Departmento de Ingeniería Química y Bioprocesos, Pontificia Universidad Católica de Chile, Avda. Vicuña Mackenna 4860, Santiago 6904411, Chile.
Sci Total Environ. 2013 Feb 1;444:327-35. doi: 10.1016/j.scitotenv.2012.12.007. Epub 2012 Dec 29.
Estimating contributions of anthropogenic sources to ambient particulate matter (PM) in desert regions is a challenging issue because wind erosion contributions are ubiquitous, significant and difficult to quantify by using source-oriented, dispersion models. A receptor modeling analysis has been applied to ambient PM(10) and PM(2.5) measured in an industrial zone ~20 km SE of Antofagasta (23.63°S, 70.39°W), a midsize coastal city in northern Chile; the monitoring site is within a desert region that extends from northern Chile to southern Perú. Integrated 24-hour ambient samples of PM(10) and PM(2.5) were taken with Harvard Impactors; samples were analyzed by X Ray Fluorescence, ionic chromatography (NO(3)(-) and SO(4)(=)), atomic absorption (Na(+), K(+)) and thermal optical transmission for elemental and organic carbon determination. Receptor modeling was carried out using Positive Matrix Factorization (US EPA Version 3.0); sources were identified by looking at specific tracers, tracer ratios, local winds and wind trajectories computed from NOAA's HYSPLIT model. For the PM(2.5) fraction, six contributions were found - cement plant, 33.7 ± 1.3%; soil dust, 22.4 ± 1.6%; sulfates, 17.8 ± 1.7%; mineral stockpiles and brine plant, 12.4 ± 1.2%; Antofagasta, 8.5 ± 1.3% and copper smelter, 5.3 ± 0.8%. For the PM(10) fraction five sources were identified - cement plant, 38.2 ± 1.5%; soil dust, 31.2 ± 2.3%; mineral stockpiles and brine plant, 12.7 ± 1.7%; copper smelter, 11.5 ± 1.6% and marine aerosol, 6.5 ± 2.4%. Therefore local sources contribute to ambient PM concentrations more than distant sources (Antofagasta, marine aerosol) do. Soil dust is enriched with deposition of marine aerosol and calcium, sulfates and heavy metals from surrounding industrial activities. The mean contribution of suspended soil dust to PM(10) is 50 μg/m(3) and the peak daily value is 104 μg/m(3). For the PM(2.5) fraction, suspended soil dust contributes with an average of 9.3 μg/m(3) and a peak daily value of 31.5 μg/m(3).
估算人为源对沙漠地区环境颗粒物(PM)的贡献是一个具有挑战性的问题,因为风蚀贡献普遍存在且显著,并且难以使用面向源的扩散模型进行量化。受体建模分析已应用于在智利北部一个中型沿海城市安托法加斯塔(23.63°S,70.39°W)东南约 20 公里的一个工业区测量的环境 PM(10)和 PM(2.5);监测点位于从智利北部延伸到秘鲁南部的沙漠地区内。使用哈佛撞击器采集了 24 小时的环境 PM(10)和 PM(2.5)的综合样本;使用 X 射线荧光、离子色谱(NO(3)(-)和 SO(4)(=))、原子吸收(Na(+)、K(+))和热光传输对元素和有机碳进行了分析。受体建模使用美国环保署的正矩阵因子化(US EPA Version 3.0)进行;通过查看特定示踪剂、示踪剂比、当地风和从美国国家海洋和大气管理局的 HYSPLIT 模型计算的风向轨迹来确定源。对于 PM(2.5)部分,发现了六个贡献源 - 水泥厂,33.7 ± 1.3%; 土壤尘埃,22.4 ± 1.6%; 硫酸盐,17.8 ± 1.7%; 矿物堆和盐水厂,12.4 ± 1.2%; 安托法加斯塔,8.5 ± 1.3%和铜冶炼厂,5.3 ± 0.8%。对于 PM(10)部分,确定了五个源 - 水泥厂,38.2 ± 1.5%; 土壤尘埃,31.2 ± 2.3%; 矿物堆和盐水厂,12.7 ± 1.7%; 铜冶炼厂,11.5 ± 1.6%和海洋气溶胶,6.5 ± 2.4%。因此,当地源对环境 PM 浓度的贡献大于远距离源(安托法加斯塔,海洋气溶胶)的贡献。土壤尘埃富含海洋气溶胶的沉积以及周围工业活动产生的钙、硫酸盐和重金属。悬浮土壤尘埃对 PM(10)的平均贡献为 50 μg/m(3),日峰值为 104 μg/m(3)。对于 PM(2.5)部分,悬浮土壤尘埃的平均贡献为 9.3 μg/m(3),日峰值为 31.5 μg/m(3)。