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Open AccessDOI: 10.12030/j.cjee.202511095Original Research

Characteristics of Autumn–Winter Daily Atmospheric Dustfall Pollution in the Core Area of Beijing

Beijing Municipal Research Institute of Eco-Environmental Protection, National Engineering Research Center for Urban Environmental Pollution Control, Beijing 100037, China

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Characteristics of Autumn–Winter Daily Atmospheric Dustfall Pollution in the Core Area of Beijing
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Published In
Chinese Journal of Environmental Engineering
Published:January 15, 2026Edition:Vol. 20, Issue 7 • pp. 100-112Citation:HUANG Yu-hu et al. (2026), Chinese Journal of Environmental Engineering
Impact FactorPeer-Reviewed Core
Source Journal环境工程学报

Key Takeaways & Executive Findings

  • • • The proposed filtration-based daily dustfall method achieved a spiked recovery of 101.1% ± 1.2% and parallelism y = 0.95x + 0.28, enabling reliable high-resolution (1-day) dustfall monitoring and component analysis, overcoming the limitations of conventional monthly total dustfall measurements. • • Daily dustfall in autumn–winter ranged from 0.06 to 2.33 t·(km²·d)−1; days exceeding 0.7 t·(km²·d)−1 constituted only 4% of sampling days but contributed 25% of total dustfall, indicating a 'few high-value days dominate' pattern that is critical for prioritizing control actions. • • Insoluble dustfall averaged 83% ± 12% of total dustfall, and the model y = 9.36ln(x) + 99.98 (x ≤ 1.00) allows rapid estimation of total dustfall from insoluble measurements, facilitating source apportionment and local fugitive dust assessment. • • Daily dustfall correlated strongly with average wind speed, with an exponential model y = 0.06e0.61x; wind speeds ≥3 on the Beaufort scale significantly amplified dustfall, supporting the implementation of emergency measures (e.g., stopping earthwork, covering bare soil, increasing watering) during high-wind forecasts.

Abstract

To address the low temporal resolution of conventional monthly dustfall monitoring and the lack of component information, this study proposed a daily dustfall measurement method that adds a filtration step to the Chinese standard method, referencing international standards. Using a sand-core filtration device with quartz or mixed cellulose ester membranes, the method achieved a spiked recovery of 101.1% ± 1.2%, good parallelism (y = 0.95x + 0.28), and satisfactory temporal closure. During autumn–winter (November 2020 to March 2021) at a representative site in Xicheng District, Beijing, daily dustfall ranged from 0.06 to 2.33 t·(km²·d)−1. Days with daily dustfall exceeding 0.7 t·(km²·d)−1 accounted for only 4% of the sampling days but contributed 25% of the total dustfall, with high values mainly occurring in January, March, and December. The insoluble fraction averaged 83% ± 12%, and a logarithmic model (y = 9.36ln(x) + 99.98) was established to estimate the insoluble proportion from insoluble dustfall (x, ≤1.00). Daily dustfall showed a strong positive correlation with average wind speed, and an exponential prediction model (y = 0.06e0.61x) was derived. Windy conditions (≥3 on the Beaufort scale) significantly amplified dustfall. The study recommends suspending earthwork, covering bare ground, and increasing watering frequency during high-wind alerts to mitigate dust pollution. This work provides a reliable method for high-resolution dustfall monitoring and insights for targeted pollution control in urban core areas.

1. Introduction

Conventional dustfall monitoring in China relies on monthly sampling and a gravimetric method that measures only total dustfall, lacking the temporal resolution to capture day-to-day variations and the compositional information needed for source apportionment. This limitation is particularly acute in megacities like Beijing, where short-term pollution episodes and meteorological drivers such as wind speed play a critical role. International standards (ISO, ASTM) employ filtration to separate insoluble and soluble fractions, but their application to daily timescales in Chinese urban settings has been limited. The absence of a validated daily filtration method hinders the identification of high-impact days and the quantification of local fugitive dust contributions.

This study addresses these bottlenecks by adapting the filtration approach to a 24-hour sampling protocol, using a sand-core filtration device and membrane filters to achieve high recovery and reproducibility. By deploying multiple parallel collectors, the method enables robust daily dustfall measurements. The study further establishes quantitative relationships between daily dustfall and wind speed, and between insoluble fraction and total dustfall, providing practical tools for rapid assessment and targeted control. These advances support the shift from passive monthly monitoring to proactive daily management of dust pollution in urban core areas.

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Cite This Research Paper
HUANG Yu-hu, LIU Li-yang, LI Bei-bei, WANG Yu, LIANG Jing, ZHAO Yu, QIN Jian-ping (2026). Characteristics of Autumn–Winter Daily Atmospheric Dustfall Pollution in the Core Area of Beijing. Chinese Journal of Environmental Engineering. https://doi.org/10.12030/j.cjee.202511095
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Frequently Asked Questions

What is the operational advantage of the sand-core filtration device over the Buchner funnel in daily dustfall measurement?

The sand-core filtration device reduced average filtration time to 53% of that of the Buchner funnel. The Buchner funnel exhibited incomplete membrane coverage, leading to sample accumulation at edges, particle loss into the filtrate, and increased risk of membrane perforation, which compromised accuracy and subsequent chemical analysis. The sand-core device ensured uniform particle distribution and reliable filtration.

How does the proposed method ensure data quality for daily dustfall measurements, and what are the key validation metrics?

Data quality was validated through spiked recovery (101.1% ± 1.2%), parallelism (y = 0.95x + 0.28), and temporal closure. These metrics confirm high accuracy, precision, and consistency across sampling periods, making the method suitable for capturing day-to-day variability.

What is the significance of the insoluble fraction (83% ± 12%) in the context of source apportionment?

The high insoluble fraction indicates that local fugitive dust sources (e.g., construction, road dust, wind erosion) dominate at the study site. This supports the use of the logarithmic model (y = 9.36ln(x) + 99.98) to estimate total dustfall from insoluble measurements, enabling rapid screening of local contributions without full chemical analysis.

How can the wind speed–dustfall model (y = 0.06e0.61x) be applied in operational dust control?

The exponential model allows forecasting daily dustfall based on predicted average wind speed. For instance, a wind speed increase from 2 to 4 m/s would raise predicted dustfall from approximately 0.20 to 0.66 t·(km²·d)−1, a 3.3-fold increase. This quantifies the need for preemptive measures such as halting earthwork and increasing watering when wind speeds exceed 3 on the Beaufort scale.

What are the limitations of this study in terms of spatial representativeness?

The study was conducted at a single rooftop site in Xicheng District, characterized by dense buildings and impervious surfaces. The results are representative of similar underlying surface conditions but may not fully apply to areas with green spaces or water bodies. Further validation across different land-use types is needed to generalize the models.

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