跟读练习: Where Did Earth's Water Come From? - 通过视频学习英语口语
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Unlike every other planet in our solar system, Earth's surface is 70 % liquid water, which while useful for life, is also kind of weird,
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because everything we know about how and when our planet formed says Earth's surface should be bone dry.
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The story goes like this.
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Our solar system formed from the collapse of a large cloud of dust and gas.
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The dense blob of gas at the center ignited to form the sun, which as a young unstable star unleashed a fierce solar wind.
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And over time, this stream of charged particles pushed the remaining gas cloud farther and farther out, leaving only solid particles behind to clump together into rocks,
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planetesimals, and finally, the rocky planets of the inner solar system that we know today.
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And here's the problem.
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Water, in the form of ice, couldn't have been one of the solid particles that stuck around to form our planet, because the early inner solar system was far too hot for frozen water,
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and any water vapor would have been blasted away by the solar wind.
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So if Earth didn't start off with water, how did we end up with such splendid oceans?
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We know H2O wasn't manufactured here over the eons, because natural processes like combustion,
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breathing and photosynthesis create and destroy roughly equal amounts of water, and either way, the amounts in question are so minuscule that they can't account for the abundance of water on the planet.
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Since Earth's water was neither part of the original package nor manufactured here, it must have flown in from far away, on meteoroids or comets or other bodies originating in the outer solar system,
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where they were far enough from the sun for frozen water to survive.
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The dirty ice balls we call comets are a logical candidate for the source of our water, but were ruled out when we discovered that they were far richer in heavy hydrogen than earth water.
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Heavy hydrogen has a neutron as well as a proton in its nucleus, and for every million hydrogen atoms in earth water, about 150 are heavy ones,
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while typical comet water has twice that many.
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These mismatched chemical signatures suggest that Earth's water couldn't have arrived on comets.
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It turns out that the most likely source for Earth's water is a type of meteorite called a carbonaceous chondrite.
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Chondrite is just the name given to the class of stony meteoroids that most commonly strike the Earth.
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But only the carbonaceous chondrites contain water, as well as lots of carbon if you couldn't tell from their name.
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They have water in them because they formed out beyond the sun's frost line, and what's more, their water has levels of heavy hydrogen similar to that of earth water,
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strongly suggesting that these earth crashers are the source of our ice caps, clouds, rivers, and oceans.
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And thus the water that turned our planet into a blue marble came, quite literally, out of the blue.
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本课的词汇与口语要点
这节 B2 级别的口语课以视频“Where Did Earth's Water Come From?”为素材。 视频中反复出现的词有:solar, planet, earth, comet, hydrogen。 这段视频共有 25 个句子、496 个单词可供跟读。 讲话部分时长为 2:24。 说话人语速较快,每分钟约 206 个词,会出现较多连读和弱读。 只有 80% 的单词属于英语最常用的 3,000 词,词汇难度较高。
视频中的重点词汇
视频中最难的 15 个单词,附发音和释义:
| 单词 | 发音 | 释义 |
|---|---|---|
| comet 名词 | /ˈkɒmɪt/ | 彗星, 掃帚星 /扫帚星 |
| hydrogen 名词 | /ˈhaɪdɹəd͡ʒ(ə)n/ | 氫 /氢 |
| chondrite 名词 | /ˈkɒndɹaɪt/ | 球粒狀隕石 /球粒状陨石 |
| particle 名词 | /ˈpɑɹtək(ə)l/ | 粒子 |
| freeze 动词 | /ˈfɹiːz/ | 凍結 /冻结, 凍 /冻 |
| ignite 动词 | /ɪɡˈnaɪt/ | 點火 /点火, 點燃 /点燃 |
| meteorite 名词 | /ˈmi.ti.əˌɹaɪt/ | 隕石 /陨石 |
| minuscule 名词 | /ˈmɪnəˌskjul/ | 小寫字母 /小写字母 |
| neutron 名词 | /ˈnu.tɹɑn/ | 中子 |
| photosynthesis 名词 | /ˌfoʊ.toʊˈsɪn.θə.sɪs/ | 光合作用 |
| proton 名词 | /ˈpɹoʊ.tɑn/ | 質子 /质子 |
| unleash 动词 | /ʌnˈliʃ/ | 釋放 /释放, 放開 /放开 |
| vapor 名词 | /ˈveɪpɚ/ | 蒸氣 /蒸气 |
| combustion 名词 | /kəmˈbʌs.t͡ʃən/ | 燃燒 /燃烧 |
| nucleus 名词 | /ˈnuː.kli.əs/ | 核心, 核 |
视频中出现的短语动词
| 单词 | 释义 |
|---|---|
| rule out 动词 | 排除 |
| turn out 动词 | 原來 /原来 |
需要注意的发音
说话人用了 6 次缩略和弱读形式,例如 couldn't, can't, didn't。请按听到的简短形式来说。
- “sh” 和 “zh” 音: carbonaceous /kɑːbəˈneɪʃəs/, unleash /ʌnˈliʃ/
- 长单词——注意重音位置: carbonaceous /kɑːbəˈneɪʃəs/, meteorite /ˈmi.ti.əˌɹaɪt/, originate /əˈɹɪd͡ʒɪneɪt/, photosynthesis /ˌfoʊ.toʊˈsɪn.θə.sɪs/
中文母语者容易读错的音:
- 词尾辅音 — 要读清楚,后面不要加元音: comet /ˈkɒmɪt/, chondrite /ˈkɒndɹaɪt/, carbonaceous /kɑːbəˈneɪʃəs/, freeze /ˈfɹiːz/, ignite /ɪɡˈnaɪt/
- /r/ 和 /l/ 的区别: particle /ˈpɑɹtək(ə)l/, marble /ˈmɑɹ.bəl/
- /æ/ — 嘴张大,不要读成 /e/: mismatch /ˈmɪs.mæt͡ʃ/, atom /ˈætəm/, collapse /kəˈlæps/
如何用这段视频练习
- 先完整听一遍视频,不要开口,记下不认识的单词。
- 先用 0.75 倍速逐句跟读,熟练之后再回到正常速度。
- 录下自己的声音并与原声对比,特别注意 comet, hydrogen, chondrite 这类单词。
什么是跟读法?
跟读法 (Shadowing) 是一种有科学依据的语言学习技巧,最初开发用于专业口译员的培训,并由多语言者Alexander Arguelles博士普及。这个方法简单而强大:您在听英语母语原声的同时立即大声重复——就像是一个延迟1-2秒紧跟说话者的影子。与被动听力或语法练习不同,跟读法强迫您的大脑和口腔肌肉同时处理并模仿真实的讲话模式。研究表明它能显着提高发音准确性,语调,节奏,连读,听力理解和口语流利度——使其成为雅思口语备考和真实英语交流最有效的方法之一。






























