【IBT 学习小组100+】听写小组 (作业贴)

可爱的小草UID: 2725141

交作业啦~~ 每天的作业会发布在2楼.



听写小组

听力乃iBT考试成功与否的关键，因为听力能力的运用不仅在听力考试一块，甚至在口语与写作部分也是得分的关键。要挑战iBT，就必然不可放松听力训练。
本小组的听力训练模式为 ETS提供的OG,老托,新托TPO听写。

每天布置的听写作业, 请组员按时完成. 在这里推荐大家使用cooledit2.1 进行听写. 小马过河有下载.

①把听写的文章与答案对照, 以红色字体标出听错的, 括号后以蓝色粗体字体标出正确的, 橙色粗体标出听漏的, 橄榄绿粗体标出多听的.

②根据saavedro推荐:听写是暴露缺陷问题的手段。 听写之后就要一遍跟读，一遍听读这样的交替进行，一共至少20遍，每篇文章均要如法炮制。跟读是看着文本，听着录音，你出声同步跟读。 听读是听着录音，眼睛不看文本，进行盲读。整体略慢于录音2-3个单词

③最后把文章的逻辑以1,2,3..列出来. 具体事项,会在群里公布.   

④把校对过的听写与文章逻辑一同上传于 听写小组帖子 中. PS:由于跟读的作业无法监督, 请组员们自觉,既然加入小组,就要有决心冲刺100+, 有个良好的心态与坚持是进军目标的基础!请大家不要偷懒.
在这里

为了刺激组员的积极性，保持大家的热情，本组的听抄形式是：只开一个听写小组帖，大家可以互相借鉴, 看到自己每天的进步.  X7 y0 t0 f) N
小组主要提供共同练习的气氛和监督力。当然也是希望交流经验.


【IBT 学习小组100+】作文小组 独立写作 (作业贴)https://bbs.gter.net/thread-1028833-1-1.html

【IBT 学习小组100+】作文小组 独立写作 (上交贴)https://bbs.gter.net/thread-1028835-1-1.html

【IBT 学习小组100+】口语小组 (评价贴)https://bbs.gter.net/thread-1028840-1-1.html

【IBT 学习小组100+】作文小组 综合写作 (上交贴)https://bbs.gter.net/thread-1028844-1-1.html

可爱的小草UID: 2725141

                                                         
大家把人体心理学做了

材料在群邮箱里, 要求: 听写(修改)---跟读---文章逻辑.   凌晨1点前交作业

文章逻辑for example: 第4篇(fossil fuels)

                                   1.主题 f.f----举例子说明
                                    2.解释 f.f----fossil
                                    3.解释 f.f----fuel
                                    4.f.f的总量 < 开采量
                                    ∴f.f ---nonrenewable
                                    5.Next: 下节课讲代替f.f                              

CandyWeiUID: 2724575

来顶了…………

lxb200709UID: 2665924

我也来顶。。

CandyWeiUID: 2724575

收到…………

可爱的小草UID: 2725141

地球interior

I’m glad you brought up the question of our investigations into the makeup of the earth’s interior. In fact, since this is the topic of your reading assignment for next time, let me spend the(these) last few minutes of class talking about it. There were several important discoveries in the early part of this century that help(helped) geologists develop a more accurate picture of the earth interior.

The first key discovery had to do with seismic waves. Remember they are the vibrations caused by earthquakes. Well, scientists found that they travel (traveled)thousands of miles through the earth’s interior. This finding enable(enabled) geologists to study the inner parts of the earth. You see, the(these) studies revealed that this vibrations were of two types. Compression or p waves, share or s waves. And researchers found that p waves travel through both liquids and solids, while s waves travel only through solid matter.

In 1906 a British geologist discovered that p waves slowed down at a certain depth. but kept travelling(traveling) deeper. On the other hand, s waves either disappear(disappeared) or were reflected back. So he concluded that the depth marked the boundary between a solid mantle and a liquid core. Three years later another boundary was discovered. That between the mantle and the earth’s crust.

There is still a lot to be learned about the earth. For instance, geologists know that the core is hot, evidence of this is the molten lava that flows out of volcano(volcanoes). But we are still not sure what the source of the heat is.

1.        主题:作业预习, discoveries to study the inner earth
2.        discovery 1----vibration: P&S waves
3.        discovery 2----boundary solid mantle & liquid core.
4.        (总结)仍需学习.

可爱的小草UID: 2725141

Climate

Today I want to talk about the earth’s last major climatic shift. At the end of the last ice age.

But first let me(us)
back up a moment, and review what we know about climatic change in general. First we defined climate as consistent patterns of weather over significant periods of time.


In general, changes in climate occur when the energy balance of the earth is disturbed. Solar energy enters the earth’s atmosphere as light, and is radiated by the earth’s surface as heat. Land, water and ice each affect this earth energy exchange differently. The system is so complex. That to date, our best computer models are only crude approximations and are not sophisticate enough to test hypothesis(hypotheses) about the causes of climatic change.

Of course, that didn’t stop (doesn’t keep)us from speculating, for instance, volcanic activity is one mechanism that might affect climatic change. When large volvano(volcanoes) erupt, they disperse tons of articles into the upper atmosphere. Where the particles then reflected(reflect) light. Since less light is entering the system of energy exchange. The result will(would)
be a cooling of the earth’s surface.

Of course, this is just one possible mechanism of global climatic change. In all probability, a complete explanation would evolve several different mechanisms operating at the same time.

1.      1.主题:climatic change
2.      2.什么是climate
3.      3.什么是change (in climate)
4.      4.可能引起的猜测
5.      5.总结: 很多可能性机制

eric1207_weiUID: 2489121

By 05/12
earth interior

I am glad you brought up the question about our investigtion(s) into the makeup of the earth's interior. In fact, since this is the topic of your reading assignment for next time, let me spend these last few minutes of class talking about it.There were several important discoveries in the inner(early) part this century that help the geologists develop more actual (accurate)pictures of the earth's interior.

The first key discovery had to do with seismic waves, remeber they are the vibrations caused by earthquakes. Well, scientists found that they travel thousands of miles through the earth's interior, this finding enabled the geologist to study the interior(inner) part of the earth. Your see, this study revealed that these vibrations were two types, compression or p-waves, and shear or s-waves. and researchers found that p-waves travel through both liquids and solids, while s-waves travel only through solid matter.

In 1906, a bristish(british) geologist discovered that p-waves slowed down at a certain depth, but can(keeping) travelling deeper. On the other hand, s-waves either disappeared or were reflected back. So he concluded that the depth marked the boundery between a solid mattle and a liquid core. Three years later, another boundery was discovered, that between the mattle and the earth's crust.

There'res still a lot to be leart about the earth. For instance,  geologists know the core is hot, evidence of this is the motto(motlen) of lava flows out of volcanos, but we're still not sure what the sources of the heat it is.

文章逻辑：
1.topic: interior part of earth
2.explaination: key discorveries--two examples(p-waves & s-waves)
3.future work: some more need to be studied

eric1207_weiUID: 2489121

By 05/12
Climate
today I want to talk about the earth last major climate(climatic) shift at the end of last Ice Age.

But first, let's back up a monment and review our what we know about climate(climatic) change in general. First, we definite climate as consistent patterns of weather over significant periods of time.

In general, changes in climate occur when the energy abounds(balance of) the earth is distubered. Solar energy enters the earth's atmosphere as light and is radiated by the earth's  surface as heat. Land, water and ice, each effects the energy change differently. this system is so compelx that to date our best computer models are only could (crude approximations and are not sophisticated enough to) test hyerpec (hypothese)about the causes of climate(climatic)  change.

of course, that does not keep us from speculation(speculating). For instance, volcanic activity is one mechansim butthat might effect climate change, when large volcano erupte, they disburse(disperse) tons of particles into the atmosphere, while particles then reflect light, since less light enters the system of energy exchange, the result will be cooling of the earth's surface.

of course, this is just one possible mechansim  of gobal(global) climate change. in our probility(all probability), a complete explanation will involve several different mechansim operating at the same time.
mechansim是本文基本没有听出来的,还有那很长的一句话 听力的路还很长~~~
文章逻辑：
1.topic: climate change
2.expansion: difinition--complexity--speculation--example
3.future work

eric1207_weiUID: 2489121

By 05/12
minerals
I'd like to begin by thanking Dr Kane for inviting me to be here today, although I am not a geologist, I have been collected(ing) minerals for years, my collection is very diverse because I travelled all over the world to find them. Today, I bought a few best of them (specimens) for you to see, after I discuss each one I will pass it around, so you can look at it more closely.

As you know, feldspars are most abundant merinals and it are devided into a number of types, the first samples are orthoclases, notice they are very(vary) in color to from white to pink to red. This glassy one is found in volconic rock, in fact, I found it in New Mexico on a collection(ng) trip.

This next sample I will pass around is micro(cline) mineral, also called amazonstone, you can identify it by the bright green color, it often used in jewelry and is really quite attractive, the final samples are plagioclas feldspars, many plagioclas were very rare, so I am particularly proud of the varity(variety) in my collection.

I've also brought a few slight(slides of) larger minerals samples, and if you'll turn on lights now, I'd like to show them to you.

文章逻辑：
1.topic: introduction about the some minerals
2.expansion: some sample minerals
3.next: some larger minerals samples will be showed

第一天的作业做完了，还有好多细节地方不是很清晰，路漫漫兮～～～

CandyWeiUID: 2724575

11月15日 CandyWei听写作业
地球（Interior）


I am glad you brought up question of our investigation make up (into the makeup of) the earth’s interior. In fact, since this is the topics of your reading assignment for the next time, let us (me) spend the (these) last few minutes of class to talk (talking) about it. There are (were) several important discoveries in the early part of earlier (this) century that help geologists develop (developed) a more accurate picture of the earth’s interior.
The first key discovery has (had) to do with size (seismic) waves. Remember they are the vibrations cased by earthquakes. Well, scientists found that they traveled thousands of miles through the earth’s interior. This finding enabled scientists (geologists) to study the inner parts of the earth. You see, this (these) studies review (reveal) that these vibration were of two types. Compression or P and shear or X wave, and the scientists (researchers) found that the P wave travel through both liquids and solids, while the X wave travel only through solid matter.
In 1906, a British scientist discovered that P waves slowed down at a certain depth but kept traveling deeper. On the other hand, X waves either disappear or were reflected back. So he concluded that the depth marked the boundary between a solid matter (mantle) and a liquid core. 3 years later, another boundary was discovered that between the mantle and the earth’s crust.
There’s still a lot to be learned about the earth. For instance, the geologists notice (know) that the core is hot. Evidence of this is molten lava that flows out from (of) the volcanoes, but we’re still not sure what the source it heated.(of the heat is)



1、主题，reading assignment for next time:study about the earth's interior
2、discovery：P and X
3、discoveries of P and X help determine boundary in the earth's interior
4、 still not sure something

CandyWeiUID: 2724575

11月15日 CandyWei 听写作业
关于climatic change



Today, I want to talk about the earth’s last major climatic shift, at the end of the last ice age. But first, let us back up a moment and review what we know about climatic changing in general. First, we define climate as constant (consistent) patterns of weather over significant periods of time. In general, changing (changes) in climate occur when the energy balance of the earth is disturbed. Solar energy enters into the earth’s atmosphere as light and is radiated by the earth’s surface as heat. Land, water and ice each effect (affect) this energy change (exchange) differently. The system is so complex that, to date, our best computer are only crude approximation and are not sophisticated enough to test the hypothesis that (about) the causes of climatic change. Of course, that doesn’t keep us from speculating. Volcano activity is one mechanism that might effect climatic change. When large volcanoes erupt, they spurs (disperse) tons of articles into the upper atmosphere, where the articles then reflect light. Since less light enter (is entering) the system of energy change (exchange), the results of (would be a) cooling of the earth’s surface. Of course, this is just one possible mechanism of global climatic change. In all probability, a complete explanation would involve several different mechanisms operating at the same time.

1、主题：about the climatic change
2、define “climate”
3、some hypotheses, for instance, volcano activity
4、还有其他可能影响气候的因素

lxb200709UID: 2665924

觉悟
地球interior

I’m glad you brought up the question of our investigations into the makeup of the earth’s interior. In fact, since this is the topic of your reading assignment for next time, let me spend the next(these last) few minutes of class talking about it. There were several important discoveries in the early part of this century that help(helped) geologists develop a more accurate picture of the earth interior.' l# j" }3 O" {: b; ` f
The first key discovery had to do with seismic waves. Remember they are the vibrations caused by earthquakes. Well, scientists found that they traveled thousands of miles through the earth’s interior. This finding enable(enabled) geologists to study the inner parts of the earth. You see, the(these) studies review(revealed) that this vibrations were of two types. Conpration(Compression) or p waves and shear or s waves. And researchers found that p waves travel through both liquids and solids, while s waves travel only through solid matter.
In 1906 a British geologist discovered that p waves slowed down at a certain death(depth). but kept travelling(traveling) deeper. On the other hand, s waves either disappear(disappeared) or were reflected back. So he concluded that death(depth) marked the boundary between a solid mantle and a liquid core. Three years later another boundary was discovered. That between the mantle and the earth’s
crust.. [4 N+ U( q. M0 p# a  A- X! l- ^" U
There is still a lot to be learned about the earth. For instance, geologists know that the core is hot, evidence of this is
the molten lava that flows off(out of) volcano(volcanoes). But we are still not sure what the source of the heat is

Topic: investigations into the makeup of the earth’s interior
Explanation: P,S waves help discovery the depth of the boundary between M&C.
Next: still a lot to learn

lxb200709UID: 2665924

觉悟
Climate  

Today I want to talk about the earth’s last major climatic shift. At the end of the last ice age. :But first let us back up a moment, and review what we know about climatic change in general. First we defined climate as consistent patterns of weather over significant periods of time.* In general, changes in climate occur when the energy balance of the earth is disturbed. Solar energy enters the earth’s atmosphere at night(as light), and as(is) radiated by the earth’s surface as heat. Land, water and ice each affect this earth energy exchange differently. The system is so complex. That today(to date), our best computer models are only crude approximations and are not sophisticate enough to test hypothesis about the causes of climatic change. Of course, that doesn’t keep us from speculating, for instance, volcanic activity is one mechanism that might affect climatic change. When large volcano(volcanoes) erupt, they disperse tons of particles into the upper atmosphere. Where the particles then reflect light. Since less light is entering the system of energy exchange. The result would$be a cooling of the earth’s surface. " [9 X6 B" G- n( `w  y
Of course, this is just one possible mechanism of global climatic change. In all probability, a complete explanation would involve several different mechanisms operating at the same time.

Topic: climate change
Explanation: 1.solar energy

2.vocanic activity
Next: complete explanation involve different mechanism

lanyouno2UID: 2649409

来自The one：
第一篇（地球interior）
I am glad you broke (brought) up the question about our investigtion(s) into the make up(makeup) of the earth('s) interior. In fact, since this is the topic of your reading assignment for next time, let me spend these last few minutes of class talking about it.There were several important discoveries in the early part this century that help the geologists develop more*( accurate) pictures of the earth('s) interior.

The first key discovery had to do with *(seismic) waves, remember they are the vibrations keys(caused )by earthquakes. Well, scientists found that they travel thousands of miles through the earth's interior, this finding enabled the geologist to study the inner part of the earth. Your see, this study revealed that these vibrations were two types, (compression) or p-waves, and (shear) or s-waves. and researchers found that p-waves travel through both liquids and solids, while s-waves travel only through solid matter.

In 1906, a british geologist discovered that p-waves slowed down at a certain depth, but kept travelling deeper. On the other hand, s-waves either disappeared or were reflected back. So he concluded that the depth marked the downdery(boundery) between a solid mattle and a liquid core. Three years later, another boundery was discovered, that between the mattle and the earth's crust.
There're still a lot to be leared about the earth. For instance,  geologists know the core is hot, evidence of this is the motlen of lawa(lava) flows out of volcanos, but we're still not sure what the sources of the heat it is.