2023-05-30 12:58:43 来源：中国教育在线

托福阅读真题Official 51 Passage 2（三）

Surface Fluids on Venus and Earth

A fluid is a substance,such as a liquid or gas,in which the component particles(usually molecules)can move past one another.Fluids flow easily and conform to the shape of their containers.The geologic processes related to the movement of fluids on a planet’s surface can completely resurface a planet many times.These processes derive their energy from the Sun and the gravitational forces of the planet itself.As these fluids interact with surface materials,they move particles about or react chemically with them to modify or produce materials.On a solid planet with a hydrosphere the combined mass of water on,under,or above a planet’s surface and an atmosphere,only a tiny fraction of the planetary mass flows as surface fluids.Yet the movements of these fluids can drastically alter a planet.Consider Venus and Earth,both terrestrial planets with atmospheres.

Venus and Earth are commonly regarded as twin planets but not identical twins.They are about the same size,are composed of roughly the same mix of materials,and may have been comparably endowed at their beginning with carbon dioxide and water.However,the twins evolved differently,largely because of differences in their distance from the Sun.With a significant amount of internal heat,Venus may continue to be geologically active with volcanoes,rifting,and folding.However,it lacks any sign of a hydrologic system(water circulation and distribution):there are no streams,lakes,oceans,or glaciers.Space probes suggest that Venus may have started with as much water as Earth,but it was unable to keep its water in liquid form.Because Venus receives more heat from the Sun,water released from the interior evaporated and rose to the upper atmosphere where the Sun’s ultraviolet rays broke the molecules apart.Much of the freed hydrogen escaped into space,and Venus lost its water.Without water,Venus became less and less like Earth and kept an atmosphere filled with carbon dioxide.The carbon dioxide acts as a blanket,creating an intense greenhouse effect and driving surface temperatures high enough to melt lead and to prohibit the formation of carbonate minerals.Volcanoes continually vented more carbon dioxide into the atmosphere.On Earth,liquid water removes carbon dioxide from the atmosphere and combines it with calcium,from rock weathering,to form carbonate sedimentary rocks.Without liquid water to remove carbon from the atmosphere,the level of carbon dioxide in the atmosphere of Venus remains high.

Like Venus,Earth is large enough to be geologically active and for its gravitational field to hold an atmosphere.Unlike Venus,it is just the right distance from the Sun so that temperature ranges allow water to exist as a liquid,a solid,and a gas.Water is thus extremely mobile and moves rapidly over the planet in a continuous hydrologic cycle.Heated by the Sun,the water moves in great cycles from the oceans to the atmosphere,over the landscape in river systems,and ultimately back to the oceans.As a result,Earth’s surface has been continually changed and eroded into delicate systems of river valleys—a remarkable contrast to the surfaces of other planetary bodies where impact craters dominate.Few areas on Earth have been untouched by flowing water.As a result,river valleys are the dominant feature of its landscape.Similarly,wind action has scoured fine particles away from large areas,depositing them elsewhere as vast sand seas dominated by dunes or in sheets of loess(fine-grained soil deposits).These fluid movements are caused by gravity flow systems energized by heat from the Sun.Other geologic changes occur when the gases in the atmosphere or water react with rocks at the surface to form new chemical compounds with different properties.An important example of this process was the removal of most of Earth’s carbon dioxide from its atmosphere to form carbonate rocks.However,if Earth were a little closer to the Sun,its oceans would evaporate;if it were farther from the Sun,the oceans would freeze solid.Because liquid water was present,self-replicating molecules of carbon,hydrogen,and oxygen developed life early in Earth’s history and have radically modified its surface,blanketing huge parts of the continents with greenery.Life thrives on this planet,and it helped create the planet’s oxygen and nitrogen-rich atmosphere and moderate temperatures.

Question 5 of 14

According to paragraph 2,what is one difference between Earth and Venus?

A.Earth has less water in its atmosphere than Venus does.

B.Earth has a hydrologic system,but Venus does not.

C.Earth is less geologically active than Venus is.

D.Earth has more carbon dioxide than Venus does.

正确答案：B

题目详解

题型分类：事实信息题

原文定位：整个段落都在讨论这个内容，可直接通过选项定位。

选项分析：

B选项，根据选项关键词hydrologic system定位到第五句：However,it lacks any sign of a hydrologic system，it指代前面的金星，和B选项对应。

A选项，根据选项关键词water定位到第六句至第九句，金星离太阳近，热量多，水蒸发了，选项说反。

C选项，根据选项关键词geologically active定位到第四句Venus may continue to be geologically active with volcanoes,rifting,and folding下一段开头地球地质活动也很活跃，所以看不出谁更活跃。

D选项，根据选项关键词carbon dioxide定位到第九句和倒数第二句，Venus...kept an atmosphere filled with carbon dioxide.On Earth,liquid water removes carbon dioxide from the atmosphere得知地球上有水移除二氧化碳，所以应该是地球上二氧化碳少。

Question 6 of 14

It can be inferred from paragraph 2 that Earth evolved differently than Venus did in part because

A.there was more volcanic activity on early Venus than on early Earth

B.they received different amounts of solar energy

C.their interiors contained different amounts of heat

D.their early atmospheres contained different levels of oxygen and nitrogen

正确答案：B

题目详解

题型分类：推论题

原文定位：根据定位词Earth evolved differently than Venus定位到第三句。

选项分析：

However,the twins evolved differently,largely because of differences in their distance from the Sun可知他们距离太阳的远近不同，即接收的能量不同，与B选项一致。

A选项，没提及