还是第一天把听写的内容发上来,额,听得~那个丢人呀~呀~
" I5 m  l" i3 T+ C5 [这就是偶的听写结果, - u: @* w$ w& C. f% t3 \: {8 o# M
, S: a- x) {- O0 |! |
第一篇：打工场景
% [$ ?( K, s- E' l, H9 d0 r0 {It seems only yesterday that I was sitting where you are. Just finishing my first year of medical school, I was wondering if I canI’d ever get a chance to use all my new knowledge on a real life live patient. Well, I have good news for you. You don’t have to wait until you third or forth year of medical school to get some hands-on experiences. The dean has admiredinvited me here to tell you the university’s rural opportunity program. If you enroll in this program, you can have the opportunity this summer. After your first year of medical school, justto spend four to six weeks observing and assisting a real physician, like me in a small rural community. You will not compete with other students for time and attention, and you can see what life of theas a country doctor is really like. 3 F) y3 {5 C: K$ q: Y! {
2 U$ a3 z' c' `  A: Z
The program was designed to encourage medical students like yourselves to consider careers in rural communities that are still under staffedunderstaffed. It seems that medical students are freeafraid to go tointo rural families practice for two reasons. First they don’t know about it and second the specialty in cities usually make money. But on the oppositeup-side, in rural practice doctor can really get to know their patients and waver the spectbe repected numbermembers in community.
+ z! s/ U/ I  X3 T! }I participated the program when it first started and spent six weeks in a small rural town. Let me tell you, it was really great. I got to work with the real patients, I watched the birth of child, a sistentassisted of an accident victim and had a lot of really practical hands on experience all in one summer.3 E5 L7 k: F- _- @' Y/ D- ^  I
To my surprise, I found the country life has a lot of ffers than city lifeto offer that the city doesn’t, no pollution, no traffic jam for instance. My experience made me want to work where I was needed and appreciated. I don’t miss the city at all.
  ?' ?# o7 F* f, L) K3 y
$ s# c, \4 V; ^" A2 @3 O2 Q第二篇：选课场景0 H! j' N, B, p& I' x
In the few minutes that remain inof today’s class, I’d like discuss next week schedule with you. Because I’ll presena I’m presenting a paper at a conference in D on Thursday, I won’t be here for either Wednesday’s or Friday’s class, I will havehowever ever beenbe on Mondays. Next Friday, a week from today, is the midterm exam, marking the halfway point ofin this semester. Professor Andrew has agreed to administrate the exam. In place of the usual Wednesday’s class, I will arrange an optional review session. Since it is optional, attendance will not be taken. However, attending the class would be a good idea for those worried about the exam. So remember, optional class next Wednesday, midterm Friday.
- A% C) |" n" e4 e7 G , d) l  i- T+ S) b; ?4 P
第三篇：打工场景
* @4 o' x' K$ m) R' TGood afternoon, I’m here today to talk to you about a career with our airline. We are speciallyespecially interested in people includingrecruiting to feelfill openings for flight attendance. & H' {3 Z4 r% J

: r- ~3 `# @4 b+ d" PFirst of all, to work as thea flight attendance with us you must be accepted into our training program, and with so many people applying, it is not easy to be selected. From thousand of applications that we receive annually, we choose fewer than thea thousand people for training. So we require experience serving the republic, and it also helps if you’ve earned some college credits. Also, not everybody who gets accepted into the training makes through. The course meets six weekdaysdays a week for five weeks. The training includes extensive courseclassroom work in such subjects as first aid, passenger psychology as well as practice training in persingersfligh procedures and musterrismeal service. A lot of very graduates savesay our fight attendance attendants to develop the skills of nurse, a head waiter and a public relationship executive. But as a flight attendance to myself I can say that all of the hard work is worthyworth it. Of course I get to travel throughout the country and the air line pays all of my expenses while I’m wayaway forfrom my base station. And what I like best of all is that I’ve made friends with people from all over the country.
/ T7 D2 {% @$ |$ ]( ~
& ^/ m7 M1 i; g第四篇：Housing场景
/ e# E* r* |) A, q1 M3 s" LI need to make sure you understand how to get house in for next year. When you entered as first students this year, the school listassigned you to a dorm and roommate. But next year as returning students you choose both your roommate and your dorm. But whether or not you actually get to leavelive in your first choice depends on what number you or your roommate draws in the lottery system. The system gives priority to the students who have been here living in longest. Forth year students get the first block numbers, third year get the second block, second year like you will be get the third. The lower the number you draw, the sooner you choose. NO.1 gets the first choice, NO.2 gets the second choice and so on. % `2 [, n' N9 J7 {
/ ?+ d) c+ D. P" t& s) B
You can use either your own or your intended roommate’s number to make your choice. If your roommate for next year has been in school longer than you have, they will be in better blot/ |0 C( R) S2 T1 }) D+ A2 ^
numbers and so have better numbers that any second year students. But most of you will probably be roommaterooming with other second year students and so neither of you will have a great number. You may not get into your first or even second choice, of course if you make plans to live off campus you don’t need to enter the lottery at all. Dorm space is especially tight this year because the dorm on north campus would be closed for ralidationsrenovations. This means the dorm you would draw worst numbers will be able to get the dorm at all. In that case, the housing office will help you find off campus housing.$ R- }4 @1 x4 o2 U* D: {! o0 k
$ E/ `% [1 L) N
好饿呀~吃,还想吃,呵呵

LZ加油啊

坚持是真理！

加油啊，fighting

昨天和我们那里的同学一起看开幕式,两点才回来,结果一觉睡到今天早上九点,被老板鄙视~
& q: `0 |+ p) h3 X  n晚上回来也只听了这么多~3 `/ E& g: V+ K3 s' q+ G# s
先反省一下,认真检讨 5 H, ^  Q4 e9 |
0 F) T: V7 z" Y' `# Z
I’m glad you brought up the question over are theof our investigations into the make upmakeup of the earth’s interior. In fact, since this is the top of your reading assignment for next time, let me spending thethese last few minutes of the class talking about it. There were several important discoveries in early part of this century that helphelped geologists develop a more accurate picture of the earth’s interior.
9 ?6 {* K" q7 t# O5 K% c' D& ~The first key discovery had to do with the signs degreesseismic wavs remember they are the vibration caused by earthquakes. Well, scientists found they travel thousands of miles through the earth interior. This finding enabled geologists to study the inner parts of the earth. You see, the studies revealed that these vibrations were of two types, compression or p-waves, and sheershear or s-waves. And the researchresearchers found that p-waves travel through both liquids and solids while s-waves travel only through solid matter. 1 B4 |8 O+ [& y( \
; {) k: a3 F$ }" Z8 Q$ c3 L: e
In 1906 a British geologist discovered that P-waves slowed down at a certain depdepth but kept traveling deeper. On the other hand, the s-wave either disappeared or were reflect back, andso he concluded that the depdepth marked the boundary between thea solid mental and thea liquid core. Three years later, another boundary was discovered that between the mental and the earth crust. & k7 G! u( x: J7 a% z" D, J! G

! w5 q7 b; k* |There are still a lot we need toto be learnlearned about the earth. For instance, geologists know that the core is hot, evidence of this is that motentmolten lava that float as flows out of
  }0 ?# E, d8 A, _volcanoes, but we are still not sure what the source itof the heat is& w, ~+ n6 ^9 o$ G- u' o; s+ Q
新词9 ^% O( F" a$ U: t( h
seismic 地震的' s) }  R2 ~9 q/ r( N2 F; D( a; T
shear v.剪切( w( ?, U* {) H6 A  V3 ^
8 c0 n) g% c5 g' }2 `. ]" Q0 O: y- F
NO.2 climate
% }/ y) i$ w: O+ t* d* Y( _Today I want to talk the earth’s last major climatic shift at the end of the last ice age. But first, let’s back up a moment and review what we know about the climatic changingchange in general. First we definedefined the climate as the consistent patterns of weather over significant periodperiods of time. In generallygeneral, the changing ofchanges in climate occurred when the energy balance of the earth is stirreddisturbed. Solar energy andenters the earth’s atmosphere is light and it is radiated by the earth’s surface at theas heat. Land, water and ice, each affect this energy exchanged differently.

一大早起来只听了这么多,晚上回来接着来~ ) ]; d5 z/ \- x9 G& W
The system is so complex that to data our best computer models are only (proved of)crude (apptoximations)approximation. (Anodoxiate)and are not （连读) sophisticated enough to test (hypothesis)hypotheses(e发长音，i发短音) about the causes of the climatic change. Of course that doesn’t keep us from (speculated)speculating, for instance, (volcanical)vocanic activity is one mechanism that might affect the climatic change. When large volcanoes erupt, they （just burst)disperse (tangs)tons of particles and (then)into the upper atmosphere where the particles then reflect the 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, the complete explanation would involve several different mechanisms (oppositing)operating at the same time.
& _  n7 ^2 @3 {& [  d' p* Q% a + I; |! N6 \3 t3 Z. x/ q- @* Z0 ?
不熟悉的词+ ]6 a: K7 i) \, F" L5 V" D
crude * e! L5 X! ~$ V- L- v& ~& N
a.粗鲁的，简陋的，天然的，未加工的( ^0 d  ]5 ~& K% P9 s
approximation
4 i! m8 j% _0 M; d6 Bn.近似值
& E) Z6 J9 b2 o4 p: w* Q5 Z5 r+ n6 |volcanic
  g) j# a7 x' G. \' Y' I& Xa.火山的
& n# ?: P' N/ S2 E9 K4 l% ctons of 成吨的9 [  n- Z5 A2 b6 |1 y) U
( M, m9 {' ~  B* Q+ h; w  v. c9 ]" q0 g
NO.3 Mineral
/ _2 B% G) G$ ]2 K; gI’d like begin by thanking Dr. Cane for inviting me to be here today. Although I’m not geologist, I have been collecting minerals for years. My collection is really (diversed)diverse because I’ve traveled all (of)over the world to find them. Today I’ve brought a few speciment)specimens for you to see. After I discuss each one I’ll pass it around so you could look at it more closely. As you know, feldspars are the most abundant minerals and are divided into (numbers)a number of types. These first samples are orthoclase, notice that they vary in color from white to pink to red. This glassy one is found in volcanic rock. In fact I found it in New Mexico on a colleting trip. This next ample that I’ll pass around is microcline mineral, also called amazonstone. You could identify by (the white)its bright green color. It is often used in (jewlry)jewelry and is really quite attractive. These final samples are all plagioclase. Many plagioclase are very (where)rare, so I’m particularly proud of the variety (of)in my collection. I’ve also brought a few s(lices)slides of some larger mineral samples, and if you turn out the (slice)lights now I’d like to show them to you.
, s1 r: T/ d3 T* |
# M0 P5 _3 A8 USpecimen
3 ]* p" I" b5 f, u. p$ K1 h9 Tn.样本，标本
8 o) @: e4 c8 I) z- |8 j2 c, a3 x0 uFeldspar
! B: [2 ]! p0 G6 X: Y5 Cn.长石
  M% a6 M2 ]0 g/ I4 r  a2 GOrthoclase6 ?% Q( M: x% w, h
n.正长石) V' M5 h4 j& B, m* U! I1 c, j2 I
Microcline
+ I3 y8 j) R$ Y/ P! G; J7 N' ?5 b* F4 ?n. 微斜长石- k7 |5 w- _/ s6 d

, @; w. [' C7 ?& m: Q: N7 J! ]2 iNO.4 fossil fuels
7 [8 L7 w( Y. n( A- g# q( ?4 W6 ZToday I want to discuss fossil fuels such as coal, oil and natural gas. The term of fossil fuel refers to the (trapering names in)trapped remains of plants and animals in sedimentary rock. You see, living plants trap energy from the sun by the process of photosynthesis and they store the energy in their chemical (conpound)compounds. Most of that energy is released when the plant dies and decays. However, sometimes the organic matter is buried before it decay completely. In this way some of the (sole)solar energy becomes trapped in rocks hence the name fossil fuel. Although the amount of the organic matter trapped in any one growing season (and)is small, the accumulated remains for millions of years are considerable. Because the accumulation rate is so low, millions of time slower than the rate at which we know the dig up this organic matter and (permit)burn it for energy, we must consider fossil fuels as non-(renewed)renewable resources. Tomorrow we’ll be discussing alternatives to fossil fuels that can be renewed.
0 i' j6 w+ |7 @/ A% B( j) u6 qCompound n.混合物，复合字
. E! F% H% R: L! h% D' Ca.复合的，混合的，合成的; r0 B: D, _' I- W
v.混合，调合，妥协* D! }) a) Z7 x( K
( n( b, G- i6 u, F+ T4 O
NO.5 Mountain
& o6 b, N, E1 f' P, U6 X8 f: FNot long ago some of you may have read about (the)a team of the mountain climbing scientists who have helped recalculating)recalculate the elevation of the highest of the world, mountain Everest. Of course the elevation of the mountain E was determined many years ago, using traditional (survey)surveying methods. But these scientists (want)wanted to make a more precise measurement using the new method (the pix)that takes advantage of recent advances intechnology, It is call the global positioning system. - b& Q  B- P, r' G* f2 T6 H0 ~
( N' u* v6 I% z
The global positioning system uses 24 satellites (in)that circle the earth. Each of the satellite constantly (sanlling)sending out signals, and each signal contains important information that can be used to determine the (longtitude)longitude, latitude and elevation of any point on the earth’s surface. , f9 ?' _& Z0 {

, q2 V& f+ @- Q5 J( K# jIn order to use the system to calculate the mountain E’s elevation, scientists (need)needed to put a special receiver on the summit to receive the signals from the satellites. The problem (of)with this was that (the impast)in the past, the receiver were much too heavy for climbers to carry, but now the receivers have been reduced to about size and weight of a hand held telephone. So the climbers were able to take the receiver to the top of E and from there to access the satellite system signals that would allow them to determine the precise elevation, and it turns out the famous peak is actually a few feet higher than (mis)was previously thought2 e. ?( q: n; Y
一大早起来只听了这么多,晚上回来接着来~

哇，从8.8开始听的呢，有纪念意义，这个贴，，

呵呵,也不知道怎么就赶上这么好日子,就当选了个黄道吉日吧~

搂主加油~别忘记跟读练脑子和嘴皮子

我的笔记本变压器坏啦！好不容易用一套福娃徽章借了一个台式机先用几天，无语了~4 q1 T4 i  h3 U/ U% N& ?2 s$ j
整整一晚上听了就这么一小点，好难好难呀，还是我脑残了，崩溃ing~
2 C( v  s, X9 i/ T' N" E0 L* B+ o* W9 B3 f- s& S
Now you (are) have been reading articles about the tremendous damage (down) done to life and property by earthquakes. That’s why (sicemologist)seismologists (to be)have been working so hard to develop (massive)methods of earthquake prediction. We can now predict earthquakes fairly well but the predictions only (allocate)locate potential areas of danger. They don’t predict the (pacific’s)specific time and location at which an earthquake (likes) is likely to occur. Today I want to introduce to you three prediction models that (win) have been developed. # j; C: M6 ~' I" C5 t# S

+ J* V2 K. P8 d  }( hThe first prediction model looks (on) along earthquake (forth) fawlts (both) those cracks (and) in the earth’s crust to find what are known as (sesimic)seismic gaps. Seismic gaps are places where the (forthy)fawlt (short) show little (known) or no seismi activity for a long time. This theory postulates that such places 9by do) are due a for major shock.
; ]  H% Z% Q2 O( t, ?* i : z  O% S& M# H
The second model relies on (reamna) phenomena like ground (tude) tilt. Using long (seligns) cylindrical tool containing water.，observers (notice) noted that the ground (tune) tilt tended to occur before major earthquakes. That (lethom) led them to correctly predicted the big HC quake of 1975, the first successful earthquake prediction scientists have ever made. A million people were evaculated from that Chinese city before the earthquake struck. Unfortunately , this method has not worked consistently so we cannot say it has been (proeffected)perfected.
$ h4 A9 x* s! c# r0 y+ i. l ! t* W% _* d2 d2 D- f* M/ F% _
The third model is based on the theory that
4 \0 ^; s6 U/ g' Smajor earthquakes closely follow (the theory) a serises of (mire) minor ones. Starting with the measurements and timing of the smaller earthquakes, a complex formula calculates the time of (inquisy) increased probability of a much larger quake. Right now this method like first method can not predict pacific time and places, but that may change (the ased of the) as it is further development.
, F' J. K5 h; ]" U# l+ U- v 8 W: D' `( m) `, v$ a
For the moment none of these models can predict with reasonable levels of confidence6 T4 \  V3 b0 L  _! R' @! _

! z7 V8 R# D: f7 P# Y& B. ofawlt 什么意思啊？我查了牛津高阶都没找到！/ S( E7 {- {$ t1 K
tilt v.（是某物）倾斜；n.倾斜，倾斜的位置。
: q/ J1 ^/ q; \7 yCylindrical a 圆柱形的，桶状的。