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1、高等学校水利类统编教材水利专业外语迟道才 振民 主编上传人单位：华北水利水电学院水利系目 录Lesson 1 importance of water 水的重要性2Lesson 2 the Hydrologic Cycle 水循环4Lesson 3 hydrology 水文学6Lesson 4 underground water 地下水10Lesson 5 what causes flooding洪水是怎样形成的14Lesson 6 nature of water pollution 水污染的性质17Lesson 7 Planning for water resources developmen
2、t水资源开发规划20Lesson 8 reservoirs 水库24Lesson 9 Properties of concrete混凝土的特性28Lesson 10 basic concepts of reinforced concrete钢筋混凝土基本概念33Lesson 11 dams 坝36Lesson 12 embankment dams 土坝40Lesson 13 concrete gravity dam on rock foundations 岩基上的混凝土重力坝44Lesson 14 Arch dams 拱坝48Lesson 15 spillways溢洪道52Lesson 16
3、design forces 设计作用力56Lesson 17 Significance of infiltration and process of infiltration入渗重要性及过程60Lesson 18 evapotranspiration 腾发量63Lesson 19 irrigation methods 灌溉法66Lesson 20 irrigation canals灌溉渠道74Lesson 21 land drainage 耕地排水77Lesson 22 methods of applications of drip irrigation systems滴灌系统的应用法81Le
4、sson 23 hydraulic turbines水轮机84Lesson 24 hydro-electric power 水力发电88Lesson 25 differential leveling 水准测量（微差水准测量）94Lesson 26 construction and equipment施工和设备99Lesson 27 engineering economy in water resources planning水利规划中工程经济102Lesson 28 soil erosion and soil conservation 土壤侵蚀与土壤保持108Lesson 29 groundw
5、ater and climate change地下水与气候变化112Lesson 30 irrigation performance evaluation 灌溉运行评价115Lesson 31 bidding, bid opening and award of contract招标、开标和授予合同118Lesson 32 how to write a scientific paper如撰写科技论文121Lesson 1 importance of water 水的重要性Water is best known and most abundant of all chemical compounds
6、 occurring in relatively pure form on the earths surface. Oxygen, the most abundant chemical element, is present in combination with hydrogen to the extent of 89 percent in water. Water covers about three fourths of the earths surface and permeates cracks of much solid land. The Polar Regions (原文pol
7、ar regions) are overlaid with vast quantities of ice, and the atmosphere of the earth carries water vapor in quantities from 0.1 percent to 2 percent by weight. It has been estimated that the amount of water in the atmosphere above a square mile of land on a mild summer day is of the order of 50,000
8、 tons.在地球表面以相对纯的形式存在的一切化合物中，水是人们最熟悉的、最丰富的一种化合物。在水中，氧这种最丰富的化学元素与氢结合，其含量多达89%。水覆盖了地球表面的大约3/4的面积，并充满了陆地上的多裂缝。地球的两极被大量的冰所覆盖，同时大气也挟带有占其重量0.1%2%的水蒸气。据估计，在温暖的夏日，每平英里陆地上空大气中的水量约为5万吨。All life on earth depends upon water, the principal ingredient of living cells. The use of water by man, plants, and animals i
9、s universal. Without it there can be no life. Every living thing requires water. Man can go nearly two months without food, but can live only three or four days without water.地球上所有的生命都有赖于水而存在，水是活细胞的基本组分（要素）。人类、植物和动物都得用水。没有水就没有生命 。每一种生物都需要水。人可以接近两个月不吃食物而仍能活着，但不喝水则只能活三四天。In our homes, whether in the c
10、ity or in the country, water is essential for cleanliness and health. The average American family uses from 65,000 to 75,000 gallons of water per year for various household purposes.在我们的家庭中，无论是在城市还是农村，水对于卫生和健康来说都是必不可少的。美庭的年平均用水量达6.57.5万加仑。Water can be considered as the principal raw material and the
11、 lowest cost raw material from which most of our farm produces is made. It is essential for the growth of crops and animals and is a very important factor in the production of milk and eggs. Animals and poultry, if constantly supplied with running water, will produce more meat, more milk, and more e
12、ggs per pound of food and per hour of labor.水可以被认为是最基本的和最廉价的原料。我们的农产品，大部分都是由它构成的。水是农作物和动物生长的要素，也是奶类和蛋类生产的一个很重要的因素。动物和家禽，如果用流动的水来喂养，那么每磅饲料和每个劳动小时会生产出更多的肉、奶和蛋。For example, apples are 87% water. The trees on which they grow must have watered many times the weight of the fruit. Potatoes are 75% water. T
13、o grow an acre of potatoes tons of water is required. Fish are 80% water. They not only consume water but also must have large volumes of water in which to live. Milk is 88% water. To produce one quart of milk a cow requires from 3.5 to 5.5 quarts of water. Beef is 77% water. To produce a pound of b
14、eef an animal must drink many times that much water. If there is a shortage of water, there will be a decline in farm production, just as a shortage of steel will cause a decrease in the production of automobiles.例如，苹果含87%的水分，苹果树就必须吸收比苹果多多倍的水分；土豆含75%的水分，那么种植每英亩土豆就需要若干吨水；牛奶含水量为88%，为了生产每夸脱牛奶，母牛需要3.55.
15、5 夸脱的水；牛肉含77%的水，为生产1磅牛肉牛必须饮用多磅水。如果缺水，就会使农产品减产，就像缺乏钢会引起汽车产量下降一样。In addition to the direct use of water in our homes and on the farm, there are many indirect ways in which water affects our lives. In manufacturing, generation of electric power, transportation, recreation, and in many other ways, water
16、 plays a very important role.水除了直接为我们的家庭和农场利用外，它还以多间接的式对我们的生活产生影响。在制造、发电、运输、娱乐以及其他多行业，水都起着很重要的作用。Our use of water is increasing rapidly with our growing population. Already there are acute shortages of both surface and underground waters in many locations. Careless pollution and contamination of our
17、 streams, lakes, and underground sources has greatly impaired the quality of the water which we do have available. It is therefore of utmost importance for our future that good conservation and sanitary measures be practiced by everyone.我们对水的利用随人口的增长而迅速增加。在多地，无论地面水或地下水都已经重短缺了。由于任意污染河流、湖泊和地下水源，已经大损害了
18、人们能够利用的水的水质。因此，人人有责对水采取保护措施和卫生措施，这对于我们人类的未来是极端重要的。Lesson 2 the Hydrologic Cycle 水循环In nature, water is constantly changing from one state to another. The heat of the sun evaporates water from land and water surfaces, this water vapor (a gas), being lighter than air, rises until it reaches the cold u
19、pper air where it condenses into clouds. Clouds drift around according to the direction of the wind until they strike a colder atmosphere. At this point the water further condenses and falls to the earth as rain, sleet, or snow, thus completing the hydrologic cycle.在自然界中，水总是不断地从一种状态改变成另一种状态。太阳热使陆地和水
20、面上的水蒸气。这些水蒸气（一种气体）由于比空气轻，会上升直至达到高空冷气层，并在那里凝结成云。云层随风飘荡，直至遇到更冷的大气层为止。此时水便进一步冷凝，并以雨、雹或雪的形式落到地面。这样便完成了水的循环。The complete hydrologic cycle, however, is much more complex. The atmosphere gains water vapor by evaporation not only from the oceans but also from lakes, rivers, and other water bodies, and from
21、moist ground surfaces. Water vapor is also gained by sublimation from snowfields and by transpiration from vegetation and trees.然而，完整的水循环要复杂得多。由于蒸发作用，大气不仅从海洋而且从湖泊、河流和其他水体，以及从潮湿的地表面获得水蒸气。也可从雪地中雪的升华和从植物与树木的蒸腾获得水蒸气。Water precipitation may follow various routes. Much of the precipitation from the atmosp
22、here falls directly on the oceans. Of the water that does fall over land areas, some is caught by vegetation or evaporates before reaching the ground, some is locked up in snowfields or ice-fields for periods ranging from a season to many thousands of years, and some is retarded by storage in reserv
23、oirs, in the ground, in chemical compounds, and in vegetation and animal life.降水可以有各种不同的途径。大部分降水都直接落到海洋。落在陆地区域的水，有些被植物所摄取，或降至地面之前就蒸发了；有些被封冻在雪原或冰川中达一个季度乃至成千上万年；有些则因储存在水库、土壤、化合物以及动植物体而滞留下来。The water that falls on land areas may return immediately to the sea as runoff in streams and rivers or when snow
24、 melts in warmer seasons. When the water does not run off immediately it percolates into the soil. Some of this groundwater is taken up by the roots of vegetation and some of it flows through the subsoil into rivers, lakes, and oceans.降到陆地区域的水可能作为溪流与江河的径流，或在温暖季节融化的雪水直接回到海洋。当降水不立即流走时，它会渗入土壤。这些地下水中有一些
25、被植物的根吸收，有一些则通过下层土壤流入河流、湖泊和海洋。Because water is absolutely necessary for sustaining life and is of great importance in industry men have tried in many ways to control the hydrologic cycle to their own advantage. An obvious example is the storage of water behind dams in reservoirs, in climates where th
26、ere are excesses and deficits of precipitation (with respect to water needs) at different times in the year. Another method is the attempt to increase or decrease natural precipitation by injecting particles of dry ice or silver iodide into clouds. This kind of weather modification has had limited s
27、uccess thus far, but many meteorologists believe that a significant control of precipitation can be achieved in the future.因为水对于维持生命来说绝对必要，在工业上也很重要，所以人们为了自身的利益试图以各种式来控制水的循环。一个明显的例子就是在一年中不同的时间根据当地降水的多寡（按对水的需要来说）将水储存在水库中。另一种法是试图将干冰或碘化银微粒射入云层来增多或减少天然降雨量。虽然这种改造气候（人工影响天气）的法迄今只取得了有限的成功，但多气象学家都认为，有效地控制降水在将
28、来是可以做到的。Other attempts to influence the hydrologic cycle include the contour plowing of sloping farmlands to slow down runoff and permit more water to percolate into the ground, the construction of dikes to prevent floods and so on. The reuse of water before it returns to the sea is another common p
29、ractice. Various water supply systems that obtain their water from rivers may recycle it several times (with purification) before it finally reaches the rivers mouth.其他一些影响水循环的努力包括沿等高线耕作梯田，以使径流减速，让更多的水渗入地下；建筑堤坝以防洪水等。在水回归大海之前将它重复使用，也是一种常用的法。自河道取水的各种供水系统可将水在最终到达河口之前，经过净化，可重复使用多次。Men also attempt to pr
30、edict the effects of events in the course of the hydrologic cycle. Thus, the meteorologist forecasts the amount and intensity of precipitation in a watershed, and the hydrologist forecasts the volume of runoff.人们还试图预测水循环过程中一些事件的结果。例如，气象学家预报一个流域的降雨量和降雨强度；水文学家预报径流量等。Lesson 3 hydrology 水文学1 historyThe
31、first hydraulic project has been lost in the mists of prehistory. Perhaps some prehistoric man found that pile of rocks across a stream would raise the water level sufficiently to overflow the land that was the source of his wild food plants and water them during a drought. Whatever the early histor
32、y of hydraulics, abundant evidence exists to show that the builders understood little hydrology. Early Greek and Roman writings indicated that these people could accept the oceans as the ultimate source of all water but could not visualize precipitation equaling or exceeding stream-flow. Typical of
33、the ideas of the time was a view that seawater moved underground to the base of the mountains. There a natural still desalted water, and the vapor rose through conduits to the mountain tops, where it condensed and escaped at the source springs of the streams. Marcus Vitruvius Pollio (ca. 100 B. C.)
34、seems to have been one of the first to recognize the role of precipitation as we accept it today.最早的水利工程在有史以前就已经销声匿迹了。也史前的人曾发现横贯河流的一堆头就能提高水位，足以淹没作为生长野生食用植物源泉的土地，而这样在干旱季节就能给植物浇水。不论水力学的早期如，充分的的迹象表明，建造者们还不懂多少水文学知识。早期的希腊和罗马文献说明这些人承认海洋是一切水的主要源泉，但是不能想象降雨量会等于或超过河道径流量。当时典型的想法是海水从地下流到山脉底部，那儿有一个天然蒸馏器除去水中的盐分，水
35、汽通过管道上升到山顶，在那里凝结，并从河流的源头流走。M.V.波利欧（大约公元前100年）看来就是像我们今天这样认识降水作用最早的人。Leonardo da Vinci (1452-1519) was the next to suggest a modern view of the hydrologic cycle, but it remained for Pierre Perrault (1608-1680) to compare measured rainfall with the estimated flow of the Seine River to show that the str
36、eam-flow was about one-sixth of the precipitation. The English astronomer Halley (1656-1742) measured evaporation from a small pan and estimated evaporation from the Mediterranean Sea from these data. As late as 1921, however, some people still questioned the concept of the hydrologic cycle.达芬奇（1452
37、-1519）是提出水文循环现代观点的第二个人，但一直到P.贝罗特（1608-1680）才把观测的雨量与估算的塞纳河的径流量进行比较，说明河川径流量约为降雨量的1/6.英国天文家哈罗（哈雷）从一个小盘子中测得的蒸发量，并且用这一资料估算地中海的蒸发量。然而直到1921年，有一些人仍然对水文循环的概念表示怀疑。Precipitation was measured in India as early as the fourth century B.C., but satisfactory methods for measuring stream-flow were a much later deve
38、lopment. Frontinus, water commissioner of Rome in A.D. 97, based estimates of flow on cross-sectional area alone without regard to velocity. In the United States, organized measurement of precipitation started under the Surgeon General of the Army in 1819, was transferred to the Signal Corps in 1870
39、, and finally, in 1891, to a newly organized U.S. Weather Bureau, renamed the National Weather Service in 1970.Scattered stream-flow measurements were made on the Mississippi River as early as 1848, but a systematic program was not started until 1888, when the U.S. Geological Survey undertook this w
40、ork. It is not surprising, therefore, that little quantitative work in hydrology was done before the early years of the twentieth century, when men such as Hortan, Mead, and Sherman began to explore the field. The great expansion of activity in flood control, irrigation, soil conservation, and relat
41、ed fields which began about 1930 gave the first real impetus to organized research in hydrology, as need for more precise design data became evident. Most of todays concepts of hydrology date from 1930. 印度早在公元前4世纪就测量降水量了，但是令人满意的测量河道流量的法很迟才得到发展。公元97年，罗马水利专员福朗堤努斯只按横断面面积估算流量，而不考虑流速。在美国，有组织地测量降水量是1819年在
42、陆军军医总监领导下开始的，1870年移交给通信兵团，最后，在1891你那移交给新改组的美国气象局，该局于1970年改名为气象局。早在1848年密西西比河上就进行分散的河道流量测量了，但是，直到1888年美国地质调查局承担这项工作时，才开始实施系统的观测计划。霍德、米德和尔曼等人在20世纪早期刚开始对这一领域进行探索，因此，在这时期之前，在水文面没有进行什么定量工作是不足为奇的。大约从1930年起，由于在防洪、灌溉、土地改良和有关领域中开展了大量活动，第一次为有组织地研究水文学提供了真正的动力，因为需要更精确的设计资料，这已是十分明显的事了。大多数现代水文学的概念从1930年就开始有了。2 hy
43、drology in engineering水文学在工程中的应用Hydrology is used in engineering mainly in connection with the design and operation of hydraulic structures. What flood flows can be expected at a spillway or highway culvert or in a city drainage system ? What reservoir capacity is required to assure adequate water f
44、or irrigation or municipal water supply during droughts? What effects will reservoirs, levees, and other control works exert on flood flows in a stream? These are typical of questions the hydrologist is expected to answer.在工程上，水文学主要用于水工建筑物的设计和运行，溢洪道、公路涵洞、或者城市排水系统会期望有什么样的洪水流量？需要多大的水库库容才能保证干旱季节里有足够的灌溉
45、水量或城市供水呢？水库、堤坝或其他控制工程对河流洪水流量有什么影响？这些典型的问题等待水文学家去解答。Large organization such as federal and state water agencies can maintain staffs of hydrologic specialists to analyze their problems, but smaller offices often have insufficient hydrologic work for full-time specialists. Hence, many civil engineers a
46、re called upon for occasional hydrologic studies. It is probable that these civil engineers deal with a larger number of projects and greater annual dollar volume than the specialists do. In any event, it seems that knowledge of the fundamentals of hydrology is an essential part of the civil enginee
47、rs training.像联邦和州辖水利机构这样的大型组织，拥有一批水文专家来分析他们的问题，但较小的单位往往没有足够的水文工作给专职水文专家做。因此，多土木工程师们应邀进行临时的水文研究。这些土木工程师处理的工程和年费用可能比水文专家还多。无论如，水文学的基础知识看来是培训土木工程师所必不可少的一部分。3 subject matter of hydrology水文学研究的主要容Hydrology deals with many topics. The subject matter as presented in this book can be broadly classified into
48、 two phases: data collection and methods of analysis. Chapter 2 to 6 deals with the basic data of hydrology. Adequate basic data are essential to any science, and hydrology is no exception. In fact, the complex features of the natural processes involved in hydrologic phenomena make it difficult to t
49、reat many hydrologic processes by rigorous deductive reasoning. One can not always start with a basic physical law and from this determine the hydrologic result to be expected. Rather, it is necessary to start with a mass of observed facts, analyze these facts, and from this analysis to establish the systematic pattern that governs these events. Thus, without adequat
