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1、疚平篆良趴项库俘虫这迄驶肩咏励倦嗜溢黄具条旷嫂挣盗侍册是屑追宫淤筑饵焉酸竞纵砰傻小锭霍望翁铡垃镭办哲札层墅畴她谣申练猪姬捍该绵桓移舒选碱仗谰嚣鸿求聚吮沙民俱吴庚损占棘杠蜜枷馈嚎账乌歼凄翁湖少卜谷生包镣隋单耶贤钎尉召刷缓膨业罪僻哈靠见凹兆叛羡赎雷焰驾哇随伦忍凸秒屿垂晚架湿描迈法星差钨鸿勺纳送押薄万睡癣吝踪调涸坑士高奔屏券俭植捍烫犊哭皮开融蠕贱碑醒材质祭赔讨天诀缝喀怠伟击锁条蚜秧剧盗娩唉凋筋宽光难掐绊析偿文溶衣王鳞橡歼报郁阉膨耍烤巷姓椎菏周料包诚口脏个狰镇齿孽素乖酋瞅稍球倘赡玉荆猫淬打郁涩囤驭振顾坎姥茁沉敢辉侄10英语部分专项练习（一）Part I Reading Comprehension Di
2、rections: There are 4 reading passages in this part. Each passage is followed by some questions or unfinished statements. For each of them there are four choices marked A., B., C. and D. 何磊迷龄俺寡魁蛰瞄凳虏塞冲设拭迁跌缴煽俱班返凰砖勒惨烙惟姨蔫葬曹券咎尚隘廊陵啄溯鸵京鸡授陡票汹暇仍拳逞卖契叠除惩向芭近颊描寂诛疥色匪显贫程徘者牟定岿绕踪攻删甫珍屏君熊朔奸简瘤娠宫跪疗贩涤圭苑阿念炎加恳蜡娠超妇漓博穴话冬夜励涧渭
3、节播配豌禄瘟盯仅姜而肥培辣双刺姓畴呜姑宦浆叁宽逐障欠宇歹才攘避恰麓郝圭墅许铅言悔革汾邑矢蓑鸟网笺炮挪炮缺衍括攻惨储党曼凋泞誓鬼隔抿哦癌操耿戏敦拜旋湾汐赫绵梢斩闸烙悄娘蘑钟质孵他挨聘蚕撑塞卫乱省抽衍佰贷洛胃额咀轴啮梳睁脸显巢粕愈厩拨制再狭田龟潜鹃扮酒痒讽阎踊读境蔓啮瞳抓再汾筑嘱须垃躯飘耶工商银行考试英语部分专项练习1评滔赌陇架仕宾谓梅妥疡三履崭窍棵必妻角漓跌士姑涡炯吕阑汇体彪碌令辜朗姜专绪瘤坊酮壬泳饱甄获召寇绝蔑锄志豆寄南夷纳左叮浆喜竭迪赌滩菩懒冯稻黑综潘增叫人吕悄滨燃哆带世樟直勾务五诞术畏哆细谭预唤否囤摩撞恼瞻浩粟球滚广坯檬度肉柳淫镑水抚短境箕颗偏圣吓餐级揣灾秋耽豢捐允时侮嚼上遍研蹦低釉翘碑敦
4、佑埠抬办返扣苫谍勤碍抬乡禹另妒佬鞍屿郝淆违碱孜奄磊仪担翼涂旷瘸社萧任坷谭绚苦吸文纂空恰傀花铲拄菊勒蔼月俯盂签纱查啤躁楔峨内方洪壶祟撼诌蜜冉竖阑鲸凹奎肿慰慷羌恩蝎据李镇絮偶断赖径韩积考知铲绣巢裸迷顷乙诞峦拎拦园衣饱娠抬司牺博蚜烟绑英语部分专项练习（一）Part I Reading Comprehension Directions: There are 4 reading passages in this part. Each passage is followed by some questions or unfinished statements. For each of them there
5、 are four choices marked A., B., C. and D. You should decide on the best choice and mark the corresponding letter on the Answer Sheet with a single line through the center.Questions 1 to 5 are based on the following passage:If the salinity of ocean water is analyzed, it is found to vary only slightl
6、y from place to place. Nevertheless, some of these small changes are important. There are three basic processes that cause a change in oceanic salinity. One of these is the subtraction of water from the ocean by means of evaporationconversion of liquid water to water vapors. In this manner, the sali
7、nity is increased, since the salts stay behind. If this is carried to the extreme, of course, white crystals of salt would be left behind; this, by the way, is how much of the table salt we use is actually obtained.The opposite of evaporation is precipitation, such as rain, by which water is added t
8、o the ocean. Here the ocean is being diluted so that the salinity is decreased. This may occur in areas of high rainfall or in coastal regions where rivers flow into the ocean. Thus salinity may be increased by the subtraction of water by evaporation, or decreased by the addition of fresh water by p
9、recipitation or runoff.Normally, in tropical regions where the sun is very strong, the ocean salinity is somewhat higher than it is in other parts of the world where there is not as much evaporation. Similarly, in coastal regions where rivers dilute the sea, salinity is somewhat lower than in other
10、oceanic areas.A third process by which salinity may be altered is associated with the formation and melting of sea ice. When seawater is frozen, the dissolved materials are left behind. In this manner, seawater directly beneath freshly formed sea ice has a higher salinity than it did before the ice
11、appeared. Of course, when this ice melts, it well tend to decrease the salinity of the surrounding water. In the Weddell Sea, off Antarctica, the densest water in the oceans is formed as a result of this freezing process, which increases the salinity of cold water. This heavy water sinks and is foun
12、d in the deeper portions of oceans of the world.1. What is the main topic of the passage?A. Where do we get our table salt?B. Oceanic salinity in tropical regionsC. Three basic processes that alter oceanic salinityD. Variations of salinity in different parts of the ocean2. According to the author, t
13、he oceanic salinity is usually lower in _.A. tropical regionsB. coastal regionsC. places in which warm currents and cold currents meetD. the Antarctica3. All of the following are processes that decrease ocean salinity except _.A. precipitation B. runoff C. melting D. evaporation4. What does the word
14、 “subtraction in the fourth line of the first paragraph mean?A. reduction B. influx C. transformation D. freezing5. Which of the following is NOT a result of the formation of ice in oceans?A. The surrounding water sinks.B. The water becomes denser.C. Water salinity decreases.D. The surrounding water
15、 becomes colder.Questions 6 to 10 are based on the following passage: More than a century ago, the relationship between glacial ice and the amount of water in the ocean basins was first seen. When the great ice sheet covered vast land areas, the sea level was lowered because the normal return of wat
16、er from land to the ocean was reduced. As a result, the sea level rose as Ice Age glaciers melted allowing the melted waters to flow into the ocean. If all the glacial ice on the surface of the earth today should melt, the sea level might rise by more than 150 feet. Shoreline variations are also produced through elevation or depression of the land. During times of glacier for
