



7月12日 第1篇
6 f# u4 x6 O/ i V v- Z7 a. Q分类下 earth science 94 A( W$ a" U/ F: H
Questions 42-46 Listen to part of a radio program about science.- M/ q; S0 K8 [
- e6 ~3 q4 z. k# N$ a: ^% J5 JScientists are always (looking up) on the lookout for alternative sources of energy. Today we are going to discuss one that’s so plentiful they say it could supply more energy than all the coal and oil in the world. It’s found in something called gas hydrate and, believe it or not, that’s a kind of ice." p* H$ x1 E2 I# s4 B
That’s right. But water in this ice was (weighed) way down blow the earth’s surface when it was frozen. So it was under a lot of pressure. And trapped inside of the crystals (width) of ice are individual molecules of methane甲烷-that’s what’s in natural gas.
' @7 E+ t. K! U; Y7 s' l9 X) [9 y# D9 Z 1 [, j! N; J5 [+ b A E3 m- {
All this (methane) makes gas hydrate (put its strain stop) pretty strange stuff. If you touch a match划火柴 to a piece of this ice, it’ll burst (and) into flame. And when geologists bring a chunk of it up to the surface to study at normal air pressure and temperature, gas hydrate begins to hiss斯斯作响 and bubble-and in (last) less than half an hour, the ice melts and the methane inside escapes into the air.
: q: F* e% K5 C; W% _! M7 E# d" G& cNow, as you might guess, this can make gas hydrate kind of hard for miners矿工 to handle. And then there’s the problem of where it’s located in frozen arctic北极
, o6 h2 s, S7 d% j, p J* Aregions or in ocean waters off the Atlantic大西洋 coast-and up to a mile down.
) Q# m" ?) q+ L. {( U1 C# w% s
% m% a% B1 O D& zEnvironmentalists warn that mining it could even be disastrous. Offshore drilling could (a loss) allow seawater to (save) seep down into the huge ice deposit and release tons of methane up into the atmosphere. And methane, our listeners may recall, is a green house gas that could (even) really worsen the problem of global warming.
7 Q5 o! Y0 l. X* S3 |0 Z6 L" R% {5 E& g6 C4 \$ N+ @* c9 }. y% E V
8 L7 x) I& x0 H2 A& F$ J
5 b7 s! y) s l( X6 c(Though) So, gas hydrate may offer some interesting possibilities, but with all these drawbacks, I’m not going to hold my breath waiting for it to fuel my furnace.
% F) O- |# E' \: V8 K5 r- b- @' `/ o9 V% T8 A- w
7月12日 第2篇
, Q! F. s" a% |- A8 U! H/ r分类下 earth science 101 E( k' M* p5 k) V; `. W9 Q
Questions 39-43 Listen to part of the talk in a geology class.
$ U+ [4 b/ A& X- X+ V- k/ Y2 r " e* O7 o$ N3 y
Look at (up) our (the top graphic) topographical地形 map, and you’ll see that the middle third of the North American Continent-from the Rocky Mountains almost to the Mississippi River-is pretty flat. This is the Great Plains, this kind of area is sometimes called a prairie大草原, sometimes a steppe, that’s s-t-e-p-p-e. The defining features are level (2 rain) terrain水平梯田, dry climate and an absence of trees. The Great Plains are actually the (formal belt) former bed of shallow (in Learn) inland Sea. Over millions of years, sediment (like) left by the glaciers, water and wind smoothed (up to) out the dry sea bed.
! ~+ j" [0 s3 Z * z9 s& L4 ~- n& T1 q2 _( c
As I said, the Great Plains are bordered on the west by the Rocky Mountains. (As) And it’s really the Rockies that are responsible for the formation of the grasslands. The mountains are so high that they block the heavy (moisture) moist air traveling (east) eastward from the Pacific ocean. (Later) Lighter, drier air passes over the mountains. Until people intervened with irrigation and farms, only grass could grow on the dry windy plain. In fact, we can divide the Great Plains into three zones. In the west, where it’s driest and windiest, the grass is very short. In the eastern zone, there is more rain and grass grows as high as 360 centimeters. In the middle third, (that makes) there’s a mix of the grass species that grow to a (Indi tide) intermediate height.8 a& r7 f' \7 u2 s% O
8 h. Y6 z+ M) ?4 ]9 y9 l
7 u# }" B- B- q# G
; P/ u6 |% X- E& B' o/ Q7 R: j" @7月12日 第3篇
- N& w" |# C+ z9 \7 `9 q- m分类下 earth science 11: {% e3 e' ?; c6 T" ?( {
Questions 42-46 Listen to part of a lecture in a college class.
+ y5 L" B8 v7 _5 b+ Q
0 X- f$ f m I. ZSince we’ve been discussing alternative fuels lately, I wanted to pass on to you some information I read about a new fuel that’s been in the news a lot lately. It’s called A-21.$ i6 z, I- `% t+ w0 L. W, u
7 B0 j, A& l. Z; V* g9 {2 l q
It’s composed of water and a chemical known as naphtha石脑油. It seems to be a very promising fuel because it’s much cleaner than the gasoline that we use today. That’s not to say that it doesn’t pollute, but it is cleaner. A-21 isn’t like some other alternative fuels that require completely new types of engines. A-21 still works on regular everyday (come bus) combustion燃烧 engines-like the ones in cars-with only miner mechanical modifications. So changing over (won’t) wouldn’t be a big deal.
! K# Y* n6 a8 V9 ~' P7 Q
4 j' B3 Z/ K" m5 f0 U: i, O- ~You may (dare) doubt (one) some of these claims that many researchers have. Some people feared that because it contains about 45% water, it would freeze in the winter. But a small (modecule) amount of antifreeze防冻剂 was (actuate) added to it, and that seems to have solved the problem.
+ L7 ?1 P( E" R6 T4 u- \ X* { - w7 W' j% w/ }5 @( {9 G/ |
A-21 has recently undergone (three) street tests in buses in Reno里诺, Nevada内华达. So far, it seems (out) to work just fine. This is a good thing, specially in Nevada because the state government there has passed a law requiring that a large percentage of vehicles in Nevada run (out of) on alternative fuels. A-21 should help.
+ { ]! S- [: H9 a# W& M7月12日 第4篇' d) U; m: N# u. a8 a+ V
" p$ c# }) X- j8 O* o" R! A
分类下 earth science 12) e7 P. K1 L3 r8 L+ |: r
Questions 48-50 Listen to part of a lecture in a geography class
. e5 R. A9 R( G7 l/ B( O" yThe winds of a tornado are the most violent and destructive ones on Earth. Any of you who (seem) have seen one knows very well how (frying) frightening and powerful they are. What’s interesting about (this) them is scientists don’t actually know exactly why tornadoes occur. $ x1 ]% h/ h' a! V( R+ Z, o
/ K& U" N. R/ e4 EWe do know, however, what happens when tornadoes are formed. As you remember, (Afrantic) a front锋面! i* P$ P" L/ ]3 W: `
occurs when cool dry air from the north meets warm, humid air coming from the south, from the Gulf海湾
2 e7 c, g! q/ V; c1 i' `of Mexico, for tornadoes in the United States. Where these air (method) masses meet, a narrow zone of storm clouds develops, and thunderstorms and sometimes tornados occur.
5 ] N+ o+ u9 M$ G1 Q
3 u& v: p l. W0 I! JHow is this violent weather produced? Well, a mass of warm, humid air rises very rapidly. As it rises, more warmer air rushes in to replace it. This in-rushing air also rises, and in some cases, (this specially) especially (wind) when there is (stream) extreme thermal instability,
. ~3 ?/ L9 x& h! gbegins to rotate. When this happens, the rotating air forms a tornado. i/ ?* e) _. }+ g
( A; _5 o0 W, W! s' hEven if you’ve seen tornados only in movies, you know that they can demolish buildings in seconds. This is possible because when a tornado passes over a house, it sucks up air from around of the house, and so the air pressure outside the house drops rapidly. Inside, pressure remains the same. So air pressure inside is greater than air pressure outside. The result is that the building explodes outward. Next we’ll talk a little bit about how new technological developments are being used to try to predict tornados. 3 V& `3 M$ U3 K" a
# D7 B$ z! \- k- ~/ C2 G0 p6 K
' o1 c0 g4 ]' b2 H+ d7 f