Department of Geology and Environmental Earth Science, Shideler Hall, Miami University, Oxford, OH, 45056, USA.
Department of Geology and Environmental Earth Science, Shideler Hall, Miami University, Oxford, OH, 45056, USA.
Environ Res. 2021 Mar;194:110619. doi: 10.1016/j.envres.2020.110619. Epub 2020 Dec 27.
The uranium boom in the United States from the 1940's to the 1980's was a period of extensive uranium mining on Native American lands. However, detailed environmental investigations of the resulting uranium pollution are sparse and typically ignore contributions from airborne particulate matter. The Midnite Mine is a 350-acre inactive open pit uranium mine located on the Spokane Indian Reservation in eastern Washington that operated from 1954 to 1981. Approximately 2.4 million tons of ore and 33 million tons of waste rock were left behind in stockpiles and have also been utilized as gravel on access and haul roads. Although the Midnite Mine is now a Superfund Site, and governmental investigations of water and soil contamination have been done, no investigations of airborne particulate matter pollution have been conducted. This study applies tree bark from 31 Pinus ponderosa trees as a biomonitor of this airborne particulate matter. Bulk trace elemental analyses via inductively coupled plasma - mass spectrometry (ICP-MS) of tree bark show that U is the most abundant trace element of interest present up to 232 ppb. Other metals that are of potential human health concern include Th, Pb, and As which are present at 20 ppb, 104 ppb, and 20 ppb respectively. Calculated geoaccumulation indices determine these metals to be at high (U), moderate (Th), and low (Pb and As) levels of contamination. Detailed scanning electron microscopy (SEM) investigations of particulate matter from the surface of tree bark confirm that U and Th-bearing particulate matter exist in the <PM size fraction while geospatial analyses indicate that uranium, thorium, and arsenic contamination are centralized along the Midnite Mine access road and at the nearby Dawn Mill where ore was further processed. Combined, these findings indicate that the nature and distribution of historic airborne particulate matter from the Midnite Mine and Dawn Mill provide context for potentially understanding past and current illness on the reservation. In addition, much needed context for future health and environmental studies for both local and national Native American populations is provided.
美国从 20 世纪 40 年代到 80 年代的铀繁荣时期是在美洲原住民土地上广泛开采铀的时期。然而,对由此产生的铀污染的详细环境调查很少,而且通常忽略了空气中颗粒物的贡献。Midnite 矿是一个位于华盛顿东部斯波坎印第安人保留地的 350 英亩的废弃露天铀矿,从 1954 年到 1981 年运营。大约 240 万吨矿石和 3300 万吨废石被留在了堆存场,也被用作进入和运输道路的砾石。尽管 Midnite 矿现在是一个超级基金站点,政府已经对水和土壤污染进行了调查,但没有对空气中颗粒物污染进行调查。本研究应用 31 株黄松的树皮作为空气中颗粒物的生物监测器。通过电感耦合等离子体质谱法(ICP-MS)对树皮的痕量元素进行批量分析,结果表明 U 是最丰富的痕量元素,含量高达 232ppb。其他对人类健康有潜在关注的金属包括 Th、Pb 和 As,它们的含量分别为 20ppb、104ppb 和 20ppb。计算的地质累积指数确定这些金属的污染程度为高(U)、中(Th)和低(Pb 和 As)。对树皮表面颗粒物的详细扫描电子显微镜(SEM)研究证实,U 和 Th 含颗粒物存在于<PM 粒径范围内,而地理空间分析表明,铀、钍和砷的污染集中在 Midnite 矿的入口道路沿线和附近的 Dawn 磨矿厂,那里进一步加工了矿石。综合这些发现表明,从中提取的历史空气中颗粒物的性质和分布为了解保留地过去和现在的疾病提供了背景。此外,为当地和全国的美洲原住民群体提供了未来健康和环境研究急需的背景。