Geological Survey of Canada , Natural Resources Canada , 601 Booth St. , Ottawa , Ontario K1A 0E8 , Canada.
Center for Earth Observation Science and Department of Environment and Geography , University of Manitoba , Winnipeg , Manitoba R3T 2N2 , Canada.
Environ Sci Technol. 2018 Oct 16;52(20):11466-11477. doi: 10.1021/acs.est.8b01246. Epub 2018 Oct 3.
In support of international efforts to reduce mercury (Hg) exposure in humans and wildlife, this paper reviews the literature concerning global Hg emissions, cycling and fate, and presents revised global and oceanic Hg budgets for the 2018 United Nations Global Mercury Assessment. We assessed two competing scenarios about the impacts of 16th - late 19th century New World silver (Ag) mining, which may be the largest human source of atmospheric Hg in history. Consideration of Ag ore geochemistry, historical documents on Hg use, and comparison of the scenarios against atmospheric Hg patterns in environmental archives, strongly support a "low mining emission" scenario. Building upon this scenario and other published work, the revised global budget estimates human activities including recycled legacy emissions have increased current atmospheric Hg concentrations by about 450% above natural levels (prevailing before 1450 AD). Current anthropogenic emissions to air are 2.5 ± 0.5 kt/y. The increase in atmospheric Hg concentrations has driven a ∼ 300% average increase in deposition, and a 230% increase in surface marine waters. Deeper marine waters show increases of only 12-25%. The overall increase in Hg in surface organic soils (∼15%) is small due to the large mass of natural Hg already present from rock weathering, but this figure varies regionally. Specific research recommendations are made to reduce uncertainties, particularly through improved understanding of fundamental processes of the Hg cycle, and continued improvements in emissions inventories from large natural and anthropogenic sources.
为支持国际减少人类和野生动物汞(Hg)暴露的努力,本文回顾了有关全球 Hg 排放、循环和归宿的文献,并为 2018 年联合国全球汞评估提供了修订后的全球和海洋 Hg 预算。我们评估了关于 16 世纪至 19 世纪晚期新大陆银(Ag)矿冶影响的两种相互竞争的情景,这可能是历史上人为向大气中排放 Hg 的最大来源。考虑到 Ag 矿石地球化学、Hg 使用的历史文献以及情景与环境档案中大气 Hg 模式的比较,强烈支持“低采矿排放”情景。在此情景的基础上,并结合其他已发表的研究,修订后的全球预算估计,包括再循环的历史遗留排放在内的人类活动使当前大气 Hg 浓度比自然水平(1450 年以前)高出约 450%。目前向大气排放的人为 Hg 为 2.5±0.5kt/y。大气 Hg 浓度的增加导致沉积量平均增加了约 300%,海洋表面水体增加了 230%。深海水体的增加仅为 12-25%。由于岩石风化产生的大量天然 Hg 已经存在,因此表层有机土壤中 Hg 总增加量(约 15%)较小,但这一数字在不同地区有所不同。本文提出了具体的研究建议,以减少不确定性,特别是通过更好地了解 Hg 循环的基本过程,以及继续改进来自大型自然和人为源的排放清单。