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首页> 外文期刊>Elements >CATCHING A FALLING STAR (OR METEORITE) - FIREBALL CAMERA NETWORKS IN THE 21ST CENTURY
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CATCHING A FALLING STAR (OR METEORITE) - FIREBALL CAMERA NETWORKS IN THE 21ST CENTURY

机译:捕捉流星(或陨石)-21世纪的火球摄影机网络

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摘要

Have you ever seen a shooting star? Have you ever seen a fireball? They are the spectacular fiery result when space dust and rocks enter our atmosphere. Meteors (also known as shooting stars) are specks of dust that leave a trail of light as they burn up in the atmosphere. Fireballs are caused by larger bits of material, making them significantly brighter, and can last several seconds in duration. Fireballs and meteors hit the atmosphere at velocities of tens of kilometres per second. Friction from the air heats the surface of the rock, melting and ablating it, giving the impression of a ball of fire. A meteorite is the surviving material from a fireball. Meteorites give planetary scientists information about the origin and evolution of the Solar System: from how the first solids formed all the way through to the accretion of planets. Meteorites provide a scientifically priceless record, but their impact is reduced because we have no spatial context to interpret their compositional data. Imagine trying to understand the geology of a continent if all you had to work with was a collection of random rocks dumped in your yard. That is where we are with meteorites. We know meteorites come from space, mostly from the asteroid belt. We can pinpoint their precise origin in the Solar System by determining the orbit that they were on before they hit our atmosphere. However, this is only possible if we are able to track the fireball before it lands. Combining the orbit with the recovered meteorite is a major step towards interpreting the record of early Solar System processes that meteorites contain.
机译:你见过流星吗?你见过火球吗?当太空尘埃和岩石进入我们的大气层时,它们是壮观的火热结果。流星(也称为流星)是尘埃斑点,它们在大气层中燃烧时会留下一丝光线。火球是由较大的材料碎片引起的,使它们明显更亮,可以持续几秒钟。火球和流星以每秒数十公里的速度撞击大气层。空气的摩擦会加热岩石的表面,使其融化并烧蚀,给人留下火球的印象。陨石是火球中幸存的物质。陨石为行星科学家提供了有关太阳系起源和演化的信息:从最初的固体如何形成一直到行星的积聚。陨石提供了科学上无价的记录,但由于我们没有空间背景来解释其组成数据,因此减少了陨石的影响。想象一下,如果您要处理的只是堆放在院子里的随机岩石的集合,便想了解一个大陆的地质情况。那就是我们与陨石在一起的地方。我们知道陨石来自太空,主要来自小行星带。我们可以通过确定它们在撞击我们的大气之前所处的轨道来确定它们在太阳系中的确切起源。但是,这只有在我们能够在火球降落之前对其进行跟踪的情况下才有可能。将轨道与回收的陨石结合是迈向解释陨石包含的早期太阳系过程记录的重要一步。

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  • 来源
    《Elements》 |2015年第3期|160-161|共2页
  • 作者单位

    Curtin University, Department of Applied Geology, Perth, WA, Australia;

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