laboratory and ambient studies
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Predicting particle critical supersaturation from hygroscopic growth measurements in the humidified TDMA. Part II: Laboratory and ambient studies

机译:根据加湿的TDMA中的吸湿性生长预测值预测颗粒的临界过饱和度。第二部分:实验室和环境研究

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Laboratory studies are used to test the method proposed in Part I for estimating the critical supersaturation of quasi-monodisperse, dry particles from measurements of hygroscopic growth at relative humidities blow 100%. An advantage of the proposed technique is that it directly links dry particle size to cloud condensation nuclei (CCN) activity and simultaneously provides some information on particle chemical composition. Studies have been conducted on particles composed of NaCl, (NH4)(2)SO4, NH4HSO4, internally and externally mixed NaCl-(NH4)(2)SO4, and on ambient particles of unknown chemical composition. A modified form of the Kohler equation is fit to measurements from a humidified tandem differential mobility analyzer to derive two chemical composition-dependent parameters and the critical supersaturation for a given dry particle size. A cloud condensation nucleus counter is used to simultaneously observe the critical supersaturation of the same dry particles. Results show that for particles composed of single salts and for diameters between 32 and 57 nm, the average agreement between critical supersaturations derived from measurements of hygroscopic growth and theoretical values of S-crit is -13% (1 sigma = 8.5%, n = 9). This agreement is similar to experimental uncertainties in critical supersaturations determined from laboratory studies on particles of known chemical composition. The agreement between values of S-crit predicted by the fit technique and CCN study-derived values is poorer (-6% to -65%) for ambient particles. This is likely due to both changes in ambient particle characteristics during the study and limitations in the modified Kohler model derived in this work. [References: 22]
机译:实验室研究用于测试第一部分中提出的方法,该方法通过测量相对湿度100%的吸湿性来估算准单分散,干燥颗粒的临界过饱和度。提出的技术的一个优点是,它直接将干粒度与云凝结核(CCN)活性联系起来,同时提供了有关颗粒化学成分的一些信息。已经对由NaCl,(NH4)(2)SO4,NH4HSO4,内部和外部混合的NaCl-(NH4)(2)SO4组成的颗粒以及化学成分未知的环境颗粒进行了研究。科勒方程的修改形式适合于加湿串联差动迁移率分析仪的测量结果,以得出两个化学成分相关的参数以及给定干粒度的临界过饱和度。云凝结核计数器用于同时观察相同干燥颗粒的临界过饱和。结果表明,对于由单盐组成且直径在32至57 nm之间的颗粒,从吸湿性生长测量值得出的临界过饱和度与S临界值的理论值之间的平均一致性为-13%(1 sigma = 8.5%,n = 9)。该协议类似于通过对已知化学成分的颗粒进行的实验室研究确定的临界过饱和度的实验不确定性。对于周围粒子,通过拟合技术预测的S-crit值与CCN研究得出的值之间的一致性较差(-6%至-65%)。这很可能是由于研究过程中环境粒子特征的变化以及这项工作中得出的改进的科勒模型的局限性所致。 [参考:22]

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