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ACS Earth Space Chem. 2021 Feb 18;5(2):356-364. doi: 10.1021/acsearthspacechem.0c00326. Epub 2021 Jan 20.
2
Laboratory simulation of uranium metal corrosion in different soil moisture regimes.不同土壤湿度条件下铀金属腐蚀的实验室模拟
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3
A novel laboratory simulation system to uncover the mechanisms of uranium upward transport in a desert landscape.一种用于揭示沙漠景观中铀向上迁移机制的新型实验室模拟系统。
MethodsX. 2019 Dec 3;7:100758. doi: 10.1016/j.mex.2019.11.031. eCollection 2020.
4
Electrokinetic-enhanced phytoremediation of uranium-contaminated soil using sunflower and Indian mustard.向日葵和芥菜联合电动强化修复铀污染土壤。
Int J Phytoremediation. 2019;21(12):1197-1204. doi: 10.1080/15226514.2019.1612847. Epub 2019 May 17.
5
The influence of heavy metals in road dust on the surface runoff quality: Kinetic, isotherm, and sequential extraction investigations.道路灰尘中重金属对地表径流水质的影响:动力学、等温线和顺序提取研究。
Ecotoxicol Environ Saf. 2019 Jul 30;176:270-278. doi: 10.1016/j.ecoenv.2019.03.106. Epub 2019 Apr 1.
6
Passive, non-intrusive assay of depleted uranium.乏铀的被动、非侵入式分析。
J Hazard Mater. 2019 Feb 15;364:293-299. doi: 10.1016/j.jhazmat.2018.08.018. Epub 2018 Aug 10.
7
Metals geochemistry and mass export from the Mississippi-Atchafalaya River system to the Northern Gulf of Mexico.密西西比-阿查法拉亚河系统向墨西哥湾北部输送的金属地球化学与质量。
Chemosphere. 2018 Aug;205:559-569. doi: 10.1016/j.chemosphere.2018.04.094. Epub 2018 Apr 17.
8
Uranium in groundwater - A synopsis based on a large hydrogeochemical data set.地下水铀——基于大型水文地球化学数据集的概述。
Water Res. 2018 Feb 1;129:29-38. doi: 10.1016/j.watres.2017.11.001. Epub 2017 Nov 2.
9
Chemical toxicity and radioactivity of depleted uranium: The evidence from in vivo and in vitro studies.贫铀的化学毒性与放射性:来自体内和体外研究的证据。
Environ Res. 2017 Jul;156:665-673. doi: 10.1016/j.envres.2017.04.032. Epub 2017 May 12.
10
Depleted Uranium and Human Health.贫铀与人类健康。
Curr Med Chem. 2018;25(1):49-64. doi: 10.2174/0929867324666170426102343.

干旱武器试验生态系统中铀的水平和垂直迁移

Horizontal and Vertical Transport of Uranium in an Arid Weapon-Tested Ecosystem.

作者信息

Kazery Joseph A, Yang Rui, Bao Li, Zhang Qinku, James Markiesha, Dasari Shaloam, Guo Fuyu, Nie Jing, Larson Steve L, Ballard John H, Knotek-Smith Heather M, Unz Ron, Tchounwou Paul B, Han Fengxiang X

机构信息

Department of Environmental Science, Jackson State University, Jackson, Mississippi 39217, United States.

Department of Chemistry, Physics and Atmospheric Science, Jackson State University, Jackson, Mississippi 39217, United States.

出版信息

ACS Earth Space Chem. 2022 May 19;6(5):1321-1330. doi: 10.1021/acsearthspacechem.2c00028. Epub 2022 Apr 6.

DOI:10.1021/acsearthspacechem.2c00028
PMID:36275877
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9585917/
Abstract

Armor-penetrating projectiles and fragments of depleted uranium (DU) have been deposited in soils at weapon-tested sites. Soil samples from these military facilities were analyzed by inductively coupled plasma-optical emission spectroscopy and X-ray diffraction to determine U concentrations and transport across an arid ecosystem. Under arid conditions, both vertical transport driven by evaporation (upward) and leaching (downward) and horizontal transport of U driven by surface runoff in the summer were observed. Upward vertical transport was simulated and confirmed under laboratory-controlled conditions, to be leading to the surface due to capillary action via evaporation during alternating wetting and drying conditions. In the field, the 92.8% of U from DU penetrators and fragments remained in the top 5 cm of soil and decreased to background concentrations in less than 20 cm. In locations prone to high amounts of water runoff, U concentrations were reduced significantly after 20 m from the source due to high surface runoff. Uranium was also transported throughout the ecosystem via plant uptake and wild animal consumption between trophic levels, but with limited accumulation in edible portions in plants and animals.

摘要

穿甲弹和贫铀(DU)碎片已沉积在武器试验场的土壤中。通过电感耦合等离子体发射光谱法和X射线衍射法对这些军事设施的土壤样本进行分析,以确定铀的浓度以及其在干旱生态系统中的迁移情况。在干旱条件下,观察到了由蒸发(向上)和淋溶(向下)驱动的垂直迁移以及夏季由地表径流驱动的铀的水平迁移。在实验室控制条件下模拟并证实了向上的垂直迁移,即在交替的湿润和干燥条件下,由于蒸发产生的毛细作用导致铀迁移至地表。在野外,来自贫铀穿甲弹和碎片的铀有92.8%留在土壤表层5厘米内,在不到20厘米的深度降至背景浓度。在容易产生大量径流的地区,由于高地表径流,距源20米后铀浓度显著降低。铀还通过植物吸收和不同营养级之间的野生动物食用在整个生态系统中迁移,但在植物和动物的可食用部分积累有限。