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Titlebook: Drainage Design; Peter Smart,J. Graham Herbertson Book 1992 Springer Science+Business Media New York 1992 attention.developing countries.f

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发表于 2025-3-21 19:27:01 | 显示全部楼层 |阅读模式
书目名称Drainage Design
编辑Peter Smart,J. Graham Herbertson
视频video
图书封面Titlebook: Drainage Design;  Peter Smart,J. Graham Herbertson Book 1992 Springer Science+Business Media New York 1992 attention.developing countries.f
描述This book provides a review of the principles and methods of drainage with an emphasis on design. The whole field of drainage is covered, and although the book concentrates mainly on the practice in North America, Europe and Britain, the practice in developing countries is also included. The book is directed primarily at the graduate engineer entering professional practice, but will also provide a useful reference for more senior engineers and for those in adjunct professions. Chapter 1 outlines the necessity for drainage on a large or small scale, for rural and urban areas. As the drainage engineer must decide how much unwanted water there will be and when it will occur, the chapter discusses climatic types, prediction of rainfall, evapotranspiration effects, return periods (of design storms and runoff events), river flow and flood prediction, and various sensing systems for providing short term predictions of rainfall, runoff, streamflow and flood warning. Chapter 2 gives a thorough review of the properties of soil in the context of drainage design. The extensive mathematical theories which relate to the crucial area of soil water movement are outlined and due attention is paid t
出版日期Book 1992
关键词attention; developing countries; flow; hydrology; water
版次1
doihttps://doi.org/10.1007/978-1-4757-5027-0
isbn_softcover978-1-4757-5029-4
isbn_ebook978-1-4757-5027-0
copyrightSpringer Science+Business Media New York 1992
The information of publication is updating

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书目名称Drainage Design被引频次




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书目名称Drainage Design读者反馈学科排名




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Surface hydrology,r small developing areas in urban centres and for larger areas of agricultural land to the successful containment of major rivers in flood. Consequently, the hydrological events producing superfluous water may be an intensive local storm, the accumulation of excess rainfall over a wet spell of a few
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Field drainage in temperate climates,urope, the equivalent region in eastern North America and the steppes and prairies of the continental interiors. The equivalent zone in the southern hemisphere is much more restricted in area but is equally productive. The soils of the prairies and steppes usually do not need drainage works because
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River systems,se catchments may be controlled by the conditions in the rivers; conversely, the rivers must themselves be designed and maintained to accept all the waters emptied into them both safely and economically. Thus, in drainage, river flows are important both directly and indirectly.
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Deep drainage,n terms of drainage and water supply than surface water, but it risks being overlooked even by the engineer because it is easy neither to see nor to quantify. In England and Wales slightly more than one-third of water for public supply derives from groundwater; in Scotland it is only 3%. In arid cli
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