Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment

Oxidative potential (OP) is considered to be an efficient indicator of particulate matter (PM) to induce oxidative stress in the lungs and is increasingly considered to be a relevant health metric. In this study, two complementary OP assays were deployed, including dithiothreitol (DTT) and ascorbic acid (AA) assays, to investigate the potential toxicity (as generators of oxidative stress) of respirable fractions (DD4, < 4 μm) of deposited dust (DD500, < 500 μm) in underground low-S and low-pyrite coal mines in Henan Province, Central China. The OPDTT of DD4 is higher than that reported for other types of atmospheric PM, whereas the OPAA of DD4 is similar and/or slightly higher. Cross-correlation and multilinear regression analyses are applied using datasets of major mineral and geochemical patterns in the DD4 samples and the respective OP values to identify the major drivers for OP in respirable coal dust. Thereafter, the patterns of DD4 are compared with those of DD500 and the parent coals to determine the sources of OP-relevant substances. OPDTT is mainly governed by some trace elements (Sb, As, Li, B, Sr, and Pb) and minor minerals (anatase, quartz, siderite), and their synergistic effect may be one of the reasons for the high DTT consumption. For OPAA, quartz, total clay (sum of illite, kaolinite, tobelite, and clinochlore) and Ni, Cr, Co, Si, and S, play an important role in regulating the OPAA of pyrite-free DD4 samples. These OP-relevant substances have three sources: coal dust, which has a similar composition in DD4, DD500, and the parent coal (such as siderite and its associated elements); gangue dust, which does not occur in the parent coal but is widely detected in DD4 and DD500 (such as quartz, kaolinite, and relevant elements); and cement dust (from gunite galleries), which is mainly calcite- and calcite-associated elements.

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Main Authors: Shangguan, Yunfei, Zhuang, Xinguo, Querol, Xavier, Li, Baoqing, Moreno, Natalia, Trechera, Pedro, Sola, Patricia Córdoba, Uzu, Gaëlle, Li, Jing
Format: artículo biblioteca
Language:English
Published: Elsevier 2022-06-01
Subjects:Source apportionment, Geochemistry, Mineralogy, Oxidative potential, Respirable dust,
Online Access:http://hdl.handle.net/10261/271260
https://api.elsevier.com/content/abstract/scopus_id/85130291904
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spelling dig-idaea-es-10261-2712602024-05-15T20:56:48Z Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment Shangguan, Yunfei Zhuang, Xinguo Querol, Xavier Li, Baoqing Moreno, Natalia Trechera, Pedro Sola, Patricia Córdoba Uzu, Gaëlle Li, Jing Source apportionment Geochemistry Mineralogy Oxidative potential Respirable dust Oxidative potential (OP) is considered to be an efficient indicator of particulate matter (PM) to induce oxidative stress in the lungs and is increasingly considered to be a relevant health metric. In this study, two complementary OP assays were deployed, including dithiothreitol (DTT) and ascorbic acid (AA) assays, to investigate the potential toxicity (as generators of oxidative stress) of respirable fractions (DD4, < 4 μm) of deposited dust (DD500, < 500 μm) in underground low-S and low-pyrite coal mines in Henan Province, Central China. The OPDTT of DD4 is higher than that reported for other types of atmospheric PM, whereas the OPAA of DD4 is similar and/or slightly higher. Cross-correlation and multilinear regression analyses are applied using datasets of major mineral and geochemical patterns in the DD4 samples and the respective OP values to identify the major drivers for OP in respirable coal dust. Thereafter, the patterns of DD4 are compared with those of DD500 and the parent coals to determine the sources of OP-relevant substances. OPDTT is mainly governed by some trace elements (Sb, As, Li, B, Sr, and Pb) and minor minerals (anatase, quartz, siderite), and their synergistic effect may be one of the reasons for the high DTT consumption. For OPAA, quartz, total clay (sum of illite, kaolinite, tobelite, and clinochlore) and Ni, Cr, Co, Si, and S, play an important role in regulating the OPAA of pyrite-free DD4 samples. These OP-relevant substances have three sources: coal dust, which has a similar composition in DD4, DD500, and the parent coal (such as siderite and its associated elements); gangue dust, which does not occur in the parent coal but is widely detected in DD4 and DD500 (such as quartz, kaolinite, and relevant elements); and cement dust (from gunite galleries), which is mainly calcite- and calcite-associated elements. This research was funded by the National Science Foundation of China (No. 41972180), the “Overseas Top Scholars Program”, part of the “Recruitment Program of Global Experts” (No. G20190017067), and the Open Research Fund Project for Key Laboratory of Tectonics and Petroleum Resources (China University of Geosciences), Ministry of Education (No. TPR-2019-14). Additionally, Gaëlle Uzu acknowledges the Predictair project (FUGA and FAL foundations) for funding analytical equipment. Peer reviewed 2022-06-02T07:33:25Z 2022-06-02T07:33:25Z 2022-06-01 artículo http://purl.org/coar/resource_type/c_6501 International Journal of Coal Geology 258: 104017 (2022) 01665162 http://hdl.handle.net/10261/271260 10.1016/j.coal.2022.104017 2-s2.0-85130291904 https://api.elsevier.com/content/abstract/scopus_id/85130291904 en International Journal of Coal Geology Postprint https://doi.org/10.1016/j.coal.2022.104017 Sí embargo_20240601 Elsevier
institution IDAEA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-idaea-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IDAEA España
language English
topic Source apportionment
Geochemistry
Mineralogy
Oxidative potential
Respirable dust
Source apportionment
Geochemistry
Mineralogy
Oxidative potential
Respirable dust
spellingShingle Source apportionment
Geochemistry
Mineralogy
Oxidative potential
Respirable dust
Source apportionment
Geochemistry
Mineralogy
Oxidative potential
Respirable dust
Shangguan, Yunfei
Zhuang, Xinguo
Querol, Xavier
Li, Baoqing
Moreno, Natalia
Trechera, Pedro
Sola, Patricia Córdoba
Uzu, Gaëlle
Li, Jing
Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment
description Oxidative potential (OP) is considered to be an efficient indicator of particulate matter (PM) to induce oxidative stress in the lungs and is increasingly considered to be a relevant health metric. In this study, two complementary OP assays were deployed, including dithiothreitol (DTT) and ascorbic acid (AA) assays, to investigate the potential toxicity (as generators of oxidative stress) of respirable fractions (DD4, < 4 μm) of deposited dust (DD500, < 500 μm) in underground low-S and low-pyrite coal mines in Henan Province, Central China. The OPDTT of DD4 is higher than that reported for other types of atmospheric PM, whereas the OPAA of DD4 is similar and/or slightly higher. Cross-correlation and multilinear regression analyses are applied using datasets of major mineral and geochemical patterns in the DD4 samples and the respective OP values to identify the major drivers for OP in respirable coal dust. Thereafter, the patterns of DD4 are compared with those of DD500 and the parent coals to determine the sources of OP-relevant substances. OPDTT is mainly governed by some trace elements (Sb, As, Li, B, Sr, and Pb) and minor minerals (anatase, quartz, siderite), and their synergistic effect may be one of the reasons for the high DTT consumption. For OPAA, quartz, total clay (sum of illite, kaolinite, tobelite, and clinochlore) and Ni, Cr, Co, Si, and S, play an important role in regulating the OPAA of pyrite-free DD4 samples. These OP-relevant substances have three sources: coal dust, which has a similar composition in DD4, DD500, and the parent coal (such as siderite and its associated elements); gangue dust, which does not occur in the parent coal but is widely detected in DD4 and DD500 (such as quartz, kaolinite, and relevant elements); and cement dust (from gunite galleries), which is mainly calcite- and calcite-associated elements.
format artículo
topic_facet Source apportionment
Geochemistry
Mineralogy
Oxidative potential
Respirable dust
author Shangguan, Yunfei
Zhuang, Xinguo
Querol, Xavier
Li, Baoqing
Moreno, Natalia
Trechera, Pedro
Sola, Patricia Córdoba
Uzu, Gaëlle
Li, Jing
author_facet Shangguan, Yunfei
Zhuang, Xinguo
Querol, Xavier
Li, Baoqing
Moreno, Natalia
Trechera, Pedro
Sola, Patricia Córdoba
Uzu, Gaëlle
Li, Jing
author_sort Shangguan, Yunfei
title Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment
title_short Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment
title_full Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment
title_fullStr Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment
title_full_unstemmed Characterization of deposited dust and its respirable fractions in underground coal mines: Implications for oxidative potential-driving species and source apportionment
title_sort characterization of deposited dust and its respirable fractions in underground coal mines: implications for oxidative potential-driving species and source apportionment
publisher Elsevier
publishDate 2022-06-01
url http://hdl.handle.net/10261/271260
https://api.elsevier.com/content/abstract/scopus_id/85130291904
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