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托福阅读事实信息题合集之TPO28-1

信息来源:网络  发布时间:2015-06-19

  托福阅读事实信息题是阅读考试中比较常见的一种题型,tpo则是托福阅读 备考最权威的材料,所以托福小编综合二者,为大家集中整理了tpo阅读中考察的事实信息题及其对应的解析,供大家参考使用。本文带来的是TPO28-1的事实信息题,一起来看看吧。

  TPO28-1 Groundwater

  Paragraph 1:

  Most of the world’s potable water----freshwater suitable for drinking----is accounted for by groundwater, which is stored in the pores and fractures in rocks. There is more than 50 times as much freshwater stored underground than in all the freshwater rivers and lakes at the surface. Nearly 50 percent of all groundwater is stored in the upper 1,000 meters of Earth. At greater depths within Earth, the pressure of the overlying rock causes pores and cracks to close, reducing the space that pore water can occupy, and almost complete closure occurs at a depth of about 10 kilometers. The greatest water storage, therefore, lies near the surface.

  2.According to paragraph 1, groundwater differs from the water in rivers and lakes in terms of its

  O portability

  O usefulness

  O abundance

  O cost

  解析:对应原文第二句话,也就是将地下水和江河湖泊水进行比较的那句话。原句说more than 50 times。就证明是地下水的水量大。这里A是饮用性,原文并没有说江水不能喝。B是有用,同理。D是代价。这个就更没提到了。所以答案为C丰富。

  【1】世界上绝大部分饮用水----可以饮用的淡水----都是地下水,它们储藏在岩石孔隙和裂缝中。储藏于地下的淡水是地表淡水河流和湖泊中总水量的50倍。大约50%的地下水存在于地下深1000m以内的地层中。随深度增加,上覆岩层压力使岩石孔隙和裂缝闭合,减少了水的储存空间,而超过10公里深的地下孔隙几乎全部闭合。因此绝大部分水储存于接近地表的地层中。

  Paragraph 2:

  Groundwater is stored in a variety of rock types. A groundwater reservoir from which water can be extracted is called an aquifer. We can effectively think of an aquifer as a deposit of water. Extraction of water depends on two properties of the aquifer: porosity and permeability. Between sediment grains are spaces that can be filled with water. This pore space is known as porosity and is expressed as a percentage of the total rock volume. Porosity is important for water-storage capacity, but for water to flow through rocks, the pore spaces must be connected. The ability of water, or other fluids, to flow through the interconnected pore spaces in rocks is termed permeability. In the intergranular spaces of rocks, however, fluid must flow around and between grains in a tortuous path; this winding path causes a resistance to flow. The rate at which the flowing water overcomes this resistance is related to the permeability of rock.

  5.According to paragraph 2, what does porosity determine?

  O The rate at which the aquifer’s water overcomes resistance to flow

  O The amount of water that the aquifer can hold

  O The likelihood that fractures and joints will occur in the aquifer

  O The depth underground at which the aquifer lies

  解析:A决定于permeability of rack,对应本段最后一句。B正确,对应本段第七句(porosity is important for water-storage capacity),这句话只要根据porosity定位就很好找。C和porosity没有直接关系。D原文就没提到。

  【2】地层水储存在多种岩石中。可以取出的地下水的聚集层叫做水层。我们可以认为水层即水的聚集地层。从地层中取水取决于水层的两个因素:孔隙度和渗透率。沉积颗粒之间的空间可以储存水,这种孔隙空间由孔隙度表征。孔隙度是岩石孔隙体积与总体积的百分比。孔隙度对地层储水能力尤为重要,但欲使水从岩石中流出,孔隙之间必须相互连通。水或其它流体从相互连通的孔隙中流动的能力即为渗透率。在粒间孔发育的岩石中,流体必须在颗粒周围的曲折通道中流动;这种曲折通道会对流动产生阻力。水克服阻力流动的速率与岩石渗透率相关。

  Paragraph 3:

  Sediment sorting and compaction influence permeability and porosity. The more poorly sorted or the more tightly compacted a sediment is ,the lower its porosity and permeability. Sedimentary rocks----the most common rock type near the surface----are also the most common reservoirs for water because they contain the most space that can be filled with water. Sandstones generally make good aquifers, while finer-grained mudstones are typically impermeable. Impermeable rocks are referred to as aquicludes. Igneous and metamorphic rocks are more compact, commonly crystalline, and rarely contain spaces between grains. However, even igneous and metamorphic rocks may act as groundwater reservoirs if extensive fracturing occurs in such rocks and if the fracture system is interconnected.

  7.The word “compacted” in the passage is closest in meaning to

  O hard

  O compressed

  O heavy

  O deeply buried

  解析:compact是压缩,紧密的意思。通过后面的and的并列内容可以推出其词义,因为and后面说rarely contain space,那就是说中间的空间很小。所以选择B压缩的。A是坚硬,C是重的,D是深埋的。

  【3】沉积物的分选性和压实程度影响其渗透率和孔隙度。岩石分选越差或压实越紧则其孔隙度和渗透率越低。沉积岩----地表最常见的岩石----也是最常见的水储集层,因为它们常带有最多的可以储水的孔隙空间。砂岩一般是最好的储水层,但小颗粒的泥岩则通常不可渗透。不渗透岩层都称为隔水层。火成岩和变质岩压实更紧,通常有结晶,并几乎没有粒间孔隙。但是即便是火成岩和变质岩也可因裂缝大量发育并相互连接而成为储水层。

  8.According to paragraph 3, when can igneous rock serve as an aquifer?

  O When it has many connected fractures

  O When it lies next to metamorphic rock

  O When it lies relatively near the surface

  O When it is crystalline

  解析:对应本段文章最后一句“even igneous rocks may act as groundwater…”后半句给出的就是答案,那么它说的是要有fractures并且要interconnected。所以选A。

  【3】沉积物的分选性和压实程度影响其渗透率和孔隙度。岩石分选越差或压实越紧则其孔隙度和渗透率越低。沉积岩----地表最常见的岩石----也是最常见的水储集层,因为它们常带有最多的可以储水的孔隙空间。砂岩一般是最好的储水层,但小颗粒的泥岩则通常不可渗透。不渗透岩层都称为隔水层。火成岩和变质岩压实更紧,通常有结晶,并几乎没有粒间孔隙。但是即便是火成岩和变质岩也可因裂缝大量发育并相互连接而成为储水层。

  以上就是托福阅读TPO28-1中的事实信息题及其解析,大家可以在备考的时候参考复习,希望能够帮助大家的考前准备。最后前程百利祝大家都能取得理想的托福考试 成绩。

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