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                    180  Chapter 5  Water Hydraulics, Transmission, and Appurtenances




































                                                                                       Figure 5.10 Concrete Water Pipe.
                                                                                       (Source: Wikipedia, http://upload.
                                                                                       wikimedia.org/wikipedia/commons/
                                                                                       2/2e/Concrete_water_pipe.jpg)




                                         number of offsets from the tangent. Sharper curves can be formed by shorter or shortened
                                         pipes. The smaller the pipe, the sharper can be the deflection. Welded pipelines less than
                                         15 in. (400 mm) in diameter are sufficiently flexible to be bent in the field. The ends of
                                         larger steel pipe must be cut at an angle that depends on the type of transverse joint, the
                                         thickness of the steel plate, and the size of the pipe.
                                             For sharp curves, transitions, and branches, special fittings are often built up or manu-
                                         factured of the same materials as the main conduit.

                    5.7.3  Depth of Cover

                                         Conduits that follow the surface of the ground are generally laid below the frost line, al-
                                         though the thermal capacity and latent heat of water are so great that there is little danger
                                         of freezing as long as the water remains in motion. To reduce the external load on large
                                         conduits, only the lower half may be laid below frost. Along the 42nd parallel of latitude,
                                         which describes the southern boundaries of Massachusetts, upper New York, and
                                         Michigan in the United States, frost seldom penetrates more than 5 ft (1.5 m) beneath the
                                         surface; along the 45th parallel the depth increases to 7 ft (2 m). The following equation
                                         approximates Shannon’s (1945) observations of frost depth:

                                                           d   1.65F 0.468   (U.S. Customary Units)         (5.41a)
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