Atmospheric collection of extraterrestrial dust at the Earth's surface in the mid-Pacific

IF 2.2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Penelope J. Wozniakiewicz, Luke S. Alesbrook, John P. Bradley, Hope A. Ishii, Mark C. Price, Michael. E. Zolensky, Donald E. Brownlee, Matthias van Ginneken, Matthew J. Genge
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Abstract

The Kwajalein micrometeorite collection utilized high volume air samplers fitted with polycarbonate membrane filters to capture particles directly from the atmosphere at the Earth's surface. This initial study focused on identifying cosmic spherule-like particles, conservatively categorizing them into four groups based on bulk compositional data: Group I exhibit a range of compositions designated terrestrial in origin; group II are Fe-rich and contain only additional O, S, and/or Ni; group III are silicate spherules with Mg-to-Si At% ratios less than 0.4; group IV are silicate spherules with Mg-to-Si At% ratios greater than 0.4. Spherules in groups I, II, and III have compositions that are also consistent with particles that are produced in great numbers by natural and/or anthropogenic terrestrial activities (e.g., volcanic microspherules, fly ash from coal fired power plants, etc.) and thus are assumed terrestrial in origin. Group IV spherules exhibit compositions closest to those of cosmic spherules identified in other collections and are, therefore, designated cosmic spherule candidates. Detailed analysis of seven group IV spherules found that whilst five exhibited morphology and compositions consistent with S-type cosmic spherules, two appear unique to this collection and could not be matched to either terrestrial or extraterrestrial spherules studied to date.

Abstract Image

中太平洋地球表面地外尘埃的大气收集
夸贾林微陨石收集利用了装有聚碳酸酯膜过滤器的大容量空气采样器,直接从地球表面的大气中捕捉微粒。这项初步研究的重点是识别宇宙球状微粒,根据大量成分数据保守地将它们分为四组:第一组显示了一系列成分,被认定为源自陆地;第二组富含铁,只含有额外的 O、S 和/或 Ni;第三组是硅酸盐球粒,镁-硅 At% 比率小于 0.4;第四组是硅酸盐球粒,镁-硅 At% 比率大于 0.4。第 I、II 和 III 组球粒的成分也与自然和/或人为陆地活动产生的大量颗粒(如火山微球粒、火力发电厂产生的飞灰等)一致,因此假定其来源于陆地。第 IV 组球粒的成分最接近于在其他采集物中发现的宇宙球粒,因此被指定为宇宙球粒候选者。对 7 个第 IV 组球粒进行详细分析后发现,虽然其中 5 个球粒的形态和成分与 S 型宇宙球粒一致,但有 2 个球粒似乎是该藏品所独有的,无法与迄今为止研究过的陆地或地外球粒相匹配。
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来源期刊
Meteoritics & Planetary Science
Meteoritics & Planetary Science 地学天文-地球化学与地球物理
CiteScore
3.90
自引率
31.80%
发文量
121
审稿时长
3 months
期刊介绍: First issued in 1953, the journal publishes research articles describing the latest results of new studies, invited reviews of major topics in planetary science, editorials on issues of current interest in the field, and book reviews. The publications are original, not considered for publication elsewhere, and undergo peer-review. The topics include the origin and history of the solar system, planets and natural satellites, interplanetary dust and interstellar medium, lunar samples, meteors, and meteorites, asteroids, comets, craters, and tektites. Our authors and editors are professional scientists representing numerous disciplines, including astronomy, astrophysics, physics, geophysics, chemistry, isotope geochemistry, mineralogy, earth science, geology, and biology. MAPS has subscribers in over 40 countries. Fifty percent of MAPS'' readers are based outside the USA. The journal is available in hard copy and online.
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