我也是进来鼓掌的~~
. d  k% w( `! |0 t/ \! o2 [( Y3 c8 G
不过LZ如果问道女生可以多得钱的话通知我一声哈~~

7月10日 第一篇' U0 k! L! d- ]( L$ [1 G
分类下 biology 9
! ^" |3 P0 G  z# I3 h, GQuestions 43-46 Listen to a talk from a biology class., S; G8 B" g0 p

/ `9 B1 \5 u$ m) v) k6 jToday I want to talk to you about wasps and their nests. You’ll recall that biologists divide species of wasps into two groups: solitary and social.1 l* K9 t% h+ [
6 H, d: N( h' U9 K& E; R3 M
Solitary wasps, (that named its plans) as the name implies, do not live together with other wasps. In most species, the male and female get together only to mate, and then the female does all the work of building the nest and providing food for the (young springs) offspring (and) by herself. Solitary wasps usually make nests in the ground and they separate the chambers室 for individual offspring with bits of grass, stone or mud, whatever is handy." J# c# _  V6 ^9 }' g! |

# q8 V# k# d% C( i/ GWhat about social wasps? They form a community and work together to build and maintain the nest. A nest begins in the spring when the fertile受精的female called the queen builds the first few compartments of the nest and lays eggs. The first offspring are small females that (comes out and) cannot lay eggs. These females called workers then build a lot of new compartments and the queen lays more eggs. They also care for the new offspring and defend the nest (was stares) with their stingers刺. By the way, only female wasps have stingers. - j& e; E" X6 m7 V! A8 t7 B
* M) L: a  Q) Y* {
Most social wasps make nests of paper. The females produce the paper by chewing up plant fibers or old wood. They spread the paper in thin layers to make cells in which the queen lays her' c" }# ^( _  O
eggs. Most of you, I am sure, have seen these nests suspended from trees. They may also be built (on the ground) underground in abandoned rodent burrows. % r1 H) {2 k2 S9 x$ Q' f5 f1 t! n7 u

7月10日 第二篇
  l) U8 D' e1 J8 l$ E分类下 biology 13 这篇听的不好。。。. P# p) b& l9 i5 X
Questions 47-50 Listen to a guide speaker in a college class.0 g! u% k4 X# h9 |5 J8 Z
# i4 F5 x" H* R, X8 V3 k
As Doc. Miller mentioned, we’re trying to (we could) recruit征募
! O4 d* P6 Q* D  F; Lvolunteers for the Hawk Mountain Sanctuary禁猎区. But before I get into the details of the volunteer program, I’d just like to tell you a little about what we do there.
  G9 N  y  I  h- H( D6 `0 B- W! O
, F# g4 [8 H* _7 `8 \* VOne of our main jobs is to keep the detailed records of migration patterns of raptors猛禽. For those of you who don’t know, raptors are birds of prey, like hawks and eagles. Between August and December, we see around 20 different species migrating from Canada and New England-about 20,000 birds.0 q5 c# o( @' [0 ?" M2 i: h
- N+ K( X  d! N- \" R
(But what about for the) Part of what attracts them to Hawk Mountain is the location on the east (region)) w9 J' @$ V# G
ridge山脊of Appalachian阿巴拉契亚Mountains. What happens is that the sun warms the ridge in such a way that the air (creasy) currents are formed. The birds just (sought) sort of (glad) glide (of long year) along on the air-so they use up very little energy.
+ f9 Z- _1 S5 U# D, s: x
' p, a# N( a! q7 C2 }/ n8 cAs volunteers, you’ll be (happening as) helping us keep (airy) accurate counts of raptors. Any (drawing) drop in number could means something (goes around) gone wrong in the environment-because (texts I saw) of pesticides杀虫剂 or diseases-even hunting.$ V' i; l; `* U; U& C/ _& O- H
' `- J( O3 C6 g2 E# b
We just had a scare with the broad-winged hawks, their numbers have drop drastically over the last ten years. It was suggested that the birds may have changed their migratory迁移的 route. So for 11 days, we had several hundred volunteers-(dictioned) stationed every five miles-to observe and count. And sure enough, they discovered that instead of hugging the Appalachians as they’d always done, the broad-wings were cutting a wide path over the Delaware特拉华 river. Needless to say, (river) we were greatly relieved.

7月10日 第三篇8 U7 L! ]2 U+ {4 s4 M
分类下 earth science 1: |$ c0 D6 Y( T1 ^$ M) S4 Q3 T$ n
Questions 47-50 Listen to part of lecture in a geology class/ f. U6 o: P* @

0 r0 E1 p* ]+ m! G/ lI’m glad you (breed up) brought up a question (over) of our investigations into the make-up of the Earth’s interior. In fact, since this is the topic of your reading (the science) assignment for next time, let me spend (it) these last few minuets of class talking about it. There were several important discoveries in the early part of this century that helped geologists develop a more accurate picture of the Earth’s interior. & i5 G8 V4 k1 ]% g3 F
1 B; |9 M9 {0 o5 n) p
The first key discovery had to do with (science of earth) seismic地震的 waves-remember they’re the vibrations caused by earthquakes. Well, scientists found that they traveled thousands of miles though the Earth’s interior. This finding enabled geologists to study the inner parts of the Earth. You see, these studies revealed that these vibrations were of (two-steps) two types: compression-or P-waves and shear剪-or S-waves. And researchers found that P waves travel though both liquids and solids, while S waves travel only though solid matter. 7 w& U! M! z4 @% s7 I( |. s  c

5 K! t- Y) {- _1 q% ]In 1906, a British geologist discovered that P waves slowed down at a certain depth but kept traveling deeper. On the other hand, S waves either disappeared or were reflected back, so he concluded that the depth (must be) 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.
! U" j! j5 [! h% l; V9 C " |2 [. }) A- T! j) F
There’s still a lot to be learned about the Earth. For instance, geologists know the core is (hard) hot. Evidence of this is the (molled) molten lava that flows out of volcanoes. But we are still not sure what the source of this heat is./ `& w' c1 t6 {0 v" S

. c8 Z( i5 x% h. J5 l( D7月10日 第四篇6 }: l! b* A9 V
分类下 earth science 2
  @& ?2 v  r9 _+ d* G# W& @* \Questions 48-50 Listen to part of talk in a geology class0 R% y. t0 |* s  m
5 s9 v+ n* M8 R% l3 R& T6 U
Today I want to talk about the earth’s last major climate shift (and ended it up at) at the end of last Ice Age. % X8 o- [, r6 t

2 y) J" R% }/ n3 ?  H7 nBut first, let’s back up a moment and review what we know about (climate) climatic change in general. First, we defined climate as consistent patterns of weather over significant periods of time. $ w8 q0 N- W' P6 Q! }' p0 f# v

- @# _5 o$ n, X: V' @. y$ hIn general, changes in climate occur when the energy balance of the earth is disturbed. Solar energy (at) enters the earth’s atmosphere as light and is radiated by the earth’s surface as heat. Land, water and ice each affect this energy exchange differently. The system is so complex that (data) to date, (are) our best computer models are only (created on) crude粗略的 approximations and are not (sufficient) sophisticated enough to test (a pop say) hypotheses about the causes of climatic change.
. r3 ^" l0 P4 @& m) c9 R
1 A! q4 b4 p9 V1 @Of course, that doesn’t (keeps) keep us from speculating. For instance, volcanic火山的 activity is one mechanism that might affect climatic change. When large volcanoes erupt, they (disburse) disperse散开 tons of particles (that then enter) into the upper atmosphere where the particles then reflect light. Since (last) less light is entering the system of energy exchange, the result would be a cooling of the Earth’s surface. : }/ O0 @; x6 ^6 H& c! H5 P+ v. W
. E. \$ P% s" U: T
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.
* x* v( F7 Z/ U  Q* b4 s, S( M8 X

7月10日 第五篇  W' Y0 h0 A0 {
分类下 earth science 3
( M" T' r6 x, X6 r. FQuestions 44-46 Listen to a presentation being given in a geology class.) @+ }! U9 q- C: P# G# O0 Q5 m

$ n* f0 C) {& a3 v7 G. \I’d like to begin by thanking Dr. Kane for inviting me to be here today. Although I’m not a geologist, I have been collecting minerals for years. My collection is really diverse because I’ve traveled all over the world to find them. Today I’ve brought a few specimens for you to see. After I discuss each one, I’ll pass it around so you can look at it more closely.
3 }! O" k  a* ]
6 j. D7 R0 r+ s9 H5 N9 AAs you know, (cells borns) feldspars长石 are the most (abandoned) abundant minerals and are divided into a number of types. These first samples are orthoclases正长石. 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 collecting trip.) g( F; d9 X( d. x
: o4 u0 V- G; r
This next sample that I’ll pass around is a microcline微斜长石 mineral, also called amazonstone. You can identify it by its bright-green color. It’s often used in jewelry and really is quite attractive.- w) X; ~. V' k; K" Z" B  r
4 N6 w5 L% w  Q( ?8 l, h+ _( [
These final samples are all plagioclase斜长岩 feldspars. Many plagioclases are very rare, so I’m particularly proud of the variety in my collection.
/ d1 g) i2 p8 @5 f& L; [& G ) e: \. m$ F" C9 N4 ^( x
I’ve also brought a few slides of some larger mineral samples. And if you (turn up let’s know) turn out the lights now, I’d like to show them to you.: x, J" A7 p4 [/ |3 f
  
( f& u8 Y  g* U- {% F: q

7月11日 第一篇
& D- ?- `; Z9 @- J# M7 m" ?分类下 earth science 40 l% d- q- S2 u0 w- r4 L4 G' u
Question 39-41 Listen to a radio talk about fossil化石 fuels.# o! Q' ^  L/ d3 X! _8 K
Today I want to discuss fossil fuels, such as coal, oil and natural gas. The term ‘fossil fuel’ refers to the trapped remains of plants and animals in sedimentary沉积的 rock. You see, living plants trapped energy from the sun by the process of photosynthesis and (then) they store the energy in their chemical compounds. Most of that energy is released when the plant dies and decays. However, sometimes organic matter is buried, before it decays completely. In this way, some of solar energy becomes trapped in rocks-(has) hence the name: fossil fuel. Although the amount of organic matter trapped in any one growing season is small, (they) the accumulated remains (for) from millions of years are considerable. Because the accumulation rate is so slow-millions of times slower than (related) rate at which we (know decarp) now dig up this organic matter and burn it for energy-we must consider fossil fuels as nonrenewable resources. Tomorrow we’ll be discussing alternatives to fossil fuels that can be renewed.
2 N2 }, ~2 Y! r3 h& z, a# X! U7月11日 第二篇
4 D$ B7 d/ R$ \, a分类下 earth science 59 n3 x! [* {# H1 X4 e) g( [
Questions 40-43 Listen to part of talk in a geography class, g% k, `3 F+ D+ j: L0 D  w
: {! c) Z: R  y  o' m" D/ p
Not long ago, some of you may have read about a team of mountain-climbing scientists (to have) who helped to recalculate the elevation of the highest mountain in the world: Mountain Everest珠穆朗玛. Of course, the elevation of Mountain Everest was determined many years ago using traditional surveying methods. But these scientists wanted to make a more precise measurement using a new method that takes advantage of recent advances in technology. It’s called the Global Positioning System.! O8 ?: J; E- C7 c/ V/ j5 i
4 \: Q2 n7 e- h. o8 W. ]: V! X
The Global Positioning System uses 24 (cite lines) satellites that circle the Earth. Each of these satellites is (consistently) constantly sending out signals. And each signal contains important information that can be used to determine the longitude, latitude and elevation of any point on the Earth’s surface. 9 R$ G2 U( M' z) M6 L# i

& y0 u6 \1 k- f+ l9 A8 PWell, in order to use this system to calculate Mountain Everest’s elevation, scientists needed to put a special receiver on its summit to receive the signals from the satellites. The problem (of) with this was that, in the past, the receivers were much too heavy for climbers to carry. But now these receivers have been reduced to about the size and weight (as) of a (hand) handheld telephone, so climbers was able to take a receiver to the top of Everest and from there, to access the satellites system signals that (were a lot) would allow them to determine the precise elevation. And it turns out that the famous peak is actually a few feet higher than was previously thought.
, N& w; ^6 t- ^' K; a; j$ w7月11日 第三篇
3 M# [1 s! z5 y( o+ A3 u分类下 earth science 6$ y5 S- @; _* x9 e
Questions 40-42 Listen to a talk in a geography class  J9 Q! x1 m1 H, E0 v: p) F
; |- t2 v- D4 _( H
Now you’ve been reading articles about the tremendous damage done to life and property by earthquakes, that’s why seismologists have been working so hard to develop methods of earthquake prediction. We can now predict earthquakes (rarely) fairly well, but the predictions only locate potential areas of danger. They don’t predict the specific time and location (that had) at which an earthquake is likely to occur. Today I want to introduce to you three prediction models that have been developed.: [5 j0 ?# P4 u. N) Y; s1 @( u/ U

/ Q& j- c% N/ k3 HThe first prediction model looks along earthquake (fort) fault断层, those cracks in the earth’ crust, (the final) to find what are known as seismic gaps. Seismic gaps are places where (there have been) the fault has shown little or no seismic activity for a long time. This theory (pose) postulates假设 that such places are due for a major shock. 0 P* q! ]. r1 }/ w

+ p! R! e8 |( ^& DThe second model relies on phenomena-like ground tilt地斜. Using long cylindrical tubes圆柱管子 containing water, observers noted that ground tilt tended to occur before major earthquakes. That led them to correctly predicted the big High Chang quake in 1975, the first successful earthquake prediction scientists have ever made. A million people were evacuated撤退 from that Chinese city before the earthquake struck. Unfortunately, this method hasn’t work consistently, so we can’t say (its being effective) it’s been perfected.
7 w1 `7 |; G* d  \. c ) y( D! E5 ]  Y+ r3 v' y
The third model is based on the theory that major earthquakes closely followed a series of minor ones. (Studying) Starting with the measurements and timing of the smaller quakes, a complex formula calculates the times of increased probability of a much larger quake. Right now, this method like the first method, can not predict specific times and places, but that may change as it is further developed.
3 {* i7 K. D% P
1 Y& ^- Y6 O7 A" g* oFor the moment, none of these models can predict with reasonable levels of confidence.

明显看到进步了！你一天听这么多啊！我要向你学习！！！！
- D/ a1 u/ Y1 J% ?/ I6 K. D大家坚持！互相监督哦~

非常非常非常的佩服LZ~~~我辞职了………………

我休假了，利用这段时间，我要努力听写，努力提高听力，努力备考！$ R  G. j' e, q9 _7 t- T9 n
谢谢大家的鼓励，一起加油！
" o& T" j' [& D# C0 L& D1 t7月11日 第四篇
3 F1 V1 S4 G2 ?7 ^8 c4 E分类下 earth science 7
+ p6 H4 |4 Z7 T5 i
9 h5 L$ k; z6 `+ Y. gQuestions 42-45 Listen to part of the talk in an oceanography class.5 j: o+ F& s* S4 C5 `3 g/ W3 K

1 H7 o2 e( M' y4 A8 x- U8 KOne reason oceanographers analyze the sediment on the ocean floor is to see how (long turn) long-terms changes in earth’s temperature have affected the depth of the ocean. By analyzing the remains of sea animals in old layers of ocean sediment, oceanographers can determine the depth of the ocean in the past. They’ve analyzed hundreds of such layers, including some from the coldest periods of the Earth’s history-the Ice Ages. What they’ve found is that during the Ice Ages, the amount of water in the oceans decreased. Water levels in the oceans dropped by about a 400 feet. Water from the ocean evaporated, and became frozen in continental glaciers, so it didn’t (dream) drain back into the ocean. When temperatures eventually rose again, the glaciers (molted) melted and the oceans returned to their formal depths. Analysis of sedimentary data indicates that periods of (glacier) glacial freezing and melting occurred in regular cycles of 20,000, 40,000 and 100,000 years.
3 R8 B: i/ n$ P! ?. T 1 Z2 t- l/ n- Q7 V
Oceanographers are interested in the history of sea water levels because they hope to use this historical data in order to predict the possible effect that global warming could have on sea water levels. If the (industry or pollutions) industrial pollutants (keep) are capable of heating global temperatures to the point that glaciers begin to melt, it is urgent for us to know precisely how high sea levels will rise, as a result.

哪位帮我把86楼的补上啊