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第1段

1 .<-NARRATOR:->Listen to part of a lecture in an astronomy class.

旁白:请听一段天文学讲座的节选片段。

第2段

1 .<-MALE PROFESSOR:->Last week we discussed the formation of Earth and the other rocky planets-the planets in the inner solar system.

教授:上一周我们讨论了地球以及其他岩态行星的形成,这些行星位于太阳系内部。

2 .Uh, s-so what about the gas giants: Jupiter, Saturn, Uranus, and Neptune?

哦,那么,气态行星是怎么形成的呢?比如说木星、土星、天王星和海王星。

3 .Well, there's two theories, but first let's recap.

现在有两种理论。但是首先,我们先简要回顾一下上节课的内容。

4 .We believe our solar system began as a huge spinning cloud of dust and gas, which flattened and eventually collapsed in on itself.

我们相信太阳系始于一大团旋转的尘土和气体的云团,这一团云团最终变平并且自己瓦解。

5 .The matter at the center condensed into a ball of hot gas and dust, eventually becoming our Sun.

它的物质浓缩成了一个热气和尘土构成的球,最终变成了太阳。

6 .And... what happened to the remaining cloud, to the disk encircling the Sun when it was a young star?

那么剩下的云层又变成了什么呢?在太阳还是一颗新生恒星的时候,作为环绕它的气体带?

第3段

1 .<-FEMALE STUDENT:->The rocky planets were born. Um, dust- little grains of rock and metal within the disk collided with each other and stuck together.

学生:岩态行星就形成了。嗯,灰尘、小的岩石碎片和气体带里的金属物质互相碰撞,彼此聚合,

2 .And this process sorta snowballed over millions of years... until the chunks grew into mini-planets-protoplanets.

这个过程就类似于一场百万年的滚雪球,直到这些碎片变成了小行星和原行星。

第4段

1 .<-MALE PROFESSOR:->Yes. Uh, this process is called accretion, and we call the disk an accretion disk.

教授:是的。这个过程被称为吸积。我们把这个环叫做吸积盘。

第5段

1 .[Explaining] Now... think of it as two parts- an inner accretion disk and an outer accretion disk.

我们把它分成两个部分来考虑:内部的吸积盘和外部的吸积盘。

2 .In the inner part, once an object gets large enough, that object's gravitational field gets stronger, which speeds up the accretion process.

在内部的吸积盘里,一旦一个物体变得足够大,它的重力就会变得更大,这就加速了吸积的过程。

3 .You know, larger objects attract smaller ones and sorta gobble them up. And eventually you get a full-size planet in its own orbit.

你知道,大的物体会吸引小的物体,把它们都“吞吃”掉。最终,我们就得到了一个有自己轨道的足尺的行星。

4 .OK... That's how the inner rocky planets probably formed-by accretion. But what about those gas planets in the outer solar system, in the outer accretion disk?

好的。这就是内部的岩态行星怎么通过吸积作用形成。但是那些位于太阳系外部、处于外部吸积盘内的气态行星,是怎么形成的呢?

第6段

1 .Well, the first theory says the accretion process was similar to the one that formed the rocky planets, with some key differences.

第一个理论认为,形成气态行星的吸积过程与形成岩态行星的吸积过程相似,但是有几个关键的不同。

2 .Remember the gas giants are farther from the Sun, where temperatures are much colder.

记得吗,气态行星距离太阳更远,在它们所处的位置,温度是更低的。

3 .So, in the outer accretion disk, compounds like water and ammonia exist in frozen form.

所以,在外部的吸积盘里,水和氨气的混合物是以冰冻状态存在的。

4 .Closer to the Sun, they're more likely to be vaporized by solar radiation.

离太阳越近,这种化合物就更有可能在太阳辐射下蒸发成气体。

5 .What this means is that, in addition to rocky and metallic particles, there's be other solids, like frozen water and frozen ammonia.

这就意味着除了岩石和金属颗粒,还有其他的固体比如说冰和固态氨气。

第7段

1 .<-FEMALE STUDENT:->[Following on]...so more solid substances are available to clump into protoplanets, right?

学生:所以越来越多的固体物质可以聚成原行星,对吗?

第8段

1 .<-MALE PROFESSOR:->Precisely. So the solid cores of the gas giants could conceivably have formed by accretion.

教授:很准确!所以可以想象的是气态行星的固态核心可以通过吸积作用形成。

2 .And once their mass reaches a certain point- around about five to ten Earths- what would happen?

一旦它们的质量达到了地球的5到10倍,什么事情会发生呢?

第9段

1 .<-FEMALE STUDENT:->Five to ten Earths? With a mass that big, I guess gravity would start to pull in more and more material faster, right?

学生:地球质量的5到10倍的话……嗯,如果质量如此之大的话,我猜重力会越来越快地把其他物质吸引过来,对吗?

2 .<-MALE PROFESSOR:->Material, meaning gas. It would rapidly pull in more and more gas from the accretion disk.

教授:物质,也就是气体。这个巨大的行星会迅速地从吸积盘里吸引越来越多的气体。

3 .So, you end up with a solid core of rock, metal, and ice surrounded by massive amounts of gas. That's the core-accretion theory.

所以我们就得到了一个由岩石、金属和冰组成的核,这个核由大量的气体包围着。这就是核吸积理论。

4 .Now-the other theory's called the disk-instability theory.

第二个理论被称为吸积盘无用论理论。

第10段

1 .The disk-instability theory holds that gas begins the planet-making process without a solid core.

吸积盘无用论理论认为,气体开始了行星形成的过程,这时候并没有一个固态的核心。

2 .You see, most of the outer accretion disk would've been gas; we believe solid particles probably made up just 1 percent of the outer accretion disk.

你看,大多数的外部吸积盘的构成都是气体。我们相信,固态粒子可能只占外部吸积盘的百分之一。

3 .So, this theory suggests that the large planets-the gas giants- they develop from large clumps of mostly gas and some dust in an accretion disk.

所以这个理论认为,大的行星,气态大行星,嗯,它们是形成于大团的吸积盘的气体和灰尘。

4 .Um, outer regions of an accretion disk can be unstable, uh, gravitationally unstable, which is what causes these clumps to form and, in some cases, grow into protoplanets.

吸积盘的外部区域是不稳定的,在重力上是不稳定的,这就导致了大团气体的形成,在某些情况下,这就导致了原行星的形成。

5 .Over time, dust particles within a gas clump coalesce-bond together-and eventually fall toward the center, creating a core.

经过较长时间,大团气体里的尘埃粒子聚合在了一起,最终向中心积聚,形成了一个核。

6 .Once this happens, the gas clump grows relatively quickly, as its gravity pulls in more and more gas and dust particles.

这个过程一旦发生,大团气体就变大地非常快,因为它的重力会吸引来越来越多的气体和尘土粒子。

7 .And this whole process can theoretically happen within 100,000 years.

这整个过程在理论上可以在十万年之间发生。

第11段

1 .<-FEMALE STUDENT:->That's amazingly fast! So, which theory's correct?

学生:真是令人吃惊地快啊!那么哪个理论是正确的呢?

第12段

1 .<-MALE PROFESSOR:->That's the debate. Most of my colleagues favor core accretion.

教授:这就是争论所在。我的同事们多数支持核吸积理论。

2 .Personally, I think the accretion theory works for the formation of rocky planets, but not necessarily for gas planets.

我个人认为核吸积理论适用于岩石星球的形成,但是对气体星球不一定成立。

3 .A major problem is that gas giants like Jupiter and Saturn would take too long to form through core accretion.

一个大问题在于巨大的气体星球,像木星和土星,如果通过核吸积的话耗费的时间就太长了。

4 .Core accretion would take several million years. But observations of other star systems indicate that a disk's gas disappears more quickly than that.

核吸积可能会耗费数百年的时间。但是对其他行星系统的观测证明盘状气体会更快消失。

5 .Whatever's not drawn into planets ends up dissipated and evaporated by solar wind and radiation, from nearby stars.

对于任何没有被吸引到星球上的东西都会被周围星系的太阳风、辐射分散和蒸发。

6 .So basically, a baby Jupiter would run out of gas before it grew up.

因此,基本上一个在木星形成之前就会耗尽所有的气体。

7 .But the disk-instability theory... well, the timing's right. That process is fast enough to finish before the gas runs out.

但是盘吸积理论,如果时间是对的话,这个过程会在气体耗尽之前就完成。