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首页> 外文期刊>Journal of the air & waste management association >Reconciliation and Interpretation of Big Bend National Park Participate Sulfur Source Apportionment: Results from the Big Bend Regional Aerosol and Visibility Observational Study—Part Ⅰ
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Reconciliation and Interpretation of Big Bend National Park Participate Sulfur Source Apportionment: Results from the Big Bend Regional Aerosol and Visibility Observational Study—Part Ⅰ

机译:大弯国家公园参与硫源分配的和解与解释:大弯区域气溶胶和能见度观测研究的结果(第一部分)

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摘要

The Big Bend Regional Aerosol and Visibility Observational (BRAVO) study was an intensive monitoring study from July through October 1999 followed by extensive assessments to determine the causes and sources of haze in Big Bend National Park, located in Southwestern Texas. Particulate sulfate compounds are the largest contributor of haze at Big Bend, and chemical transport models (CTMs) and receptor models were used to apportion the sulfate concentrations at Big Bend to North American source regions and the Carbon power plants, located 225 km southeast of Big Bend in Mexico. Initial source attribution methods had contributions that varied by a factor of ≥ 2. The evaluation and comparison of methods identified opposing biases between the CTMs and receptor models, indicating that the ensemble of results bounds the true source attribution results. The reconciliation of these differences led to the development of a hybrid receptor model merging the CTM results and air quality data, which allowed a nearly daily source apportionment of the sulfate at Big Bend during the BRAVO study. The best estimates from the reconciliation process resulted in sulfur dioxide (SO_2) emissions from U.S. and Mexican sources contributing ~55% and 38%, respectively, of sulfate at Big Bend. The distribution among U.S. source regions was Texas, 16%; the Eastern United States, 30%; and the Western United States, 9%. The Carbon facilities contributed 19%, making them the largest single contributing facility. Sources in Mexico contributed to the sulfate at Big Bend on most days, whereas contributions from Texas and Eastern U.S. sources were episodic, with their largest contributions during Big Bend sulfate episodes. On the 20% of the days with the highest sulfate concentrations, U.S. and Mexican sources contributed ~71% and 26% of the sulfate, respectively. However, on the 20% of days with the lowest sulfate concentrations, Mexico contributed 48% compared with 40% for the United States.
机译:大弯曲地区气溶胶和能见度观测(BRAVO)研究是从1999年7月至1999年10月的一项密集监视研究,随后进行了广泛评估,以确定德克萨斯州西南部大弯曲国家公园的霾成因和来源。颗粒状硫酸盐化合物是大弯曲地区雾霾的最大贡献者,化学迁移模型(CTM)和受体模型用于将大弯曲地区的硫酸盐浓度分配给位于大弯曲东南225公里的北美源区和碳电厂在墨西哥弯曲。最初的来源归因方法的贡献相差≥2。方法的评估和比较确定了CTM和受体模型之间的对立偏差,表明结果的集合限制了真正的来源归因结果。这些差异的调和导致了混合受体模型的发展,该模型融合了CTM结果和空气质量数据,从而在BRAVO研究期间几乎每天都能在Big Bend分配硫酸盐。根据对帐过程的最佳估计,美国和墨西哥来源的二氧化硫(SO_2)排放分别贡献了大弯曲地区约55%和38%的硫酸盐。美国来源地区之间的分布是德克萨斯州,为16%;美国东部,占30%;美国西部占9%。 Carbon设施贡献了19%,使其成为最大的单一贡献设施。在大多数情况下,墨西哥的排放源是大弯曲地区硫酸盐的来源,而得克萨斯州和美国东部的来源是偶发性的,在大弯曲地区硫酸盐事件中贡献最大。在硫酸盐浓度最高的20%的日子中,美国和墨西哥的来源分别贡献了约71%和26%的硫酸盐。但是,在硫酸盐浓度最低的20%的日子里,墨西哥贡献了48%,而美国为40%。

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