Department of Geology. University of Sonora, Rosales y Encinas, Hermosillo, Sonora 83000, Mexico; Department of Geology. Graduate Program, Rosales y Encinas, Hermosillo, Sonora 83000, Mexico.
Earth Sciences Graduate Program. Institute of Geology, National University of Mexico. Colosio y Madrid, Hermosillo, Sonora 83240, Mexico.
Sci Total Environ. 2018 Jul 15;630:1596-1607. doi: 10.1016/j.scitotenv.2018.02.285. Epub 2018 Mar 20.
The environmental fate of lead derived from traffic paint has been poorly studied in developing countries, mainly in arid zones. For this purpose, a developing city located in the Sonoran desert (Hermosillo, Mexico), was chosen to conduct a study. In this paper the lead chromate (crocoite) sources in atmospheric dust were addressed using a combination of Raman microspectroscopy, X-ray diffraction, scanning electron microscopy (SEM), and Pb isotope measurements. A high concentration of Pb and Cr as micro- and nanostructured pigments of crocoite is reported in yellow traffic paint (n=80), road dust (n=146), settled dust in roofs (n=21), and atmospheric dust (n=20) from a developing city located in the Sonoran Desert. 10 samples of peri-urban soils were collected for local geochemical background. The paint photodegradation and erosion of the asphaltic cover are enhanced by the climate, and the presence of the mineral crocoite (PbCrO) in road dust with an aerodynamic diameter ranging from 100nm to 2μm suggests its integration into the atmosphere by wind resuspension processes. A positive PbCr correlation (R=0.977) was found for all studied samples, suggesting a common source. The Pb-isotope data show signatures in atmospheric dust as a product of the mixing of two end members: i) local soils and ii) crocoite crystals as pigments in paint. The presence of lead chromates in atmospheric dust has not been previously documented in Latin America, and it represents an unknown health risk to the exposed population because the identified size of crystals can reach the deepest part of lungs.
交通漆中的铅的环境归宿在发展中国家,特别是在干旱地区,研究得很少。为此,选择了位于索诺兰沙漠(墨西哥)的一个发展中城市进行研究。本文采用拉曼微光谱、X 射线衍射、扫描电子显微镜(SEM)和 Pb 同位素测量相结合的方法,研究了大气尘中铬酸铅(铬铅矿)的来源。报告了在黄色交通漆(n=80)、道路尘(n=146)、屋顶沉降尘(n=21)和位于索诺兰沙漠的发展中城市的大气尘(n=20)中,Pb 和 Cr 以微纳米结构的铬铅矿颜料的形式存在,浓度较高。采集了 10 个城郊土壤样本作为当地地球化学背景。气候会促进油漆的光降解和沥青覆盖层的侵蚀,而在大气尘中存在的矿物铬铅矿(PbCrO),其空气动力学直径在 100nm 至 2μm 之间,表明它通过风再悬浮过程进入大气。在所研究的所有样本中都发现了 PbCr 之间的正相关(R=0.977),表明存在共同的来源。Pb 同位素数据显示,大气尘中的特征是两种端元的混合产物:i)当地土壤和 ii)油漆中的铬铅矿晶体作为颜料。大气尘中存在铬酸铅在拉丁美洲以前没有记录过,对暴露人群构成了未知的健康风险,因为所识别的晶体大小可以到达肺部的最深部位。