Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang, 550025, China; North Alabama International College of Engineering and Technology, Guizhou University, Guiyang, 550025, China.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Beijing), Beijing 100083, China.
Water Res. 2024 Jun 15;257:121657. doi: 10.1016/j.watres.2024.121657. Epub 2024 Apr 22.
The coastal urban region is generally considered an atmospheric receptor for terrestrial and marine input materials, and rainfall chemistry can trace the wet scavenging process of these materials. Fast urbanization in China's east coastal areas has greatly altered the rainwater chemistry. However, the chemical variations, determinants, and sources of rainfall are unclear. Therefore, the typical coastal city of Fuzhou was selected for 1-year rainwater sampling and inorganic ions were detected to explore above problems. The findings depicted that rainwater ions in Fuzhou were slightly different from those in other coastal cities. Although NO, SO, Ca and NH dominated the rainwater ions, the marine input Cl (22 %) and Na (11 %) also contributed a considerable percentage to the rainwater ions. Large differences in ion concentrations (2∼28 times) were found in monthly scale due to the rainfall amount. Both natural and anthropogenic determinants influenced the rainwater ions in coastal cities, such as SO emission, air SO and PM content on rainwater SO, NO, and Ca, and soot & dust emission on rainwater SO, NO, indicating the vital contribution of human activities. Stoichiometry and positive matrix factorization-based sources identification indicated that atmospheric dust/particles were the primary contributor of Ca (83.3 %) and F (83.7 %), and considerable contributor of SO (39.5 %), NO (38.3 %) and K (41.5 %). Anthropogenic origins, such as urban waste volatilization and fuel combustion emission, contributed 95 % of NH, 54.5 % of NO and 41.9 % of SO, and the traffic sources contribution was relatively higher than fixed emission sources. The marine input represented the vital source of Cl (77.7 %), Na (84.9 %), and Mg (55.3 %). This work highlights the significant influence of urban human activities and marine input on rainwater chemicals and provides new insight into the material cycle between the atmosphere and earth-surface in coastal city.
沿海城市地区通常被认为是陆地和海洋输入物质的大气受体,而降雨化学可以追踪这些物质的湿清除过程。中国东部沿海地区的快速城市化极大地改变了雨水化学性质。然而,降雨化学性质的变化、决定因素和来源尚不清楚。因此,选择典型的沿海城市福州进行了为期一年的雨水采样,并检测了无机离子,以探讨上述问题。研究结果表明,福州的雨水离子与其他沿海城市略有不同。尽管 NO、SO、Ca 和 NH 主导了雨水离子,但海洋输入的 Cl(22%)和 Na(11%)也对雨水离子有相当大的贡献。由于降雨量的不同,离子浓度在月度尺度上存在较大差异(2∼28 倍)。自然和人为因素都会影响沿海城市的雨水离子,如 SO 排放、空气中的 SO 和 PM 含量对雨水 SO、NO 和 Ca 的影响,以及烟尘排放对雨水 SO、NO 的影响,表明人类活动的重要贡献。化学计量学和基于正定矩阵因子分解的来源识别表明,大气粉尘/颗粒是 Ca(83.3%)和 F(83.7%)的主要贡献者,也是 SO(39.5%)、NO(38.3%)和 K(41.5%)的重要贡献者。人为来源,如城市废物挥发和燃料燃烧排放,贡献了 95%的 NH、54.5%的 NO 和 41.9%的 SO,交通源的贡献相对高于固定排放源。海洋输入代表了 Cl(77.7%)、Na(84.9%)和 Mg(55.3%)的重要来源。这项工作强调了城市人类活动和海洋输入对雨水化学物质的重要影响,并为沿海城市大气与地球表面物质循环提供了新的见解。