Scientists: Evidence of Crash with Another Planet under Earth's Surface

2023-11-14 13:48:49来源:网络

Scientists: Evidence of Crash with Another Planet under Earth's Surface

科学家:地球表面下另一颗行星坠毁的证据

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  By John Russell

  12 November 2023

  Scientists have recognized since the 1970s that there are two large, mysterious blobs in the deepest part of Earth's mantle.

  One of the masses is under Africa and the other under the South Pacific Ocean.

  Recent research suggests these masses, which are denser than the material surrounding them, might be from a huge crash early in our planet's history.

  Researchers recently said the crash between Earth and a Mars-sized object called Theia might have created the moon.

  Recent research suggests the event happened more than 4.46 billion years ago. Pieces of Theia, however, might have remained inside Earth, sinking to an area just above our planet's hot core of iron and nickel.

  Researchers created computer simulations to study their theory of the event. Based on these simulations, they proposed that most of Theia was absorbed into Earth, forming the two masses, while the remaining pieces formed the moon.

  Qian Yuan is a geophysicist at Caltech and the lead writer of the study that was published recently in Nature.

  "The bottoms of these blobs are 2,900 kilometers below our feet. The two blobs are about 2 percent of Earth's mass. They were detected by seismology as seismic waves travel slower within these two regions compared to the surrounding mantle. Each of the blobs are twice the mass of the whole moon. So, the blobs are massive," Yuan said.

  If the theory is correct, these two masses would represent evidence of the possible moon-forming crash.

  Caltech professor and study co-writer Paul Asimow said there has not been agreement "on whether we can find evidence for this event not just in the moon but also in some observable property of the modern Earth."

  The two masses, Asimow added, are the biggest difference "in Earth structure from a simple layered planet."

  Study co-writer Hongping Deng of the Chinese Academy of Sciences' Shanghai Astronomical Observatory said, "It is incredible because we can uncover relics of another planet - Theia - if we dig deep enough in Earth's mantle."

  The increased density of the masses is believed to come from their high level of iron. Moon rocks also contain high iron levels. So, the researchers think it would make sense if they came from the same place: Theia.

  The moon, which orbits Earth at an average distance of about 385,000 km, has a diameter of about 3,475 km, a bit more than a quarter of our planet's diameter.

  Asimow said that, if the theory is correct, some volcanic rocks that reach Earth's surface might provide pieces of Theia.

  "If our model is correct, the blobs should have isotopes - trace elements - that are similar to the lunar mantle rocks, which can be tested in future lunar missions," Yuan said.

  Gaining a greater understanding of the hypothesized giant impact could provide information concerning the evolution of Earth and other rocky planets in our solar system and beyond it.

  "Earth is still the only confirmed habitable planet, and we do not know why," Yuan said. He added the crash set the early conditions for Earth's development and said: "Studying its consequences may help us to figure out why Earth is different than other rocky planets."

  I'm John Russell.

  Will Dunham reported on this story for Reuters. John Russell adapted it for VOA Learning English.

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  约翰·罗素

  日期:2023年11月12日

  自1970年代以来,科学家们就已经发现,在地球最深的地幔部分有两个大而神秘的团块。

  其中一个团块位于非洲下方,另一个位于南太平洋海底下方。

  最近的研究表明,这些比周围物质更密的团块,可能来自于我们星球早期的一次巨大碰撞。

  研究人员最近表示,地球与一个名为希亚的火星大小的物体之间的碰撞可能创造了月球。

  最近的研究表明,这次事件发生在46亿多年前。然而,希亚的一部分可能仍然留在地球内部,沉降到我们星球炽热的铁和镍核心之上的区域。

  研究人员创建了计算机模拟来研究他们的事件理论。基于这些模拟,他们提出,希亚的大部分被吸收进地球,形成了这两个团块,而剩下的部分形成了月球。

  钱源是加州理工学院的一位地球物理学家,他是最近在《自然》杂志上发表的这项研究的主要作者。

  "这些团块的底部离我们的脚下有2900公里远。这两个团块约占地球质量的2%。通过地震学检测到它们,因为地震波在这两个区域内的传播速度比在周围的地幔中慢。每个团块的质量是整个月球的两倍。所以,这些团块是巨大的,"钱源说。

  如果这个理论是正确的,那么这两个团块将代表可能形成月球的碰撞的证据。

  加州理工学院的教授和研究报告的合著者保罗·阿西莫夫说,人们一直没有达成一致,“我们是否能在月球以外的现代地球的某些可观察属性中找到这次事件的证据。”

  阿西莫夫补充说,这两个团块是“地球结构与简单分层行星的最大区别。”

  中国科学院上海天文台的研究报告合著者邓洪平说,“这是令人难以置信的,因为如果我们在地球的地幔深处挖掘足够深,我们可以发现另一个行星——希亚的遗迹。”

  人们认为,这些团块的密度增加是由于它们含有高含量的铁。月球岩石也含有高含量的铁。因此,研究人员认为,如果它们来自同一个地方——希亚,这是有道理的。

  月球环绕地球运行,平均距离约为385,000公里,直径约为3,475公里,略大于我们星球直径的四分之一。

  阿西莫夫说,如果这个理论是正确的,那么一些到达地球表面的火山岩可能会提供希亚的碎片。

  钱源说:“如果我们的模型是正确的,那么这些团块应该有与月球地幔岩石相似的同位素——微量元素,这可以在未来的月球任务中进行测试。”

  对假设的巨大撞击有更深入的理解,可能会提供关于地球和我们太阳系以及其之外的其他岩石行星演化的信息。

  "地球仍然是唯一被确认的适宜居住的星球,我们不知道为什么,"钱源说。他补充说,这次撞击设定了地球早期的发展条件,并说:“研究其后果可能会帮助我们弄清楚为什么地球与其他岩石行星不同。”

  我是约翰·罗素。

  这个故事是由路透社的Will Dunham报道的,约翰·罗素为VOA学习英语改编了它。

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  这个故事中的词语

  blob -- n. (非正式)没有规则形状的东西

  mantle -- n. 地球的中间层,位于顶部地壳和内核之间

  core –n. 某物的中心部分,如地球

  simulation -- n.使某物看起来、感觉或行为像其他东西的东西

  absorb –v. 吸收某种物质,尤其是液体

  seismology -- n. 地震的科学研究

  relic -- n. 来自过去的时间或地方的东西

  isotope -- n. 同一化学元素的各种形式之一

  trace –adj.以小量存在的

  habitable –adj. 可居住的;能够支持生命的

  consequences –n. (复数)事件或决定的结果


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