Changes in oxidative potential of soil and fly ash after reaction with gaseous nitric acid

Zhan, Y; Ginder-Vogel, M; Shafer, MM; Rudich, Y; Pardo, M; Katra, I; Katoshevski, D; Schauer, JJ

HERO ID

4389386

Reference Type

Journal Article

Year

2018

HERO ID 4389386
In Press No
Year 2018
Title Changes in oxidative potential of soil and fly ash after reaction with gaseous nitric acid
Authors Zhan, Y; Ginder-Vogel, M; Shafer, MM; Rudich, Y; Pardo, M; Katra, I; Katoshevski, D; Schauer, JJ
Journal Atmospheric Environment
Volume 173
Page Numbers 306-315
Abstract The goal of this study was to examine the impact of simulated atmospheric aging on the oxidative potential of inorganic aerosols comprised primarily of crustal materials. Four soil samples and one coal fly ash sample were artificially aged in the laboratory through exposure to the vapor from 15.8 M nitric acid solution for 24 h at room temperature. Native and acid-aged samples were analyzed with a cellular macrophage and acellular dithionthreitol assays to determine oxidative potential. Additionally, the samples were analyzed to determine the concentration of 50 elements, both total and the water-soluble fraction of these elements by Sector Field Inductively Coupled Plasma Mass Spectrometry (SF-ICMS) and crystalline mineral composition using X-ray Diffraction (XRD). The results show that reactions with gaseous nitric acid increase the water-soluble fraction of many elements, including calcium, iron, magnesium, zinc, and lead. The mineral composition analysis documented that calcium-rich minerals present in the soils (e.g., calcite) are converted into different chemical forms, such as calcium nitrate (Ca(NO3)(2)). The nitric acid aging process, which can occur in the atmosphere, leads to a 200-600% increase in oxidative potential, as measured by cellular and acellular assays. This laboratory study demonstrates that the toxic effects of aged versus freshly emitted atmospheric dust may be quite different. In addition, the results suggest that mineralogical analysis of atmospheric dust may be useful in understanding its degree of aging.
Doi 10.1016/j.atmosenv.2017.11.008
Wosid WOS:000423007600029
Is Certified Translation No
Dupe Override No
Is Public Yes
Keyword Acid aging; Mineral dust; ROS activity; Metals