Spatial Variability and Source Identification of Trace Elements in Aerosols From Northwest Pacific Marginal Sea, Indian Ocean and South Pacific to Antarctica

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES Global Biogeochemical Cycles Pub Date : 2024-09-04 DOI:10.1029/2024GB008235
Yuncong Ge, Wenkai Guan, Kuo Hong Wong, Ruifeng Zhang
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Abstract

Aerosols continuously transport trace elements (TEs) across long distances to the ocean, fueling marine primary production and affecting global carbon cycles. Given the multiple sources and complex transport mechanisms, field investigations of aerosol TEs on a global scale are significant for understanding their role in marine biogeochemical cycles. Here, aerosol samples were collected along a 50,000-km route covering subtropical Northwest Pacific (NWP) marginal seas, Indian Ocean, Southern Ocean, Drake Passage, and South Pacific. Samples were analyzed for the concentrations of Al, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, As, Cd, Tl, and Pb. Aerosol TEs were distributed heterogeneously, with significantly lower concentrations over remote oceans compared to coastal seas. Meanwhile, TE concentrations were generally high in the Indian Ocean, moderate in the Southern Ocean, and low in the South Pacific. Cr, Ni, Cu, Zn, Cd, As, and Pb were widely enriched, primarily originating from anthropogenic sources, while Al, Ti, V, Mn, Fe, and Co were mainly from crustal sources in remote oceans. Moreover, specific sources of TEs were clarified, for example, Cr and Ni were mainly from vehicle emissions. The estimated bulk TE deposition fluxes also varied spatially. For instance, the greatest deposition of Fe occurs in the NWP marginal sea, followed by the Drake Passage, Indian Ocean Sector of Southern Ocean, Pacific Sector of Southern Ocean, and South Pacific. This study contributes to a deeper understanding of the complex dynamics of aerosol TEs in the global ocean, providing valuable information for future studies and policy making regarding climate change.

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西北太平洋边缘海、印度洋和南太平洋至南极洲气溶胶中痕量元素的空间变异性和来源识别
气溶胶不断将痕量元素(TEs)远距离迁移到海洋中,促进海洋初级生产并影响全球碳循环。鉴于气溶胶的多种来源和复杂的传输机制,在全球范围内对气溶胶痕量元素进行实地调查对于了解它们在海洋生物地球化学循环中的作用意义重大。在此,我们沿一条长达 5 万公里的路线收集了气溶胶样本,覆盖了亚热带西北太平洋(NWP)边缘海、印度洋、南大洋、德雷克海峡和南太平洋。对样本中的铝、钛、钒、铬、锰、铁、钴、镍、铜、锌、砷、镉、碲和铅浓度进行了分析。气溶胶 TE 分布不均,偏远海洋的浓度明显低于沿海海洋。同时,印度洋的 TE 浓度普遍较高,南大洋的浓度适中,而南太平洋的浓度较低。铬、镍、铜、锌、镉、砷和铅广泛富集,主要来自人为来源,而铝、钛、钒、锰、铁和钴则主要来自偏远海洋的地壳来源。此外,还明确了 TE 的具体来源,例如,铬和镍主要来自汽车尾气排放。估计的大量 TE 沉积通量在空间上也存在差异。例如,最大的铁沉积发生在西北太平洋边缘海,其次是德雷克海峡、南大洋印度洋区、南大洋太平洋区和南太平洋。这项研究有助于加深对全球海洋中气溶胶 TEs 复杂动态的理解,为未来气候变化研究和政策制定提供宝贵信息。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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