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DOI10.1016/j.atmosres.2020.105227
Spatial distribution and potential sources of methanesulfonic acid in High Asia glaciers
Li Y.; Wang N.; Barbante C.; Kang S.; Niu H.; Wu X.; Barbaro E.; Argiriadis E.; Dong Z.; Wang S.; Gambaro A.; Li Q.
发表日期2021
ISSN0169-8095
卷号248
英文摘要As a receptor of atmospheric deposition, glaciers are considered an ideal archive in the study of climate change and geochemical cycles. The deposition of methanesulfonic acid (MSA) in the glaciers provides good opportunities to study the biogeochemical cycle of sulfur in the cryosphere. In the present work, snow samples were collected from six High Asia glaciers along a north-to-south transect to determine the spatial distribution of MSA and elucidate its potential sources. The median MSA concentration in the Urumqi Glacier No.1 of Tien Shan was 138.8 ng mL−1, which was distinctly higher than those observed in the Tibetan Plateau (TP) glaciers and polar regions. The levels of MSA in the interior TP glaciers were higher than those observed in the margins of northeastern and southeastern TP. Good correlations between MSA and K+ (r = 0.86, n = 30, α = 0.01), Mg2+ (r = 0.86), and NH4+ (r = 0.73) were observed in continental glaciers. Principal component analysis indicated that MSA may have terrigenous material inputs. At Yulong Snow Mountain, MSA was correlated with Na+ (r = 0.76, n = 8, α = 0.1), a sea-salt tracer ion, suggesting that MSA may be derived from marine environments. According to dimethyl sulfide (DMS) production and NH3 emissions in High Asia, we deduced that the high concentrations of MSA in continental glaciers are possibly related to the sources of hypersaline soil environments and animal husbandry in nomadic areas. This work is useful for further studies on regional sulfur cycling and the impacts of human activities on climate change. © 2020 Elsevier B.V.
英文关键词Glacier; High Asia; Methanesulfonic acid; Sources; The Tibetan Plateau
语种英语
scopus关键词Ammonia; Biogeochemistry; Deposition; Meteorological problems; Organic acids; Snow; Soil pollution; Spatial distribution; Sulfur compounds; Atmospheric depositions; Biogeochemical cycle; Dimethyl sulfide; Geochemical cycles; Good correlations; Marine environment; Methane sulfonic acid; Potential sources; Climate change; anthropogenic effect; atmospheric deposition; climate change; glacier; source identification; spatial distribution; sulfonate; sulfur cycle; China; Qinghai-Xizang Plateau; Urumqi Glacier No.1; Xinjiang Uygur; Yulong Snow Mountains; Yunnan; Animalia
来源期刊Atmospheric Research
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/141693
作者单位State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, 730000, China; Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Xi'an, 710127, China; Institute of Earth Surface System and Hazards, Northwest University, Xi'an, 710127, China; College of Urban and Environmental Sciences, Northwest University, Xi'an, 710127, China; Institute of Polar Sciences-CNR, Venice-Mestre, 30172, Italy; Department of Environmental Sciences, Informatics and Statistics, Ca’ Foscari, University of Venice, Venice-Mestre, 30172, Italy; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100085, China; University of Chinese Academy of Sciences, Beijing, 100049, China
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Li Y.,Wang N.,Barbante C.,et al. Spatial distribution and potential sources of methanesulfonic acid in High Asia glaciers[J],2021,248.
APA Li Y..,Wang N..,Barbante C..,Kang S..,Niu H..,...&Li Q..(2021).Spatial distribution and potential sources of methanesulfonic acid in High Asia glaciers.Atmospheric Research,248.
MLA Li Y.,et al."Spatial distribution and potential sources of methanesulfonic acid in High Asia glaciers".Atmospheric Research 248(2021).
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