极地冰雪电荷及其对大气化学的潜在影响

IF 2.8 Q3 ENVIRONMENTAL SCIENCES Environmental science: atmospheres Pub Date : 2024-01-20 DOI:10.1039/D3EA00084B
Kateryna Tkachenko and Hans-Werner Jacobi
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引用次数: 0

摘要

冰-水汽界面带电是冰物理学和大气电化研究的一个重要课题。然而,在研究极地地区雪的化学过程时,尚未考虑这些效应,因为迄今为止,冰表面的电势被认为不足以引发化学反应和化学过程。在本综述中,我们分析了文献数据,以估算地球表面发生的不同过程可能导致的雪和其他冰冻物体的电化水平。分析表明,在不同气象和物理过程的共同作用下,电场强度可能会超过电晕放电的临界值,甚至会形成瑞利喷流。电荷的积累会导致不同的化学变化,如电渗现象或大气中的杂质在生长的冰晶中积累。此外,作为 "热点 "出现并在微秒内消散的高能状态有可能引发自由基过程,甚至产生带电气溶胶。综述还详细讨论了部分实地观测结果,指出电荷驱动的过程如何有助于解释这些观测结果,这些观测结果至少部分与我们目前对冰雪化学的理解不一致。最后,还介绍了在实地和实验室实验中研究这些效应的一些方法。在冰物理和雪化学的交叉领域进一步发展这一新领域,对于更好地理解与冰冻圈有关的化学过程似乎大有希望。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Electrical charging of snow and ice in polar regions and the potential impact on atmospheric chemistry

Charging of the ice–vapor interface is a well-studied topic in ice physics and atmospheric electrification. However, these effects were not yet considered to examine chemical processes in snow in polar regions because electric potentials at ice surfaces have so far been considered insufficient to initiate chemical reactions and processes. In this review, we analyze literature data to estimate levels of electrification in snow and other frozen objects that can be caused by different processes occurring at the Earth's surface. This analysis demonstrates that threshold values of electric field strength can be exceeded for the appearance of corona discharges and even for the formation of Rayleigh jets due to combined effects of different meteorological and physical processes. The accumulation of electrical charges can lead to different chemical modifications such as electroosmotic phenomena or the accumulation of impurities from the atmosphere in growing ice crystals. Moreover, highly energetic states that occur and dissipate in microseconds as “hot spots” have the potential to initiate free radical processes and even the production of charged aerosols. The review also discusses in detail selected field observations to point out how processes driven by electrical charging may help to interpret these observations, which are at least partly inconsistent with our present understanding of snow and ice chemistry. Finally, some approaches are presented how these effects can be studied in field and laboratory experiments. A further development of this new field at the intersection of ice physics and snow chemistry seems very promising for a better understanding of relevant chemical processes related to the cryosphere.

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