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【托福听力资料】托福TPO7听力文本——Conversation 1

【托福听力资料】托福TPO7听力文本——Conversation 1
【托福听力资料】托福TPO7听力文本——Conversation 1

【托福听力资料】托福TPO7听力文本——Conversation 1

众所周知,托福TPO材料是备考托福听力最好的材料。相信众多备考托福的同学也一直在练习这套材料,那么在以下内容中我们就为大家带来托福TPO听力练习的文本,希望能为大家的备考带来帮助。

TPO 6 Lecture 4 Earth Science

Narrator:Listen to part of a lecture in an earth science class.

Professor:We’re really just now beginning to understand how quickly drastic climate change can take place. We can see past occurrences of climate change that took place over just a few hundred years.

Take uh… the Sahara Desert in Northern Africa. The Sahara was really

different 6,000 years ago. I mean, you wouldn’t call it a tropical paradise or anything, uh…or maybe you would if you think about how today in some parts of the Sahara it…it only rains about once a century. Um… but basically, you had greenery and you had water.

And what I find particularly interesting... amazing really, what really

indicates how undesert-like the Sahara was thousands of years ago, was something

painted on the rock, prehistoric art, hippopotamuses, as you know hippos need a

lot of water and hence? Hence what?

Student:They need to live near a large source of water year around.

Professor:That’s right.

Student:But how is that proof that the Sahara used to be a lot wetter? I

mean the people who painted those hippos, well, couldn’t they have seen them on

their travels?

Professor:Okay, in principle they could, Karl. But the rock paintings aren’t the only evidence. Beneath the Sahara are huge aquifers, basically a sea of fresh water, that’s perhaps a million years old filtered through rock layers. And…er…and then there is fossilized pollen, from low shrubs and grasses that once grew in the Sahara. In fact these plants still grow, er…but hundreds of miles away, in more vegetated areas. Anyway, it’s this fossilized pollen along with the aquifers and the rock paintings, these three things are all evidence that the Sahara was once much greener than it is today, that there were hippos and probably elephants and giraffes and so on.

Student:So what happened?

Professor:How did it happen? Well, Now, we’re so used to hearing about how human activities are affecting the climate, right? But that takes the focus away from the natural variations in the earth climate, like the Ice Age, right? The planet was practically covered in ice just a few thousand years ago. Now as far as the Sahara goes, there is some recent literature that points to the migration of the monsoon in that area

Students:Huh?????

Professor:What do I mean? Okay, a monsoon is a seasonal wind that can bring in a large amount of rainfall. Now if the monsoon migrates, well, that means that the rains move to another area, right?

So what caused the monsoon to migrate? Well, the answer is: the dynamics of

earth’s motions, the same thing that caused the Ice Age by the way. The earth’s

not always the same distance from the sun, and it’s not always tilting toward the sun at the same angle. There are slight variations in these two parameters.

They’re gradual variations but their effects can be pretty abrupt. And can cause the climate to change in just a few hundred years.

Student:That’s abrupt?

Professor:Well, yeah, considering that other climate shifts take thousands of years, this one is pretty abrupt. So these changes in the planet’s motions, they caused the climate to change.

But it was also compounded. What the Sahara experienced was uh…a sort of “runaway drying effect”. As I said the monsoon migrated itself, so there was less rain in the Sahara. The land started to get drier, which in turn caused a huge decrease in the amount of vegetation, because vegetation doesn’t grow as well in dry soil, right? And then, less vegetation means the soil can’t hold water as well, the soil loses its ability to retain water when it does rain. So then you have less moisture to help clouds form, nothing to evaporate for cloud formation. And then the cycle continues, less rain, drier soil, less vegetation, fewer clouds, less rain etc. etc..

Student:But, what about the people who made the rock paintings?

Professor:Good question. No one really knows. But there might be some

connections to ancient Egypt. At about the same time that the Sahara was

becoming a desert…hmm ...5,000 years ago, Egypt really began to flourish out in

the Nile River valley. And that’s not that far away. So it’s only logical to hypothesize that a lot of these people migrated to the Nile valley when they realized that this was more than a temporary drought. And some people take this

a step further. And that’s okay, that’s science and they hypothesize that this

migration actually provided an important impetus in the development of ancient Egypt. Well, we’ll stay tuned on that.

23《力的合成与分解》教学案含答案

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解析:选AD 合力与分力是等效替代关系,合力产生的效果与分力共同作用时的效果是相同的,因而合力与分力不是同时作用在物体上的,也不涉及力的性质的问题,故A 、D 正确,B 、C 错误。 [力的合成] 3.[多选]作用在同一点上的两个力,大小分别是5 N 和4 N ,则它们的合力大小可能是( ) A .0 B .5 N C .3 N D .10 N 解析:选BC 根据|F 1-F 2|≤F ≤F 1+F 2得,合力的大小范围为1 N ≤F ≤9 N ,B 、C 正确。 [力的分解] 4.[多选]将物体所受重力按力的效果进行分解,下列图中正确的是( ) 解析:选ABD A 项中物体重力分解为垂直于斜面使物体压紧斜面的分力G 1和沿斜面向下使物体向下滑的分力G 2;B 项中物体的重力分解为沿两条细绳使细绳张紧的分力G 1和G 2,A 、B 图均正确;C 项中物体的重力应分解为垂直于两接触面使物体压紧两接触面的分力G 1和G 2,故C 图错;D 中物体的重力分解为水平向左压紧墙的分力G 1和沿绳向下使绳张紧的分力G 2,故D 图正确。 核心考点·分类突破——析考点 讲透练足考点一 共点力的合成 1.共点力合成的常用方法(1)作图法:从力的作用点起,按同一标度作出两个分力F 1和F 2的图示,再以F 1和F 2的图示为邻边作平行 四边形,画出过作用点的对角线,量出对角线的长度,计算出合力的大小,量出对角线与某一力的夹角确定合力的方向(如图所示) 。(2)计算法:几种特殊情况的共点力的合成。类型作图合力的计算 ①互相垂直 F =F +F tan θ=F 1 F 2

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