Home    |    Contact   |    Chinese   |    CAS
Upcoming Events : The International Training Program on Soil Carbon Cycling in Arid Ecosystems ...
Location :Home > Papers
Paper Code   20230016
Title   Comparison of chemical composition and acidity of size-resolved inorganic aerosols at the top and foot of Mt. Hua, Northwest China: The role of the gas-particle distribution of ammonia.
Authors   Feng Qiao
Corresponding Author   Zhou Bianhong; Li Jianjun
Year   2023
Title of Journal  
Volume   905
Number  
Page   166985
Abstract   Aerosol pH is not only a diagnostic indicator of secondary aerosol formation, but also a key factor in the specific chemical reaction routes that produce sulfate and nitrate. To understand the characteristics of aerosol acidity in the Mt. Hua, the chemical fractions of water-soluble inorganic ions in the atmospheric PM2.5 and size-resolved particle at the top and foot of Mt. Hua in summer 2020 were studied. The results showed the mass concentrations of PM2.5 and water-soluble ions at the foot were 2.0-2.6 times higher than those at the top. The secondary inorganic ions, i.e., SO42-, NO3-, and NH4+ (SNA) were 56%-61% higher by day than by night. SO42- was mainly distributed in the fine particles (Dp<2.1mum). NO3- showed a unimodal size distribution (peaking at 0.7-1.1mum) at the foot and a bimodal (0.7-1.1mum and 4.7-5.8mum) size distribution at the top. At the top site, the distribution of NO3- in coarse particles (> 2.1mum) was mainly attributed to the gaseous HNO3 volatilized from fine particles reacting with cations in coarse particles to form non-volatile salts (such as Ca(NO3)2). The pH values of PM2.5 were 2.7±1.3 and 3.3±0.42 at the top and foot, respectively. NH4+/NH3(g) plays a decisive role in stabilizing aerosol acidity. In addition, the increase of the liquid water content (LWC) at the foot facilitates the gas-particle conversion of NH3, while the H+ concentration was diluted, resulting in a decrease in acidity at the foot. NH4+/NH3 had good linear correlations with SO42-, NO3-, and LWC during the daytime at both sites, indicating that SO42-, NO3-, and LWC together affect the gas-particle distribution of ammonia by day: however, the effect of LWC at night was not evident.
Full Text  
Full Text Link   https://doi.org/10.1016/j.scitotenv.2023.166985    
Others:
Classification:
Source:
 
© 2015 Institute of Earth Environment,CAS
Address:No. 97 Yanxiang Road, Xi'an 710061, Shaanxi, China