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.
Aquifers, Porosity and Permeability
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.
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.
The Water Table
The water table is the underground boundary below which all the cracks and pores are filled with water. In some cases, the water table reaches Earth’s surface, where it is expressed as rivers, lakes and marshes. Typically, though, the water table may be tens or hundreds of meters below the surface. The water table is not flat but usually follows the contours of the topography. Above the water table is the vadose zone, through which rainwater percolates. Water in the vadose zone drains down to the water table, leaving behind a thin coating of water on mineral grains. The vadose zone supplies plant roots near the surface with water.
Because the surface of the water table is not flat but instead rises and falls with topography, groundwater is affected by gravity in the same fashion as surface water. Groundwater flows downhill to topographic lows. If the water table intersect the land surface, groundwater will flow out onto the surface at springs, weather to be collected there or to subsequently flow farther along a drainage. Groundwater commonly collects in stream drainages but may remain entirely beneath the surface of dry stream-beds in arid regions. In particularly wet years, short stretches of an otherwise dry stream-bed may have flowing water because the water table rises to intersect the land surface.
[Glossary]
Sediment: materials (such as sand or small rocks) that are deposited by water, wind, or glacial ice.
Topography: the shape of a surface such as Earth’s, including the rise and fall of such features as mountains and valleys.
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.
1.In paragraph 1, why does the author mention “the pressure of the overlying rock”?
O To show how water can be forced deep under Earth’s surface
O To show why groundwater is more plentiful than surface freshwater
O To correct a commonly made error about the location of groundwater
O To explain why most groundwater lies near Earth’s 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
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.
3.The word “extracted” in the passage is closest in meaning to
O used
O poured
O removed
O kept out
4.The word “termed” in the passage is closest in meaning to
O considered
O called
O limited to
O caused by
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
6.According to paragraph 2, what is the relationship between permeability and porosity?
O The more pores a rock has, the higher its porosity but the lower its permeability.
O Rocks with many internal spaces that are not connected with each other will have high porosity but low permeability.
O If water flows through a rock easily, it has high permeability but low porosity.
O Rocks that have high permeability have high porosity and vice versa.
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
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
Paragraph 4: The water table is the underground boundary below which all the cracks and pores are filled with water. In some cases, the water table reaches Earth’s surface, where it is expressed as rivers, lakes and marshes. Typically, though, the water table may be tens or hundreds of meters below the surface. The water table is not flat but usually follows the contours of the topography. Above the water table is the vadose zone, through which rainwater percolates. Water in the vadose zone drains down to the water table, leaving behind a thin coating of water on mineral grains. The vadose zone supplies plant roots near the surface with water.
9.The word “coating” in the passage is closest in meaning to
O stream
O barrier
O amount
O layer
10.Paragraph 4 implies which of the following about the roots of plants?
O They prevent water from reaching the vadose zone.
O They mark the boundary between the vadose zone and the water table
O They do not typically get their water from the water table.
O They help keep the water table from dropping farther.
Paragraph 5: Because the surface of the water table is not flat but instead rises and falls with topography, groundwater is affected by gravity in the same fashion as surface water. Groundwater flows downhill to topographic lows. If the water table intersect the land surface, groundwater will flow out onto the surface at springs, weather to be collected there or to subsequently flow farther along a drainage. Groundwater commonly collects in stream drainages but may remain entirely beneath the surface of dry stream-beds in arid regions. In particularly wet years, short stretches of an otherwise dry stream-bed may have flowing water because the water table rises to intersect the land surface.
11. Which of the sentences below best expresses the essential information in the highlighted sentence in the passage? Incorrect choices change the meaning in important ways or leave out essential information.
O Groundwater only flows out of the ground if the water table intersects the land surface.
O If the land surface and the water table intersect, groundwater can flow underground.
O Groundwater may be drained if springs occur where the water table intersects the land surface.
O Where the water table meets the land surface, groundwater flows out through surface springs.
12.Paragraph 5 implies which of the following about the level of the water
O It may rise or fall from year to year, depending on annual rainfall.
O It does not vary in arid regions.
O It rarely intersects the land surface of most regions.
O It is unrelated to the rate at which groundwater flows.
Paragraph 4: The water table is the underground boundary below which all the cracks and pores are filled with water. In some cases, the water table reaches Earth’s surface, where it is expressed as rivers, lakes and marshes. ■Typically, though, the water table may be tens or hundreds of meters below the surface. ■The water table is not flat but usually follows the contours of the topography. ■Above the water table is the vadose zone, through which rainwater percolates. ■Water in the vadose zone drains down to the water table, leaving behind a thin coating of water on mineral grains. The vadose zone supplies plant roots near the surface with water.
13. Look at the four squares [■] that indicate where the following sentence could be added to the passage.
This is a consequence of the slow rate of movement of the groundwater, which often prevents the water table from attaining a flat (horizontal) level.
Where would the sentence best fit?
14. Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selecting the THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points.
Most of the world’s potable water is stored as groundwater in the pores and fractures of underground rock, much of it at depths of less than 1,000 meters.
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Answer Choices
O Sedimentary rock may make poor aquifers because of tightly compacted sediment, which reduces porosity and permeability.
O Porosity is a measure of the empty space within rock while permeability measures the degree to which water can flow freely through rock.
O In arid regions, the water tables remain at a constant level far below the surface, preventing stream-beds from filling up even during wet years.
O Groundwater reservoirs are characterized by the porosity and permeability of the rock in which they lie, and these factors vary according to the type of rock.
O The vadose zone is typically dry because water does not stay in it, but instead percolates down to aquifers below or drains out through springs and streams.
O Although the water table usually follows the contours of the land surface, its level may vary from year to year and may intersect to the surface in places.
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14. Porosity is a measure of the…
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Although the water table usually …
世界上絕大部分飲用水----可以飲用的淡水----都是地下水，它們儲藏在巖石孔隙和裂縫中。儲藏于地下的淡水是地表淡水河流和湖泊中總水量的50倍。大約50%的地下水存在于地下深1000m以內的地層中。隨深度增加，上覆巖層壓力使巖石孔隙和裂縫閉合，減少了水的儲存空間，而超過10公里深的地下孔隙幾乎全部閉合。因此絕大部分水儲存于接近地表的地層中。
水層，孔隙度和滲透率
地層水儲存在多種巖石中�？梢匀〕龅牡叵滤木奂瘜咏凶鏊畬�。我們可以認為水層即水的聚集地層。從地層中取水取決于水層的兩個因素：孔隙度和滲透率。沉積顆粒之間的空間可以儲存水，這種孔隙空間由孔隙度表征�？紫抖仁菐r石孔隙體積與總體積的百分比�？紫抖葘Φ貙觾λ芰τ葹橹匾�，但欲使水從巖石中流出，孔隙之間必須相互連通。水或其它流體從相互連通的孔隙中流動的能力即為滲透率。在粒間孔發(fā)育的巖石中，流體必須在顆粒周圍的曲折通道中流動；這種曲折通道會對流動產生阻力。水克服阻力流動的速率與巖石滲透率相關。
沉積物的分選性和壓實程度影響其滲透率和孔隙度。巖石分選越差或壓實越緊則其孔隙度和滲透率越低。沉積巖----地表最常見的巖石----也是最常見的水儲集層，因為它們常帶有最多的可以儲水的孔隙空間。砂巖一般是最好的儲水層，但小顆粒的泥巖則通常不可滲透。不滲透巖層都稱為隔水層。火成巖和變質巖壓實更緊，通常有結晶，并幾乎沒有粒間孔隙。但是即便是火成巖和變質巖也可因裂縫大量發(fā)育并相互連接而成為儲水層。
地下水位
地下水位指地層巖石裂縫和孔隙充滿水的邊界。某些情況下，地下水位可能到達地表，在那里它以河流、湖泊或沼澤地的形式存在。但通常情況下地下水位位于地面數(shù)十或數(shù)百米以下。地下水位不是水平的，而是通常沿著地勢起伏。地下水位以上稱為包氣帶，在這里降水得以過濾。包氣帶中的水會沉降到地下水位，只在礦物顆粒表面留下一層水膜。包氣帶為地表附近植物根部提供水分。
因為地下水位表面并非水平，而是沿著地勢起伏，地下水和地表水受到重力影響的模式相同。地下水沿著下傾地層流向地勢低洼處。如果地下水位與地表相交，地下水將以噴泉的形式流出地面，要么就地聚集，要么沿排水通道流向更遠的地方。地下水通常在小溪中聚集，但在干旱地區(qū)也可能全部停留在干涸河床下。在特定濕潤的年月里，一段干涸的河床下游可能有水流動，因為地下水位抬升到了那里的地表以上。
