a我考网

 找回密码
 立即注册

QQ登录

只需一步,快速开始

扫一扫,访问微社区

查看: 180|回复: 2

[雅思模拟题] 2012年雅思阅读考试考前冲刺试题(23)

[复制链接]
发表于 2012-8-14 20:43:07 | 显示全部楼层 |阅读模式
2012年雅思阅读考试考前冲刺试题(23)
9 q1 h; G$ |$ k. }2 g1 There's a dimmer switch inside the sun that causes its brightness to rise and fall on timescales of around 100,000 years - exactly the same period as between ice ages on Earth. So says a physicist who has created a computer model of our star's core.
; l" H. @' n* r- _7 \5 B7 B  2 Robert Ehrlich of George Mason University in Fairfax, Virginia, modelled the effect of temperature fluctuations in the sun's interior. According to the standard view, the temperature of the sun's core is held constant by the opposing pressures of gravity and nuclear fusion. However, Ehrlich believed that slight variations should be possible.2 e9 |  Q: p) E. g
  3 He took as his starting point the work of Attila Grandpierre of the Konkoly Observatory of the Hungarian Academy of Sciences. In 2005, Grandpierre and a collaborator, Gábor ágoston, calculated that magnetic fields in the sun's core could produce small instabilities in the solar plasma. These instabilities would induce localised oscillations in temperature." O5 r5 u! P  w( |) M( [/ [* j: H
  4 Ehrlich's model shows that whilst most of these oscillations cancel each other out, some reinforce one another and become long-lived temperature variations. The favoured frequencies allow the sun's core temperature to oscillate around its average temperature of 13.6 million kelvin in cycles lasting either 100,000 or 41,000 years. Ehrlich says that random interactions within the sun's magnetic field could flip the fluctuations from one cycle length to the other.% N/ \& ?% z% t1 L: f# ]
  5 These two timescales are instantly recognisable to anyone familiar with Earth's ice ages: for the past million years, ice ages have occurred roughly every 100,000 years. Before that, they occurred roughly every 41,000 years.
% N% K8 j5 q$ x6 \. a0 I7 I' c  6 Most scientists believe that the ice ages are the result of subtle changes in Earth's orbit, known as the Milankovitch cycles. One such cycle describes the way Earth's orbit gradually changes shape from a circle to a slight ellipse and back again roughly every 100,000 years. The theory says this alters the amount of solar radiation that Earth receives, triggering the ice ages. However, a persistent problem with this theory has been its inability to explain why the ice ages changed frequency a million years ago.$ ]4 F* ?* b9 u* c1 G
  7 "In Milankovitch, there is certainly no good idea why the frequency should change from one to another," says Neil Edwards, a climatologist at the Open University in Milton Keynes, UK. Nor is the transition problem the only one the Milankovitch theory faces. Ehrlich and other critics claim that the temperature variations caused by Milankovitch cycles are simply not big enough to drive ice ages.
' V  Y4 a6 t, I; v6 w2 i; \  8 However, Edwards believes the small changes in solar heating produced by Milankovitch cycles are then amplified by feedback mechanisms on Earth. For example, if sea ice begins to form because of a slight cooling, carbon dioxide that would otherwise have found its way into the atmosphere as part of the carbon cycle is locked into the ice. That weakens the greenhouse effect and Earth grows even colder.
: t. M, b! w5 B% s/ R  t  9 According to Edwards, there is no lack of such mechanisms. "If you add their effects together, there is more than enough feedback to make Milankovitch work," he says. "The problem now is identifying which mechanisms are at work." This is why scientists like Edwards are not yet ready to give up on the current theory. "Milankovitch cycles give us ice ages roughly when we observe them to happen. We can calculate where we are in the cycle and compare it with observation," he says. "I can't see any way of testing [Ehrlich's] idea to see where we are in the temperature oscillation."
) V- b1 A( c3 d/ C5 U2 z8 N; q; a+ ~# N9 {9 X
  10 Ehrlich concedes this. "If there is a way to test this theory on the sun, I can't think of one that is practical," he says. That's because variation over 41,000 to 100,000 years is too gradual to be observed. However, there may be a way to test it in other stars: red dwarfs. Their cores are much smaller than that of the sun, and so Ehrlich believes that the oscillation periods could be short enough to be observed. He has yet to calculate the precise period or the extent of variation in brightness to be expected.1 2 3尾页
回复

使用道具 举报

 楼主| 发表于 2012-8-14 20:43:08 | 显示全部楼层

2012年雅思阅读考试考前冲刺试题(23)

 Questions 1-4</p>  Complete each of the following statements with One or Two names of the scientists from the box below.
  D8 X9 [" V( X1 ^% P2 Q9 x  Write the appropriate letters A-E in boxes 1-4 on your answer sheet.
- a. G) R% H: u/ D( R  A. Attila Grandpierre7 b% b% E2 |8 J/ P* T
  B. Gábor ágoston: X3 f* u% Z* N
  C. Neil Edwards
% c: q2 [0 h4 c% {- G  D. Nigel Weiss2 w8 y* I8 g7 ]: B" [4 J( w
  E. Robert Ehrlich  @0 S1 w9 S* p: f  c, c- d
  1. ...claims there a dimmer switch inside the sun that causes its brightness to rise and fall in periods as long as those between ice ages on Earth.6 r# F( [. [1 F) v# s& ~2 y4 e
  2. ...calculated that the internal solar magnetic fields could produce instabilities in the solar plasma.8 ]" R1 k$ P- _. G
  3. ...holds that Milankovitch cycles can induce changes in solar heating on Earth and the changes are amplified on Earth.
, i& H% w7 c  k2 p4 y, D  4. ...doesn't believe in Ehrlich's viewpoints at all.
+ j! M& u  L3 E) b# O$ t6 {% a0 @! D# R
  Questions 5-91  2 3尾页
回复 支持 反对

使用道具 举报

 楼主| 发表于 2012-8-14 20:43:09 | 显示全部楼层

2012年雅思阅读考试考前冲刺试题(23)

 Answer keys and explanations:</p>  1. E
% ]2 n+ p& u* W6 J; }2 X0 R  See the sentences in paragraph 1(There's a dimmer switch inside the sun that causes its brightness to rise and fall on timescales of around 100,000 years - exactly the same period as between ice ages on Earth. So says a physicist who has created a computer model of our star's core.) and para.2 (Robert Ehrlich of George Mason University in Fairfax, Virginia, modelled the effect of temperature fluctuations in the sun's interior.)
9 i4 O: r% |" j  Z  2. A B1 A0 g& _2 f+ F7 z9 ]% T" e; i
  See para.3: Grandpierre and a collaborator, Gábor ágoston, calculated that magnetic fields in the sun's core could produce small instabilities in the solar plasma.
3 G( J7 E+ F4 S1 z" R, m5 U# O  3. C
: H! w7 d+ e0 R8 R  See para.8: Edwards believes the small changes in solar heating produced by Milankovitch cycles are then amplified by feedback mechanisms on Earth.
! f% K2 f8 V& }1 d  4. D
: J. R5 q- \5 f0 J2 H6 L9 s  See para.11: Nigel Weiss, a solar physicist at the University of Cambridge, is far from convinced. He describes Ehrlich's claims as "utterly implausible".7 b0 f7 _3 C# G) K7 o: ^
  5. False" `6 `" I# `8 R6 u1 L/ V3 F
  See para.5: for the past million years, ice ages have occurred roughly every 100,000 years. Before that, they occurred roughly every 41,000 years.8 J0 F0 w' n% ?  J3 r1 U7 {/ d1 p
  6. False
! l- q$ v' S" Y  See para.7: "In Milankovitch, there is certainly no good idea why the frequency should change from one to another," ... Nor is the transition problem the only one the Milankovitch theory faces.中 华 考 试 网% Y; }' ]* m( ^2 [3 n: B
  7. Not Given8 m# J' {5 B: F8 ~) m/ u) J3 ?  y
  See para.8: if sea ice begins to form because of a slight cooling, carbon dioxide?is locked into the ice. That weakens the greenhouse effect. (The passage doesn抰 mention anything about locking Co2 into ice artificially.)" n* A5 N8 a: |6 F
  8. True% I' Q% _- ^; x1 O- Z  Q- Q0 N
  See para.9: there is no lack of such mechanisms. "If you add their effects together, there is more than enough feedback to make Milankovitch work,"?"The problem now is identifying which mechanisms are at work." This is why scientists like Edwards are not yet ready to give up on the current theory.! G% x$ |+ g: t
  9. True& l+ `1 `2 u4 \6 E' i: A( Y
  See the sentences in para.9 (According to Edwards, he says. "I can't see any way of testing [Ehrlich's] idea to see where we are in the temperature oscillation.") and para.10 (Ehrlich concedes this. "If there is a way to test this theory on the sun, I can't think of one that is practical).
1 V+ b" b; _, N  10. constant
8 K3 Z# D1 `7 z$ h  See para.2: According to the standard view, the temperature of the sun's core is held constant by the opposing pressures of gravity and nuclear fusion.2 ^: H$ r& }- G5 J+ _
  11. orbit4 J0 \9 }! ~( p$ b
  See para.6: Most scientists believe that the ice ages are the result of subtle changes in Earth's orbit, Earth's orbit gradually changes shape from a circle to a slight ellipse and back again roughly every 100,000 years.8 E* E: Z  K2 K4 i' V

/ g, Q6 {: K3 V; l( u" ^, Q  12. instabilities1 2  3 尾页
回复 支持 反对

使用道具 举报

您需要登录后才可以回帖 登录 | 立即注册

本版积分规则

Archiver|手机版|小黑屋|Woexam.Com ( 湘ICP备18023104号 )

GMT+8, 2024-5-8 11:16 , Processed in 0.287771 second(s), 25 queries .

Powered by Discuz! X3.4 Licensed

© 2001-2017 Comsenz Inc.

快速回复 返回顶部 返回列表