几种冰川碳氢化合物的气溶胶来源

H. Wilson, R. Scuderi
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引用次数: 0

摘要

最近对冰雪的分析表明,在华盛顿北喀斯喀特山脉的许多冰川中都有碳氢化合物的痕迹。(史古德利,1980)。有机化合物全年在局部积雪上的收集缓慢,但在夏末消融面达到最大浓度约200-500 ng l -1。然而,在新鲜的冬季雪中,它们的浓度远低于100毫微克升。与植被区相邻的雪原通常异常富含碳氢化合物,通常为3-5毫克升,这可能是植物蒸气和碎屑积聚的结果。夏季在冰川表面聚集的薄膜被冬季的积雪所掩埋,成为冰川永久的地层特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Aerosol Sources of Some Types of Glacier Hydrocarbons
Recent analyses of ice and snow have shown that there are traces of hydrocarbons in many glaciers in the North Cascade mountains of Washington. (Scuderi, 1980). The organic compounds collect slowly throughout the year on topical snow, but they reach their maximal concentrations of about 200-500 ng liter-1 on late summer ablation surfaces. In fresh winter snow, however, their concentrations fall well below 100 ng liter-1. Snowfields adjacent to vegetated areas are often abnormally rich in hydrocarbons, typically 3-5 mg liter-1, probably as as a result of the accumulation of plant vapors and debris. Films that collect on the surfaces during the summer are buried by winter snows and become permanent stratigraphic features in the glaciers.
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