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Glass formation and unusual hygroscopic growth of iodic acid solution droplets with relevance for iodine mediated particle formation in the marine boundary layer

机译:碘溶液滴的玻璃形成和异常吸湿性增长与海洋边界层中碘介导的颗粒形成有关

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Iodine oxide particles are known to nucleate in the marine boundary layerwhere gas phase molecular iodine and organoiodine species are produced bymacroalgae. These ultra-fine particles may then grow through the condensationof other materials to sizes where they may serve as cloud condensationnuclei. There has been some debate over the chemical identity of theinitially nucleated particles. In laboratory simulations, hygroscopicmeasurements have been used to infer that they are composed of insolubleI2O4, while elemental analysis of laboratory generated particlessuggests soluble I2O5 or its hydrated form iodic acid, HIO3(I2O5·H2O). In this paper we explore the response ofsuper-micron sized aqueous iodic acid solution droplets to varying humidityusing both Raman microscopy and single particle electrodynamic traps. Thesemeasurements reveal that the propensity of an iodic acid solution droplet tocrystallise is negligible on drying to ~0% relative humidity(RH). On applying mechanical pressure to these droplets they shatter in amanner consistent with an ultra-viscous liquid or a brittle glass. Waterretention in amorphous material at low RH is important for understanding thehygroscopic growth of aerosol particles and uptake of other condensablematerial. Subsequent water uptake between 10 and 20% RH causes theirviscosity to reduce sufficiently that the cracked droplets flow and merge.The persistence of iodic acid solution in an amorphous state, rather than acrystalline state, suggests they will more readily accommodate othercondensable material and are therefore more likely to grow to sizes wherethey may serve as cloud condensation nuclei. On increasing the humidity to~90% the mass of the droplets only increases by ~20%with a corresponding increase in radius of only 6%, which is remarkablysmall for a highly soluble material. We suggest that the small growth factorof aqueous iodic acid solution droplets is consistent with the small aerosolgrowth factors observed in previous experiments.
机译:已知氧化碘颗粒在海洋边界层中成核,在该边界层中由宏藻产生气相分子碘和有机碘物质。这些超细颗粒然后可以通过其他材料的凝结而生长到一定尺寸,在这些尺寸中它们可以充当云凝结核。关于初始成核颗粒的化学特性一直存在一些争论。在实验室模拟中,已使用吸湿测量法推断它们由不溶性I 2 O 4 组成,而实验室生成的颗粒的元素分析建议可溶I 2 O 5 或它的水合碘酸HIO 3 (I 2 O 5 ·H 2 O)。在本文中,我们使用拉曼显微镜和单粒子电动捕集阱,探索了超微尺寸的碘酸水溶液液滴对不同湿度的响应。这些测量结果表明,在干燥至〜0%相对湿度(RH)时,碘酸溶液液滴的结晶倾向可忽略不​​计。在对这些液滴施加机械压力时,它们会以与超粘液体或脆性玻璃一致的方式破碎。在低RH下,无定形材料中的保水性对于了解气溶胶颗粒的吸湿性增长和其他可凝结材料的吸收非常重要。随后在10%到20%RH之间吸水会导致其粘度降低到足以使破裂的液滴流动并融合的程度。碘酸溶液在非晶态而不是非晶态下的持久性表明它们将更容易容纳其他可凝结的物质,因此更易吸收可能会增长到可能充当云凝结核的大小。在将湿度增加到〜90%时,液滴的质量仅增加〜20%,相应的半径仅增加6%,这对于高度可溶的材料而言非常小。我们建议碘酸水溶液液滴的小生长因子与先前实验中观察到的小气溶胶生长因子一致。

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