Department of Chemistry, Tufts University, Medford, Massachusetts 02155, USA.
Environ Sci Technol. 2010 Apr 1;44(7):2360-4. doi: 10.1021/es9033606.
In the past few years, it has become increasingly apparent that perchlorate (ClO(4)(-)) is present on all continents, except the polar regions where it had not yet been assessed, and that it may have a significant natural source. Here, we report on the discovery of perchlorate in soil and ice from several Antarctic Dry Valleys (ADVs) where concentrations reach up to 1100 microg/kg. In the driest ADV, perchlorate correlates with atmospherically deposited nitrate. Far from anthropogenic activity, ADV perchlorate provides unambiguous evidence that natural perchlorate is ubiquitous on Earth. The discovery has significant implications for the origin of perchlorate, its global biogeochemical interactions, and possible interactions with the polar ice sheets. The results support the hypotheses that perchlorate is produced globally and continuously in the Earth's atmosphere, that it typically accumulates in hyperarid areas, and that it does not build up in oceans or other wet environments most likely because of microbial reduction on a global scale.
在过去的几年中,人们越来越明显地认识到,除了尚未进行评估的极地地区外,高氯酸盐(ClO4-)存在于所有大陆上,并且它可能有一个重要的自然来源。在这里,我们报告了在几个南极干旱谷(ADV)的土壤和冰中发现高氯酸盐的情况,其浓度高达 1100μg/kg。在最干燥的 ADV 中,高氯酸盐与大气中沉积的硝酸盐相关。远离人类活动的 ADV 高氯酸盐提供了明确的证据,表明地球上普遍存在天然高氯酸盐。这一发现对高氯酸盐的起源、其全球生物地球化学相互作用以及与极地冰盖的可能相互作用具有重要意义。研究结果支持了以下假设,即在地球大气中全球范围内持续产生高氯酸盐,它通常在极度干旱地区积累,并且由于全球范围内的微生物还原作用,它不会在海洋或其他潮湿环境中积累。