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SAWNUC模型与硫酸-水成核的CLOUD测量结果的比较。

Comparison of the SAWNUC model with CLOUD measurements of sulphuric acid-water nucleation.

作者信息

Ehrhart Sebastian, Ickes Luisa, Almeida Joao, Amorim Antonio, Barmet Peter, Bianchi Federico, Dommen Josef, Dunne Eimear M, Duplissy Jonathan, Franchin Alessandro, Kangasluoma Juha, Kirkby Jasper, Kürten Andreas, Kupc Agnieszka, Lehtipalo Katrianne, Nieminen Tuomo, Riccobono Francesco, Rondo Linda, Schobesberger Siegfried, Steiner Gerhard, Tomé António, Wimmer Daniela, Baltensperger Urs, Wagner Paul E, Curtius Joachim

机构信息

Goethe University FrankfurtInstitute for Atmospheric and Environmental SciencesFrankfurt am MainGermany; CERNGenevaSwitzerland.

Goethe University FrankfurtInstitute for Atmospheric and Environmental Sciences Frankfurt am Main Germany; Now at Institute for Atmospheric and Climate Science ETH Zurich Zürich Switzerland.

出版信息

J Geophys Res Atmos. 2016 Oct 27;121(20):12401-12414. doi: 10.1002/2015JD023723.

Abstract

Binary nucleation of sulphuric acid-water particles is expected to be an important process in the free troposphere at low temperatures. SAWNUC (Sulphuric Acid Water Nucleation) is a model of binary nucleation that is based on laboratory measurements of the binding energies of sulphuric acid and water in charged and neutral clusters. Predictions of SAWNUC are compared for the first time comprehensively with experimental binary nucleation data from the CLOUD chamber at European Organization for Nuclear Research. The experimental measurements span a temperature range of 208-292 K, sulphuric acid concentrations from 1·10 to 1·10 cm, and distinguish between ion-induced and neutral nucleation. Good agreement, within a factor of 5, is found between the experimental and modeled formation rates for ion-induced nucleation at 278 K and below and for neutral nucleation at 208 and 223 K. Differences at warm temperatures are attributed to ammonia contamination which was indicated by the presence of ammonia-sulphuric acid clusters, detected by an Atmospheric Pressure Interface Time of Flight (APi-TOF) mass spectrometer. APi-TOF measurements of the sulphuric acid ion cluster distributions ( (H2SO4)i·HSO4- with i = 0, 1, ..., 10) show qualitative agreement with the SAWNUC ion cluster distributions. Remaining differences between the measured and modeled distributions are most likely due to fragmentation in the APi-TOF. The CLOUD results are in good agreement with previously measured cluster binding energies and show the SAWNUC model to be a good representation of ion-induced and neutral binary nucleation of sulphuric acid-water clusters in the middle and upper troposphere.

摘要

硫酸-水粒子的二元成核预计是低温下自由对流层中的一个重要过程。SAWNUC(硫酸-水成核)是一种基于实验室对带电和中性团簇中硫酸与水结合能测量的二元成核模型。首次将SAWNUC的预测与欧洲核子研究组织CLOUD室的实验二元成核数据进行了全面比较。实验测量的温度范围为208 - 292K,硫酸浓度为1·10至1·10个/cm,并且区分了离子诱导成核和中性成核。在278K及以下的离子诱导成核以及208K和223K的中性成核的实验和模型形成速率之间,发现了在5倍因子范围内的良好一致性。温暖温度下的差异归因于氨污染,这通过大气压界面飞行时间(APi - TOF)质谱仪检测到的氨 - 硫酸团簇的存在得以表明。APi - TOF对硫酸离子团簇分布((H2SO4)i·HSO4-,i = 0, 1, ..., 10)的测量与SAWNUC离子团簇分布显示出定性一致性。测量和模型分布之间的剩余差异很可能是由于APi - TOF中的碎片化。CLOUD结果与先前测量的团簇结合能良好一致,并表明SAWNUC模型是对流层中层和上层中硫酸 - 水团簇离子诱导和中性二元成核的良好代表。

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