利用 IMAGES 模拟 ATHLETIC 运动期间的室内无机气溶胶浓度

Bryan Berman, Bryan Cummings, Hongyu Guo, Pedro Campuzano-Jost, Jose Jimenez, Demetrios Pagonis, Douglas Day, Zachary Finewax, Anne Handschy, Benjamin A. Nault, Peter DeCarlo, Shannon Capps and Michael Waring*, 
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引用次数: 0

摘要

2018 年,在科罗拉多大学达尔沃德体育中心开展了 ATHLETIC 活动,对体育馆环境中的动态室内空气成分进行了表征。除其他参数外,还在体育馆的供应管道和举重室交替测量了无机颗粒物和气相物种。气溶胶、气体、排放物和表面的室内模型(IMAGES)使用无机气溶胶热力学平衡模型 ISORROPIA 来估算无机气溶胶和相应气体的分配情况。本研究使用 ATHLETIC 活动的测量数据来评估 IMAGES 的性能。氨气排放率、硝酸沉积和颗粒沉积速度与观测到的占用率相关,这为 IMAGES 运行中的这些比率提供了依据。起初,建模的室内无机气溶胶浓度与测量结果不太一致。参数调查显示,降低 ISORROPIA 模型中使用的温度或提高相对湿度会使半挥发性物质更趋向于粒子相,从而大大改善了模型与测量结果的一致性。推测这些解决方案的原因之一是,相对湿度的增加或温度的降低增强了气溶胶的水分。另一个原因是在这种室内环境中没有建立热力学平衡,或者 ISORROPIA 中的热力学参数对于典型的室内环境不太准确。这一结果表明,在室内应用 ISORROPIA 需要进一步仔细的实验验证。这项工作应用了室内气溶胶模型 IMAGES,该模型通过利用一所大学体育中心的测量数据以及占用率与硝酸沉积、颗粒沉积和氨排放之间的衍生关系,估算出无机气溶胶成分及其相应气相物种与 ISORROPIA 的分配情况。这项研究表明,在室内应用 ISORROPIA 有时会导致气体-粒子分配不准确。然而,通过提高相对湿度或降低温度来迫使模型预测颗粒物水分的增加,将导致准确的气体-颗粒物分配。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Modeling Indoor Inorganic Aerosol Concentrations During the ATHLETIC Campaign with IMAGES

Modeling Indoor Inorganic Aerosol Concentrations During the ATHLETIC Campaign with IMAGES

In 2018, the ATHLETIC campaign was conducted at the University of Colorado Dal Ward Athletic Center and characterized dynamic indoor air composition in a gym environment. Among other parameters, inorganic particle and gas-phase species were alternatingly measured in the gym’s supply duct and weight room. The Indoor Model of Aerosols, Gases, Emissions, and Surfaces (IMAGES) uses the inorganic aerosol thermodynamic equilibrium model, ISORROPIA, to estimate the partitioning of inorganic aerosols and corresponding gases. In this study herein, measurements from the ATHLETIC campaign were used to evaluate IMAGES’ performance. Ammonia emission rates, nitric acid deposition, and particle deposition velocities were related to observed occupancy, which informed these rates in IMAGES runs. Initially, modeled indoor inorganic aerosol concentrations were not in good agreement with measurements. A parametric investigation revealed that lowering the temperature or raising the relative humidity used in the ISORROPIA model drove the semivolatile species more toward the particle phase, substantially improving modeled-measured agreement. One speculated reason for these solutions is that aerosol water was enhanced by increasing the RH or decreasing the temperature. Another is that thermodynamic equilibrium was not established in this indoor setting or that the thermodynamic parametrizations in ISORROPIA are less accurate for typical indoor settings. This result suggests that applying ISORROPIA indoors requires further careful experimental validation.

This work applies an indoor aerosol model, IMAGES, that estimates the partitioning of inorganic aerosol components and their corresponding gas-phase species with ISORROPIA by leveraging measurements from a university athletic center and derived relationships between occupancy and nitric acid deposition, particle deposition, and ammonia emissions. This study highlights that applying ISORROPIA indoors can sometimes result in inaccurate gas-particle partitioning. However, forcing the model to predict increased particle water by either adjusting relative humidity up or temperature down will result in accurate gas-particle partitioning.

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