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2012å¹´12月英è¯å››çº§é€‰è¯�填空专项è®ç»ƒ
- 第1页:UnitOne
- 第2页:Unit Two
- 第3页:UnitThree
- 第4页:UnitFour
- 第5页:UnitFive
- 第6页:Unit Six
- 第7页:UnitSeven
- 第8页:Unit Eight
- 第9页:Unit Nine
- 第10页:UnitTen
- 第11页:UnitEleven
- 第12页:UNIT 12
- 第13页:UnitThirteen
- 第14页:Unit Fourteen
- 第15页:Unit Fifteen
- 第16页:UnitSixteen
- 第17页:UnitSeventeen
- 第18页:Unit Eighteen
- 第19页:Unit Nineteen
- 第20页:Unit Twenty
- 第21页:UNIT 21
- 第22页:UnitTwenty-Two
- 第23页:Unit Twenty-Three
- 第24页:UnitTwenty-Four
- 第25页:UnitTwenty-Five
- 第26页:Unit Twenty-Six
- 第27页:UnitTwenty-Seven
- 第28页:UnitTwenty-Eight
- 第29页:UnitTwenty-Nine
- 第30页:Unit Thirty
- 第31页:Unit Thirty-Two
- 第32页:Unit Thirty-Two
- 第33页:Unit Thirty
- 第34页:Unit Thirty-One
- 第35页:Unit Thirty-Five
- 第36页:Unit Thirty-Six
- 第37页:Unit Thirty-Seven
- 第38页:Unit Thirty-Eight
  Unit Twenty-Three
  Passage 2
  The difference between a liquid and a gas is obvious under the conditions of temperature and pressure commonly found at the surface of the Earth. A liquid can be kept in an open container and fill it to the level of a free surface. A gas forms no free surface but tends to diffuse throughout the 11 available; it must therefore be kept in a closed container or held by a gravitational field, as in the 12 of a planet’s atmosphere. The distinction was a 13 feature of early theories describing the phases of matter. In the nineteenth century, for example, one theory maintained that a liquid could be "dissolved" in a vapor without losing its identity, and another theory 14 that the two phases are made up of different kinds of molecules. The theories now prevailing take a quite different approach by emphasizing what liquids and gases have in 15 They are both forms of matter that have 6 structure, and they both flow readily.
  The fundamental similarity of liquids and gases becomes clearly apparent when the temperature and pressure are 17 somewhat. Suppose a closed container 18 filled with a liquid is heated. The liquid expands, or in other words becomes less dense; some of it evaporates. In contrast, the vapor above the liquid surface becomes denser as the evaporated molecules are 19 to it. The combination of temperature and pressure at which the densities become 20
  is called the critical point.
  Passage 2
  The difference between a liquid and a gas is obvious under the conditions of temperature and pressure commonly found at the surface of the Earth. A liquid can be kept in an open container and fill it to the level of a free surface. A gas forms no free surface but tends to diffuse throughout the 11 available; it must therefore be kept in a closed container or held by a gravitational field, as in the 12 of a planet’s atmosphere. The distinction was a 13 feature of early theories describing the phases of matter. In the nineteenth century, for example, one theory maintained that a liquid could be "dissolved" in a vapor without losing its identity, and another theory 14 that the two phases are made up of different kinds of molecules. The theories now prevailing take a quite different approach by emphasizing what liquids and gases have in 15 They are both forms of matter that have 6 structure, and they both flow readily.
  The fundamental similarity of liquids and gases becomes clearly apparent when the temperature and pressure are 17 somewhat. Suppose a closed container 18 filled with a liquid is heated. The liquid expands, or in other words becomes less dense; some of it evaporates. In contrast, the vapor above the liquid surface becomes denser as the evaporated molecules are 19 to it. The combination of temperature and pressure at which the densities become 20
  is called the critical point.
|
A. added |
B. case |
C. |
prominent |
D. |
held |
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E. equal |
F. partially |
G. |
example |
H. |
previous |
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' I. space |
J, lifted |
K. |
permanent |
L. |
particularly |
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M. extended |
N. raised |
0. |
common |
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