Official 05 Set 3

  • Q1
  • Q2
  • Q3
  • Q4
  • Q5
  • Q6

Moon Landing

  • Q1
  • Q2
  • Q3
  • Q4
  • Q5
  • Q6
What is the main purpose of the lecture?
  • A. To explain why scientists disagree about the age of the Moon

  • B. To present arguments in favor of another Moon landing

  • C. To explain how scientists discovered a crater on the far side of the Moon

  • D. To review some finding of a recent mission to the Moon

显示答案 正确答案: B

我的笔记 编辑笔记

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    NARRATOR:Listen to part of a lecture in an Astronomy Class.

    MALE PROFESSOR:Last week, we covered some arguments against going back to the Moon.But there are compelling reasons in favor of another Moon landing too, um... not the least of which is trying to pinpoint the moon's age.

    We could do this in theory by studying an enormous impact crater, known as the South Pole–Aitken Basin.Um... it's located in the moon's South Polar Region.But, since it's on the far side of the moon, it can only be seen from space.

    Here is an image of… we'll call it the SPA Basin.This color-coated image of the SPA Basin—those aren't its actual colors obviously—this image is from the mid 90s, from the American spacecraft called Clementine.Um... unlike earlier lunar missions, Clementine didn't orbit only around the moon's equator.Its orbits enable it to send back data to create this topographical map of…well, the gray-and-white area towards the bottom is the South Pole, the purples and blues in the middle correspond to low elevations—the SPA Basin itself, the oranges and reds around it are higher elevations.

    The basin measures an amazing 2,500 km in diameter, and its average depth is 12 km.That makes it the biggest known crater in our solar system and it may well be the oldest.You know planetary researchers love studying deep craters until learn about the impacts that created them, how they redistributed pieces of a planet's crust and in this case, we especially want to know if any of the mantle, the layer beneath the crust, was exposed by the impact.Not everyone agrees, but some experts are convinced that whatever created the SPA Basin did penetrate the Moon's mantle.And we need to find out, because much more than the crust, the mantle contains information about a planet's or Moon's total composition.And that's key to understanding planet formation.Um... Dian?

    FEMALE STUDENT:So the only way to know the basin's age is to study its rocks directly?

    MALE PROFESSOR:Well, from radio survey data, we know that the basin contains lots of smaller craters.So it must be really old—about 4 billion years, give or take a few hundred million years.But that's not very precise.If we had rock samples to study, we'd know whether the small craters were formed by impacts during the final stages of planetary formation, or if they resulted from later meteor showers.

    But if we know around how old the Basin is, I'm not sure that's reason enough to go to the Moon again.

    No... but such crude estimates, um... we can do better than that.

    Besides, there are other things worth investigating, like is there water ice on the moon?Clementine's study indicated that the wall of the south-polar crater was more reflective than expected.So some experts think there's probably ice there.Also, data from a later mission indicates significant concentrations of hydrogen and by inference water less than a meter underground at both poles.

    Well if there's water, how did it get there? Underground rivers?

    We think meteors that crashed into the moon or tails of passing comets may have introduced water molecules.Any water molecules that found their way to the floors of craters near the moon's poles, that water would be perpetually frozen, because the floors of those craters are always in shadow.Um... furthermore, if the water ice was mixed in with rock and dust, it would be protected from evaporation.

    So are you saying there might be primitive life on the moon?

    That's not my point at all.Um... OK, say there is water ice on the moon.That would be a very practical value for a future moon base for astronauts.Water ice could be melted and purified for drinking.It could also be broken down into its component parts - oxygen and hydrogen.Oxygen could be used to breathe, and hydrogen could be turned into fuel, rocket fuel.So water ice could enable the creation of a self-sustaining moon base someday, a mining camp perhaps or a departure point for further space exploration.

    But holding tons of equipment to the moon to make fuel and build a life support system for a moon base, wouldn't that be too expensive?

    Permanent base, maybe a ways off, but we shouldn't have to wait for that.The dust at the bottom of the SPA Basin really does have a fascinating story to tell.I wouldn't give for a few samples of it.

  • 旁白:听一部分天文学的课程。



    我这里有一张图片。我们将之命名为SPA 盆地。可以看到盆地上一层着色的图层,很明显这不是真实的月球的颜色。这张图拍摄于九十年代中期,来自名为克莱门的宇宙飞船。嗯,不像早些时候的月球探测一样,克莱门飞船并没有仅仅沿着月球的轨道飞行。这种特殊的飞行使得飞船能够发送数据回地球,从而得出这张地形图。延伸到底部的灰白区域是南极,中间紫色和蓝色的部分是海拔较低的地带,即SPA 盆地,它周围的橙红色地带,海拔较高。

    该盆地直径竟达2500 千米,平均深度达到12 千米。这使得它成为了太阳系中已知的最大的撞击坑,很可能也是年代最久远的。我们知道,行星研究人员喜欢研究撞击深坑直到了解产生它们的影响,它们是怎么重新分配行星的地壳物质,并且在这种情况下,我们特别想知道,地壳下层的地幔是否受撞击影响而被裸露在外。不是所有人都同意这样的说法,但是某些专家坚信不管什么东西使SPA 盆地形成,它都会穿透月球的地幔层。由于地幔层包含信息比地壳层要多得多,我们需要找出地幔层包含关于行星或是月球总体成分的信息。这是了解行星形成的关键所在。嗯...Dian?


    教授:嗯,通过无线电调查的数据显示,我们知道盆地里有很多较小的火山口。因此应该有一定历史了,大概40 亿年,或多或少有几亿年的误差。但也不是很精确。如果我们研究岩石样本,我们就知道小火山口是不是在行星形成的最后阶段影响而形成的,或者是否由于最近的流星雨造成的。









    永久基地,也许是一种解决方式,但我们不需要等那么久。SPA 盆地底部的灰尘蕴藏着非常有趣的故事。我不会错失一些样本的。

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  • 本题对应音频:
    8 感谢 不懂



    Last week, we covered some arguments against going back to the Moon. But there are compelling reasons in favor of another Moon landing, too, um, not the 

    least of which is trying to pinpoint the Moon’s age.


    文章的一开始,教授就说到有一些compelling reasons支持另一次登月计划,之后的文章也在讲登月会有什么收获,对应着答案B。

    A选项,why disagree未提及。C选项,如何发现crater未提及。D选项,是不是recent mission发现的,未提及。





Moon Landing