Download Applied Hydrogeology (4th Edition) by C. W. Fetter PDF

By C. W. Fetter

Book Details:

ISBN: 0130882399
Publisher: Prentice Hall
Publication Date: 2000-11-26
Number of Pages: 598
Website: Amazon, LibraryThing, Google Books, Goodreads

Synopsis from Amazon:

This most sensible promoting ebook, Applied Hydrogeology provides readers a balanced exam of all elements of hydrogeology. It textual content stresses the applying of arithmetic to challenge fixing instead of derivation of thought. It offers a stability among actual and chemical hydrogeology. a variety of case reports domesticate reader figuring out of the prevalence and move of flooring water in a number of geologic settings. This beneficial reference comprises 5 new case histories: The Dakota Aquifer, Fractures Sedimentary Rocks-Newark basin, Faults as Aquifer limitations, wilderness Hydrology-Azraq basin, Jordan. makes use of the net to procure hydrogeologic info and knowledge. comprises well-developed case reports in many of the chapters. comprises tables overlaying a number of capabilities, unit conversions, and extra facts for fixing good hydraulics, water chemistry, and contaminant shipping difficulties. For readers drawn to complicated hydrology, groundwater hydrology, hydrogeology, and civil engineering.

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Extra resources for Applied Hydrogeology (4th Edition)

Sample text

63 cm has four significant digits. 5 cm, and the m easurement has been made to two significant digits. W hen two or more numbers are multiplied (or divided), their product (or quotient) should have the sam e number of significant digits as the m ultiplier (or divi­ sor) with the least number. 97363 cm2. We use the num ­ ber of significant digits of the least precise measurement, in this case four. 0, not 251, to show the num ber of significant digits. W hen m easurements are added (or subtracted), the sum (or difference) should not have any significant digits to the right of the last significant digit of any of the addends (or subtrahends).

As condensation is the reverse of evaporation, the process of cor densation releases about 590 cal of heat to the surroundings per gram o water, termed the latent heat of condensation. 38 -1 0 -5 0 5 10 15 20 25 30 Source: Handbook of Chemistry and Physics (Cleveland, Ohio: CRC Publishing Company, 1976). place from free-water surfaces— lakes, reservoirs, puddles, dew droplets, for example. The rate depends on factors such as the water tem perature and the tem perature and absolute humidity o f the layer of air ju st above the free-water surface.

Should there be doe as to w hich stations to connect, lines should be between the closest stations. 6C). It is best to start w ith a centrally located station and then expand t polygonal network outward.

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