托福聽寫訓練營

基本介紹

• 中文名：托福聽寫訓練營
• 外文名：TOEFL Dictation Training Camp
• 教材：ETS官方真題
• 獨家解決方案：聽寫創始人馬駿聽寫理論

課程重點

聽不懂？——教你聽懂文章！

不知道聽什麼點？——教你聽到出題點！

聽懂了不會做題？——做題技巧！

專業辭彙和話題不了解？——考前機經點撥！

教材

ETS官方真題

教學目標

（1）辭彙量缺乏，導致學生聽不進去

（2）聽力文章內容生僻晦澀，無人督導無法進行聽力學習

（3）傳統聽力訓練方法抽象枯燥，學生不願執行

（4）只聽聽力，缺少大量朗讀，無法達到聽力學習效果

（5）聽力材料不夠精準系統，聽力學習付出與回報不成比例

獨家解決方案

第一步：聽寫創始人馬駿聽寫理論

（1）聽寫就是聽一句寫一句，對照文字找到自己沒有識別出來的聲音；同時在這個過程里訓練自己的聽覺存儲力。聽寫只是一個工具而已。每天都要使用這個工具來檢查我們的耳朵到底有哪些漏洞，無論是對於單詞只是熟悉形狀不熟悉發音，還是我們不認識的單詞，只要是我們耳朵陌生的聲音，都可以使用這個工具檢查出來。因為我們那多年學習英文靠眼睛，疏忽了耳朵作為一個識別工具去識別單詞，這樣一來，想理解句子是根本不可能的。所以，要從最簡單的入手，首先讓你的耳朵聽出來的東西更多，才能提高理解的程度。記住，聽寫只是一個工具，不能敷衍了事，你在使用工具的過程中，到得到一些東西；千萬別把聽寫當成一個任務，大家都聽寫，為什麼有的人進步快，有的人進步慢？根本上就是你是否在使用聽寫這個工具的時候查漏了！聽寫之後一定要做跟讀。如果說聽寫是查漏的過程，看到自己的耳朵漏洞百出，你到底該為這些漏洞做點什麼？如果不為漏洞做點什麼的話，你早晚要為你的漏洞付出代價！所以：沒有讀過的聽寫不是完整的聽寫。我們說：先聽寫再跟讀，語音語調耳朵熟。
（2）聽一句寫一句有利於提高大腦的存儲力。識別出來聲音了，要把識別出來的聲音聯繫起來串成句子理解。存儲時間短暫會讓你來不及串起句子；存儲空間有限讓你根本耳朵識別出的聲音不夠組成句子！
聽寫是耕一片冬僵了土地，邊耕邊抓到種子在手裡，趁著土地翻開播種到裡面；跟讀是灌溉你的種子。發芽的時候就是你的耳朵對所以認識的單詞的聲音熟悉的時候。

對於你跟不上的文章，你需要經歷幾個步驟：

（1）先不跟，先把整篇文章大聲朗讀熟練。讀的過程中，找出自己不會的或不熟悉的單詞，標註好音標，朗讀多少遍能熟悉要看：你自己的基本實力；你對自己的和對目標的要求。

（2）開始開著原文跟著讀。在你已經讀熟練的基礎上，你是絕對可以跟得上的，如果暫時不能，只能說明你還是沒有讀熟練，這樣才會導致沒有注意力去跟著標準的聲音而完全把注意力放在你眼前的單詞該怎么發音上，以至於：跟不上。讀幾遍算過關呢？無論你的基本實力處於什麼位置，最後只要能做到當以後耳邊再次響起缺陷聲音的時候能迅速反映，就算過關。具體你自己幾遍可以達到，這不是一個數字能概括得了的。就好象你背單詞，你背幾遍能背下來？誰知道呢……（

（3）拋開原文，只跟著聲音走，這是最高境界。

跟讀就好象學習滑冰。剛開始的時候站不穩，需要手扶著凳子，勉強前行，久之，撒開凳子，自由滑行。跟不上的時候需要藉助的凳子是指文字答案，邊看著文字答案邊讀，熟練後，慢慢把注意力放在耳朵識別上，最後拋離開眼睛識別。

第二步：獨家聽寫進階教材

托福聽力馬駿名老師九年教學經驗凝聚而成的托福經典教材。

第三步：名師跟進聽寫21 步訓練

第四步：智慧型聽力學習軟體配合學生朗讀

訓練營作業

2011年4月20日作業

聽寫托福聽力文章月球SPA part2-part4

You know planetary researchers love studying deep craters to 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?

Dian

So, the only way to know the basin’s age is to study its rocks directly?

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.

Dian

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

Professor

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 data 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.

Student

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

Professor

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.

Dian

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

Professor

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.

Student

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?

Professor

Permanent base, maybe a way’s 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.