跟讀練習: Why is it Hot Underground? - 通過影片學習英語口語
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44 句
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Way back in the Middle Ages,
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miners began to notice that the deeper they dug into the Earth,
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the toastier it got.
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Who knows what they made of the heat,
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but the physicist Lord Kelvin,
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of temperature fame, naturally, had a theory.
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Earth started off hot, and has been cooling down ever since,
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like a baked potato pulled from the oven.
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What's more, Kelvin was confident this idea would allow him to calculate the age of our potato—I mean, planet.
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Imagine pulling two recently baked potatoes out of a freezer,
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one that's been in there for just a minute,
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the other for half an hour.
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The minute-old one would still feel like a hot potato,
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while the half-hour frozen spud would have cooled well below the skin.
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You'd have to poke all the way to the center to feel its residual warmth. And
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so in principle,
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you can tell how long ago a potato was cooked just by feeling how warm it is right beneath its surface.
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Which is exactly what Kelvin did,
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except with the Earth and scientific rigor.
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He took temperature measurements from the mines,
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put them into his calculations,
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and he got 20 million years.
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Which is, of course, very, very wrong.
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Somehow, the hot temperatures just under Earth's skin made it seem to Kelvin
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that our planet was pretty much fresh out of its cosmic oven,
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when we now know that it's 4,500 million years old.
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Calvin's error is usually attributed to the fact that he didn't know about radioactivity,
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which creates a ton of heat in Earth's core and helps keep the planet warm.
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But heat from radioactive decay moves so slowly through solid rock that taking radioactivity into account only improves Calvin's estimate by,
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well, pretty much nothing.
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Calvin's real oversight was in thinking of the Earth like a baked potato,
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a solid lump through which heat slowly diffuses.
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Earth's mantle, the thick layer between the crust and the core,
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is mostly solid, but it isn't rigid.
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In fact, the rock closest to the molten outer regions of the core gets so hot that it becomes slightly more pliable,
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like warmed candle wax.
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And like the hot air above a candle,
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the warm rock rises in convection currents over millions of years,
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spreading heat more evenly throughout the planet.
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This stirring carries tremendous amounts of heat from the core to the crust,
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fueling volcanoes, maybe helping to drive plate tectonics,
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and heating mine shafts to temperatures that make Earth seem like it's fresh out of the cosmic oven.
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Even though it's not.
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loud too.
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背景與概述
在中世紀時期,礦工們逐漸注意到,他們挖掘得越深,地面的溫度就越高。雖然當時的人們對這種熱量有不同的理解,但物理學家開爾文勳爵提出了一個理論:地球最初是熱的,但隨著時間的推移逐漸冷卻,就像剛從烤箱裡取出的土豆。而開爾文對這個理論的渴望,不僅希望說明地球的年紀,也試圖通過測量地下溫度來實現。這段探討地球內部熱量來源的旅程,不僅是一段科學的歷程,同時也是理解英語表達能力的契機。
日常交流的五個短語
- “溫度越來越高” - 通過觀察環境變化來加強描述能力。
- “堅固但不靈活” - 理解並表達物體的特性。
- “熱氣流上升” - 學習描述科學現象,與日常生活關聯。
- “時間的推移” - 使用表達涉及時間的詞彙加深描述的深度。
- “地下深處的熱量” - 增強對特定主題的表達能力,幫助進行更深入的交流。
逐步影子跟讀指南
對於希望提高英語口語與聽力的學習者,影子跟讀是一種有效的方法。您可以採取以下步驟來充分利用影片內容:
- 選擇合適的影片:找一個相關的科學或文化主題的英語影片,例如關於地球熱源的分析。
- 初步聽力理解:觀看影片時,儘量理解大意,不必過於關注每個單詞的意思。
- 播放與暫停:使用影子跟讀練習的過程中,慢慢播放影片。每聽到一個句子,就暫停並嘗試模仿。
- 重複練習:不斷重複這一過程,直到能夠自如地跟上說話者的節奏,同時注意語音語調。
- 錄音對比:自己錄製跟讀的聲音,並與原影片進行比較,找出需要改進的地方,特別是在發音和語調上。
通過這種方式,不但能增加對科學知識的理解,還能提升自己的英語口語能力,運用這個英語影子跟讀的技巧,您將體驗到更有效的英語口語練習,從而更深入地理解和掌握英語!同時,建議使用看YouTube學英語的方式,開啟您的英語學習之旅!
什麼是跟讀法?
跟讀法 (Shadowing) 是一種有科學依據的語言學習技巧,最初開發用於專業口譯員的培訓,並由多語言者Alexander Arguelles博士普及。這個方法簡單而強大:您在聽英語母語原聲的同時立即大聲重複——就像是一個延遲1-2秒緊跟說話者的影子。與被動聽力或語法練習不同,跟讀法強迫您的大腦和口腔肌肉同時處理並模模擬實的講話模式。研究表明它能顯著提高發音準確性,語調,節奏,連讀,聽力理解和口語流利度——使其成為雅思口語備考和真實英語交流最有效的方法之一。
































