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Long-range transport of giant particles in Asian dust identified by physical, mineralogical, and meteorological analysis

机译:通过物理,矿物学和气象学分析确定亚洲尘埃中巨大颗粒的远距离传输

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Giant particles transported over long distances are generally of limitedconcern in atmospheric studies due to their low number concentrations inmineral dust and possible local origin. However, they can play an importantrole in regional circulation of earth materials due to their enormous volumeconcentration. Asian dust laden with giant particles was observed in Korea on31 March 2012, after a migration of about 2000 km across the Yellow Sea fromthe Gobi Desert. Scanning electron microscopy (SEM) revealed that 20% ofthe particles exceeded 10 μm in equivalent sphere diameter, with amaximum of 60 μm. The median diameter from the number distributionwas 5.7 μm, which was larger than the diameters recorded of 2.5 and2.9 μm in Asian dust storms in 2010 and 2011, respectively, and wasconsistent with independent optical particle counter data. Giant particles(>10 μm) contributed about 89% of the volume of thedust in the 2012 storm. Illite–smectite series clay minerals were the majormineral group followed by quartz, plagioclase, K-feldspar, and calcite. Thetotal phyllosilicate content was ~52%. The direct long-rangetransport of giant particles was confirmed by calcite nanofibers closelyassociated with clays in a submicron scale identified by high-resolution SEMand transmission electron microscopy. Since giant particles consisted of clayagglomerates and clay-coated quartz, feldspars, and micas, the mineralcomposition varied little throughout the fine (<5 μm),coarse (5–10 μm), giant-S (10–20 μm), and giant-L(>20 μm) size bins. Analysis of the synopticconditions of the 2012 dust event and its migration indicated that themid-tropospheric strong wind belt directly stretching to Korea induced rapidtransport of the dust, delivering giant particles. Giant dust particles withhigh settling velocity would be the major input into the terrestrial andmarine sedimentary and ecological systems of East Asia and the westernPacific. Analysis of ancient aeolian deposits in Korea suggested the commondeposition of giant particles from Asian dust through the late QuaternaryPeriod. The roles of giant particles should be reviewed with regard toregional circulation of mineral particles and nutrients.
机译:在大气研究中,长距离运输的巨型颗粒通常受到关注,因为它们的矿物质尘埃含量低,并且可能是当地来源。然而,由于其巨大的体积浓度,它们可以在地球材料的区域循环中发挥重要作用。 2012年3月31日,在韩国从戈壁沙漠横渡约2000公里的黄海之后,在韩国观察到了充满大颗粒的亚洲尘埃。扫描电子显微镜(SEM)显示,当量球直径中有20%的颗粒超过10μm,最大为60μm。数量分布的中值直径为5.7μm,分别大于2010年和2011年亚洲沙尘暴记录的直径2.5和2.9μm,并与独立的光学粒子计数器数据一致。在2012年的风暴中,巨大的颗粒(> 10μm)贡献了约89%的粉尘。伊利石-蒙脱石系列粘土矿物是主要矿物类,其次是石英,斜长石,钾长石和方解石。层状硅酸盐总量约为52%。方解石纳米纤维与粘土密切相关,通过高分辨率SEM和透射电子显微镜鉴定出亚微米级的方解石纳米纤维,证实了巨颗粒的直接远距离传输。由于巨型颗粒由粘土团聚体和粘土包覆的石英,长石和云母组成,因此在细颗粒(<5μm),粗颗粒(5–10μm),巨型S(10–20μm)和巨型颗粒中,矿物成分变化很小-L(> 20μm)尺寸的纸槽。对2012年尘埃事件及其迁徙的天气条件进行的分析表明,直接延伸到韩国的对流层中强风带引起了尘埃的快速输送,传递了巨大的颗粒。具有高沉降速度的巨大粉尘颗粒将成为东亚和西太平洋陆地和海洋沉积和生态系统的主要输入。对韩国古代风成矿的分析表明,在第四纪末期,亚洲尘埃中的大颗粒普遍沉积。应当就矿物颗粒和养分的区域循环来审查巨型颗粒的作用。

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