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Physical and chemical characterization of bioaerosols — Implications for nucleation processes

机译:生物气溶胶的物理和化学特征—对成核过程的影响

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The importance of organic compounds in the oxidative capacity of the atmosphere, and as cloud condensation and ice-forming nuclei, has been recognized for several decades. Organic compounds comprise a significant fraction of the suspended matter mass, leading to local (e.g. toxicity, health hazards) and global (e.g. climate change) impacts. The state of knowledge of the physical chemistry of organic aerosols has increased during the last few decades. However, due to their complex chemistry and the multifaceted processes in which they are involved, the importance of organic aerosols, particularly bioaerosols, in driving physical and chemical atmospheric processes is still very uncertain and poorly understood. Factors such as solubility, surface tension, chemical impurities, volatility, morphology, contact angle, deliquescence, wettability, and the oxidation process are pivotal in the understanding of the activation processes of cloud droplets, and their chemical structures, solubilities and even the molecular configuration of the microbial outer membrane, all impact ice and cloud nucleation processes in the atmosphere. The aim of this review paper is to assess the current state of knowledge regarding chemical and physical characterization of bioaerosols with a focus on those properties important in nucleation processes. We herein discuss the potential importance (or lack thereof) of physical and chemical properties of bioaerosols and illustrate how the knowledge of these properties can be employed to study nucleation processes using a modeling exercise. We also outline a list of major uncertainties due to a lack of understanding of the processes involved or lack of available data. We will also discuss key issues of atmospheric significance deserving future physical chemistry research in the fields of bioaerosol characterization and microphysics, as well as bioaerosol modeling. These fundamental questions are to be addressed prior to any definite conclusions on the potential significance of the role of bioaerosols on physico-chemical atmospheric processes and that of climate.
机译:几十年来,人们已经认识到有机化合物在大气氧化能力中以及作为云凝结和冰核形成的重要性。有机化合物占悬浮物质量的很大一部分,导致局部(例如毒性,健康危害)和全球(例如气候变化)影响。在过去的几十年中,对有机气溶胶的物理化学的了解有所增加。但是,由于它们复杂的化学作用和涉及的多方面过程,有机气溶胶,特别是生物气溶胶在驱动物理和化学大气过程中的重要性仍然是非常不确定的,人们对此知之甚少。诸如溶解度,表面张力,化学杂质,挥发性,形态,接触角,潮解性,润湿性和氧化过程等因素对于理解云滴的活化过程及其化学结构,溶解度甚至分子构型至关重要在微生物外膜中,所有物质都会影响大气中的冰和云成核过程。本文的目的是评估有关生物气溶胶化学和物理表征的当前知识状态,重点关注成核过程中重要的那些特性。我们在此讨论生物气溶胶的物理和化学性质的潜在重要性(或缺乏其重要性),并说明如何使用建模练习将这些性质的知识用于研究成核过程。由于缺乏对所涉及流程的了解或缺乏可用数据,我们还列出了主要的不确定性清单。我们还将讨论对大气有意义的关键问题,值得在生物气溶胶表征和微观物理学以及生物气溶胶建模领域进行未来的物理化学研究。在就生物气溶胶对理化大气过程和气候的作用的潜在意义作出任何明确结论之前,必须解决这些基本问题。

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