生物质燃烧有机气溶胶的水溶性和不溶性多相处理

Habeeb H. Al-Mashala, Meredith Schervish, Sithumi M. Liyanage, Jace A. Barton, Manabu Shiraiwa and Elijah G. Schnitzler*, 
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引用次数: 0

摘要

生物质燃烧是大气中有机气溶胶最重要的来源之一。据观察,生物质燃烧产生的有机气溶胶(BBOA)会发生液-液相分离(LLPS),形成疏水相包裹亲水相的核壳形态,从而通过多相过程对光吸收成分(即褐碳(BrC))的演化产生潜在影响。在此,我们展示了 BBOA 的水溶性相(即亲水性相)和不溶性相(即疏水性相)在涂层壁流动管中对臭氧的反应性吸收方面的多相处理过程有何不同。研究了相对湿度(RH)和紫外线(UV)照射的影响。实验时间序列被用于多层动力学模型的模拟。在未经过辐照的薄膜中,水溶性相在相对湿度为 75% 时的吸收系数最大(3 × 10-5,对应的 BrC(DBrC)扩散系数为 3 × 10-9 cm2 s-1),而同一相在相对湿度为 0% 时的吸收系数最小(1 × 10-5,对应的 DBrC 扩散系数为 1 × 10-10 cm2 s-1)。水不溶性相的吸收系数介于两者之间(约 1.5 × 10-5),与相对湿度无关,相应的 DBrC 仅略有增加(0% 相对湿度时为 8 × 10-10 cm2 s-1,75% 相对湿度时为 9 × 10-10 cm2 s-1)。在紫外线照射后,两相在 0% 相对湿度下的吸收系数都显著下降,这与从粘性液体向固体的转变是一致的,并得到了定性显微镜观察的支持。大气中主要溴化碳成分的多相臭氧氧化模型显示,首先,在中等至高相对湿度条件下,液相-液相分离和紫外线照射可能会限制生物质燃烧有机气溶胶的多相处理,从而影响其气候效应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multiphase Processing of the Water-Soluble and Insoluble Phases of Biomass Burning Organic Aerosol

Biomass burning is one of the most significant sources of organic aerosol in the atmosphere. Biomass burning organic aerosol (BBOA) has been observed to undergo liquid–liquid phase separation (LLPS) to give core–shell morphology with the hydrophobic phase encapsulating the hydrophilic phase, potentially impacting the evolution of light-absorbing components, i.e., brown carbon (BrC), through multiphase processes. Here, we demonstrate how multiphase processing differs between the water-soluble (i.e., hydrophilic) and insoluble (i.e., hydrophobic) phases of BBOA in terms of reactive uptake of ozone in a coated-wall flow tube. Effects of relative humidity (RH) and ultraviolet (UV) irradiation were investigated. Experimental timeseries were used to inform simulations using multilayer kinetic modeling. Among non-irradiated thin films, the uptake coefficient was greatest for the water-soluble phase at 75% RH (3 × 10–5, corresponding to a diffusion coefficient of BrC, DBrC, of 3 × 10–9 cm2 s–1) and least for the same phase at 0% RH (1 × 10–5, corresponding to DBrC of 1 × 10–10 cm2 s–1). The uptake coefficient for the water-insoluble phase fell between these two (about 1.5 × 10–5), regardless of RH, and the corresponding DBrC increased only slightly (8 × 10–10 cm2 s–1 at 0% RH to 9 × 10–10 cm2 s–1 at 75% RH). The uptake coefficients of both phases at 0% RH decreased significantly after UV irradiation, consistent with a transition from viscous liquid to solid and supported by qualitative microscopy observations. Modeling multiphase ozone oxidation of primary BrC components in the atmosphere demonstrated, first, that LLPS may extend the lifetime of water-soluble BBOA encapsulated by water-insoluble species by a factor of 1.5 at moderate to high RH and, also, that UV irradiation may extend the lifetime of both phases by more than a factor of 2.5.

Liquid−liquid phase separation and ultraviolet irradiation may restrict the multiphase processing of biomass burning organic aerosol governing its climate effects.

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