Department of Civil and Environmental Engineering, University of Houston , Houston, Texas 77204, United States.
Environ Sci Technol. 2013 Sep 17;47(18):10179-87. doi: 10.1021/es4015663. Epub 2013 Sep 9.
The trans-Atlantic transport of North African dust by summertime trade winds occasionally increases ambient particulate matter (PM) concentrations in Texas above air quality standards. Exemptions from such exceedences can be sought for episodic events that are beyond regulatory control by providing qualitative supportive information such as satellite images and back-trajectories. Herein we demonstrate that chemical mass balancing can successfully isolate, differentiate, and quantify the relative contributions from local and global mineral dust sources through detailed measurements of a wide suite of elements in ambient PM. We identified a major dust storm originating in Northwest Africa in mid-July 2008 which eventually impacted air quality in Houston during July 25, 26, and 27, 2008. Daily PM2.5 and PM10 samples were collected at two sites in Houston over a 2-week period encompassing the Saharan dust episode to quantify the transported mineral dust concentrations during this peak event. Average PM concentrations more than doubled during the Saharan intrusion compared with non-Saharan. Relative concentrations of several elements often associated with anthropogenic sources were significantly diluted by crustal minerals coincident with the large-scale Saharan dust intrusion. During non-Saharan days, local mineral dust sources including cement manufacturing and soil and road dust contributed in total 26% to PM2.5 mass and 50% to PM10 mass; during the three-day Saharan episode the total dust contribution increased to 64% for PM2.5 and 85% for PM10. Importantly, this approach was also able to determine that local emissions of crustal minerals dominated the period immediately following the Saharan dust episode: simple quantification of bulk crustal materials may have misappropriated this elevated PM to trans-Atlantic transport of Saharan dust.
夏季贸易风偶尔会将北非尘埃输送到跨大西洋地区,使德克萨斯州的环境颗粒物(PM)浓度超过空气质量标准。对于超出法规控制的偶发事件,可以通过提供卫星图像和后向轨迹等定性支持信息来寻求豁免。在此,我们通过对环境 PM 中广泛元素的详细测量,证明了化学质量平衡可以成功地分离、区分和量化来自本地和全球矿物尘埃源的相对贡献。我们确定了 2008 年 7 月中旬起源于西北非的一场主要沙尘暴,该沙尘暴最终于 2008 年 7 月 25、26 和 27 日影响了休斯顿的空气质量。在涵盖撒哈拉尘暴事件的两周内,在休斯顿的两个地点采集了每日 PM2.5 和 PM10 样本,以量化在该峰值事件中传输的矿物尘埃浓度。与非撒哈拉期间相比,撒哈拉入侵期间的每日 PM2.5 和 PM10 浓度平均值增加了一倍以上。与人为源相关的几种元素的相对浓度因与大规模撒哈拉尘埃入侵同时出现的地壳矿物质而显著稀释。在非撒哈拉期间,包括水泥制造和土壤及道路尘埃在内的本地矿物尘埃源对 PM2.5 质量的总贡献为 26%,对 PM10 质量的总贡献为 50%;在撒哈拉尘暴的三天期间,尘埃总贡献增加到 PM2.5 的 64%和 PM10 的 85%。重要的是,这种方法还能够确定本地地壳矿物质的排放在撒哈拉尘埃事件之后立即占主导地位:简单地量化大块地壳物质可能会将这种升高的 PM 错误地归因于撒哈拉尘埃的跨大西洋传输。