Pollution of the snow surface with polycyclic aromatic hydrocarbons during the formation of frost

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY
M. Tentyukov, D. N. Gabov, D. Simonenkov, E. Yazikov
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引用次数: 1

Abstract

When analyzing chemical compositions of snow the high variability of content of polycyclic aromatic hydrocarbons (PAHs) in snow cover between snowfalls is observed. Researchers explain this by concentrating of snow. However, another mechanism of atmospheric contamination of the snow cover surface is possible. It may be a precipitation of fine crystals of PAHs from the atmosphere in the composition of cryohydrates, which can form aerogenic anomalies on the snow surface at formation of hoarfrost. The process starts in the atmosphere during the interaction of finely dispersed crystals of PAHs with cloud supercooled drops. This results in the cryogenic concentration of solid particles of PAHs by way of formation of solid eutectic mixture – cryohydrates, which are a two-phase system consisting of a fine mixture of crystals of solid particles and ice. Evidence of their manifestation is the presence of the Forel hatching on the surface of the facets of the hoarfrost crystals appearing due to the different optical density of alternating zones, which consist of interpenetrating domains of crystallized solid aerosols and ice. At the same time, due to the presence of temperature inversion over the snow cover and its drying effect on the near-snow layer of air, a stable mass transport of water vapor down to the snow cover is formed, which can initiate the flow of fine cryohydrates from the PAHs. Therefore, the growth of atmospheric ice crystals, begun in the surface atmosphere, continues on the snow surface during formation of hoarfrost, thus creating a special nano-relief of snow cover. The paper presents the results of observations of changes in the concentration of individual PAHs in the upper 18 mm layer of snow at accumulation of the surface hoarfrost during a long period between snowfalls. Some micro-morphological features of the forms of skeletal rime micro-crystals are shown, with which an increase in the nano-roughness of the snow surface is associated, as well as the manifestation of the signal of the aerogenic PAH anomaly on the snow surface. Since the conditions for the formation of surface hoarfrost occur more often than for snowfalls, the hoarfrost may be an informative object of testing when detecting hydrocarbon contamination of snow cover during the intervals between snowfalls.
结霜过程中多环芳烃对雪表面的污染
在积雪化学成分分析中,发现积雪中多环芳烃(PAHs)含量在降雪之间具有较高的变异性。研究人员通过集中雪来解释这一点。然而,积雪表面大气污染的另一种机制是可能的。它可能是大气中多环芳烃的细晶以冻水化合物的形式析出,在霜形成时可在雪面形成气成异常。这一过程始于大气中精细分散的多环芳烃晶体与云过冷液滴的相互作用。这导致多环芳烃的固体颗粒通过形成固体共晶混合物-低温水合物的方式低温浓缩,这是一种由固体颗粒和冰的晶体的精细混合物组成的两相体系。它们表现的证据是,由于交替区不同的光学密度而出现的白霜晶体表面上的佛瑞尔孵化的存在,这是由结晶固体气溶胶和冰的互穿域组成的。同时,由于积雪上逆温的存在及其对近雪层空气的干燥作用,形成了稳定的水汽向积雪的大量输送,这可以启动多环芳烃中细冷冻水合物的流动。因此,在霜的形成过程中,从地表大气开始的大气冰晶的生长在雪表面继续,从而形成一种特殊的纳米积雪浮雕。本文介绍了在长时间的降雪间隔期间,对地表霜冻积累过程中18 mm积雪上层各多环芳烃浓度变化的观测结果。骨霜微晶形态的一些微观形态特征与雪表面纳米粗糙度的增加有关,也与雪表面气源性多环芳烃异常信号的表现有关。由于地表白霜形成的条件比降雪发生的条件更频繁,因此在降雪间隔期间检测积雪的碳氢化合物污染时,白霜可以作为检测的信息对象。
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来源期刊
Led i Sneg-Ice and Snow
Led i Sneg-Ice and Snow GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.50
自引率
42.90%
发文量
11
审稿时长
8 weeks
期刊介绍: The journal was established with the aim of publishing new research results of the Earth cryosphere. Results of works in physics, mechanics, geophysics, and geochemistry of snow and ice are published here together with geographical aspects of the snow-ice phenomena occurrence in their interaction with other components of the environment. The challenge was to discuss the latest results of investigations carried out on Russia’s territory and works performed by Russian investigators together with foreign colleagues. Editorial board works in collaboration with Glaciological Association that is professional community of specialists in glaciology from all republics of the Former Soviet Union which are now new independent states. The journal serves as a platform for the presentation and discussion of new discoveries and results which help to elucidate the state of the Earth’s cryosphere and the characteristics of the evolution of the snow-ice processes and phenomena under the current conditions of rapid climate change.
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