Hydraulic Design of Large-Diameter Pipes

Total Page:16

File Type:pdf, Size:1020Kb

Hydraulic Design of Large-Diameter Pipes Hydraulic Design of Large-Diameter Pipes Fabia´n A. Bombardelli1 and Marcelo H. Garcı´a, M.ASCE2 Abstract: The Hazen–Williams formula is frequently used for the design of large-diameter pipes, without regard for its limited range of applicability. This practice can have very detrimental effects on pipe design, and could potentially lead to litigation. Available evidence shows that the application of the formula is accurate only if the operation of the pipe is located within the transition or smooth, turbulent-flow regimes. Most working ranges for water-supply pipes usually fall outside such conditions. This paper presents an analysis which highlights the potential implications of current use of the Hazen–Williams formula for the design of large-diameter pipe systems. DOI: 10.1061/͑ASCE͒0733-9429͑2003͒129:11͑839͒ CE Database subject headings: Pipe flow; Resistance coefficients; Roughness; Pipe design. Introduction with the help of the Hazen–Williams equation. After only 5 years in service, it was found that the network was inadequate in deliv- Worldwide population growth has brought along a clear need to ering the amount of water it had been designed for. The authors increase the capacity of water-supply and sewerage systems. were asked to analyze why the recently built pipeline could not Pipes having large diameters are commonly found in modern meet that water demand. The analysis consisted of: ͑1͒ reviewing water-distribution networks located in major metropolitan areas. the literature concerning issues such as range of validity and ac- Consequently, the misuse of any design formulation to estimate curacy of the Hazen–Williams formula; ͑2͒ revisiting the original flow resistance in large pipes can lead to serious practical draw- dataset employed by Hazen and Williams to develop the equation; backs. More specifically, those systems might not be able to meet and ͑3͒ using pressure-head and velocity measurements taken in- the demand they were designed for, thus reducing their useful life. dependently by two consulting engineering firms to estimate flow The Hazen–Williams formula, which dates back to the early resistance ͑i.e., resistance coefficients͒ in the pipeline system in 1900s, has traditionally been regarded as a general, simple tool to ͑ ͒ question. compute head losses in pipes carrying water Chen 1992 . The In what follows, the analysis inspired by the case study is equation includes a conveyance coefficient usually assumed to be presented, followed by a discussion of the results, and the con- constant for a certain pipe-wall material, regardless of the pipe clusions. size or the flow range. This fact can result in deficient designs under a wide set of conditions. Unfortunately, the formula is cur- rently being used outside of its actual range of validity throughout Preliminary Theoretical Considerations the United States and worldwide. Furthermore, in many cities and and Analysis some counties throughout the States, any computation dealing with water flow in pipes is simply rejected if the Hazen–Williams There are a number of equations commonly used to estimate flow formula is not used, without any regard for its intrinsic limitations resistance in channels and pipes. They are: ͑Diskin 1960; Jain et al. 1978; Liou 1998; Christensen 2000; • Manning equation Locher 2000; Swamee 2000͒. 2/3 1/2 KnR S In this paper, an analysis illustrating the implications of cur- Uϭ (1) rent use of available resistance formulations is presented. The n ͑ ͒ case study that motivated the analysis refers to a large water- • Dimensionally homogeneous Manning formula Yen 1992b supply system for a major metropolitan area, originally designed g1/2R2/3S1/2 Uϭ (2) ng 1 Research Assistant, Ven Te Chow Hydrosystems Laboratory, Dept. of • Chezy equation Civil and Environmental Engineering, Univ. of Illinois at Urbana- Champaign, 205 North Mathews Ave., Urbana, IL 61801. On leave from UϭCR1/2S1/2 (3) Instituto Nacional del Agua ͑INA͒, Argentina. E-mail: • Darcy–Weisbach equation [email protected] 1/2 1/2 2Chester and Helen Siess Professor, and Director, Ven Te Chow Hy- 2g h f Uϭͩ ͪ D1/2ͩ ͪ (4) drosystems Laboratory, Dept. of Civil and Environmental Engineering, f L Univ. of Illinois at Urbana-Champaign, 205 North Mathews Ave., Ur- • Hazen–Williams equation bana, IL 61801. E-mail: [email protected] ϭ 0.63 0.54 Note. Discussion open until April 1, 2004. Separate discussions must U KHWCHWR S (5) be submitted for individual papers. To extend the closing date by one month, a written request must be filed with the ASCE Managing Editor. where U indicates the cross-sectional averaged velocity; ϭ ϭ ϭ The manuscript for this paper was submitted for review and possible R hydraulic radius; S slope of the energy grade line; D pipe ϭ ϭ publication on July 30, 2001; approved on May 14, 2003. This paper is diameter; L length of the reach of the pipe; h f energy loss in part of the Journal of Hydraulic Engineering, Vol. 129, No. 11, Novem- the pipe reach ͑expressed as per unit weight of fluid͒; ϭ ϭ ber 1, 2003. ©ASCE, ISSN 0733-9429/2003/11-839–846/$18.00. g acceleration of gravity; Kn and KHW unit conversion factors; JOURNAL OF HYDRAULIC ENGINEERING © ASCE / NOVEMBER 2003 / 839 Fig. 1. Predictions obtained with the Hazen–Williams formula plotted in the Moody diagram ͓adapted from Diskin ͑1960͔͒. Operational points of the pipes pertaining to the case study ͑measurements by the two consulting engineering firms͒. ͑ ͒ and n, ng , C, f, and CHW refer to the resistance/conveyance co- and slope. Vennard 1958 highlighted that one of the disadvan- 1/2 ͑ ͒ efficients. Kn is equal to 1 m /s International System, SI or to tages of the equation was related to ‘‘the impossibility of applying 1.486 ft1/3 m1/6/s if English units are employed ͑Yen 1992b͒. For it to all fluids under all conditions.’’ Nevertheless, Diskin ͑1960͒ KHW , values of 0.849 and 1.318 are used in each of the above was apparently the first to strongly acknowledge the limitations systems, respectively ͑Jeppson 1977͒. Hazen and Williams evalu- associated with the formula and to undertake a rather careful ϭ ated the factor 1.318 as a means of keeping CHW C, for a slope analysis of its range of validity. Diskin first rearranged the Ϫ3 ͑ ͒͑ of 10 and a hydraulic radius of 0.305 m 1ft Williams and Hazen–Williams equation in the shape of the Darcy–Weisbach ͒ Hazen 1920 . A considerable number of papers has been devoted formula, in a similar way as previously done by Vennard ͑1958͒. to the determination of values for CHW pertaining to pipes made Thus he was able to obtain a power relation between f, C , D, ͑ HW of different materials, including polyethylene pipes Moghazi and R ͑the pipe Reynolds number, RϭUD/␯; ␯ is the water ͒ 1998 . Also, several papers have addressed the optimization of the kinematic viscosity͒, that reads for D in meters design of pipe networks, either using the Hazen–Williams for- mula ͓e.g., Datta and Sridharan ͑1994͒; and Niranjan Reddy et al. 1.852 0.2004͑100/CHW͒ 1 ͑1996͔͒, or modified formulations ͓Elimam et al. ͑1989͒; and f ϭ (6) 0.019 0.148 Charalambous and Elimam ͑1990͔͒. D R It has been well known since the beginning of the last century In Eq. ͑6͒, the value of water viscosity at 15°C was employed. ͑King et al. 1948͒, that the Darcy–Weisbach and Manning formu- las can be both used for computations in either open-channel or This expression demonstrates that CHW is not a constant for a pipe, fully rough turbulent flow. Thus it is possible to determine certain wall condition, as is interpreted in numerous engineering ͑ ͒ backwater profiles in open channels using the Darcy–Weisbach manuals Liou 1998 . Instead, it depends on the flow condition, equation or, conversely, to compute energy losses in pipes em- the pipe diameter and relative roughness, and the water tempera- ␯ ploying Manning’s equation, provided the convenient equivalence ture, through the kinematic viscosity, . Dϭ4R is considered, and reliable estimates for the resistance Based on this result, Diskin plotted Eq. ͑6͒ for different values ͑ ͒ coefficients are at hand ͑Yen 1992a, 2002͒. The Chezy equation of CHW and D into the Moody diagram Fig. 1 . Using this plot, can also be employed in either case. However, the Hazen– he was able to conclude that the formula is applicable ‘‘in part of Williams formula has quite a restricted range of application that the transition zone.’’ Diskin determined the ranges of Reynolds limits its use. numbers for which the original lines of the Moody diagram are In their classic monograph, Williams and Hazen ͑1920͒ stated parallel to the lines representing the predictions of the Hazen– that the exponents of their equation depended on pipe diameter Williams equation. Those limiting Reynolds numbers increase 840 / JOURNAL OF HYDRAULIC ENGINEERING © ASCE / NOVEMBER 2003 Table 1. Measurements Performed by Two Engineering Firms ͑Values Computed by Authors͒ ͑a͒ First line corresponds to the main pipe; second line pertains to another pipe in the system with another discharge. Pipe Velocity Losses Reach Slope diameter Area measured measured length of energy ng C ͑ ͒ ͑ 2͒ ͑ ͒ ͑ ͒ ͑ ͒ ͑ 1/6͒ ͑ 1/2 ͒ m m m/s m m line CHW fnm C f m /s R 2.286 4.104 1.076 9.604 13,692.53 0.00070 91 0.027 0.017 0.053 0.0034 54 2,450,000 1.829 2.627 0.960 1.884 3,213.506 0.00059 103 0.023 0.015 0.047 0.0029 59 1,750,000 ͑b͒ All measurements pertain to the main pipes.
Recommended publications
  • Properties and Definitions
    Properties and Definitions Useful constants, properties, and conversions 2 2 gc = 32.2 ft/sec [lbm-ft/lbf-sec ] 3 ρwater = 1.96 slugs/ft 3 γwater = 62.4 lb/ft 1 ft3/sec = 449 gpm 1 mgd = 1.547 ft3/sec 1 foot of water = 0.433 psi 1 psi = 2.31 ft of water Definitions discharge: flow rate, usually in ft3/sec or gpm Properties Density Density (ρ) is mass per unit volume (slugs/ft3) Specific Weight (aka Unit Weight) Specific Weight (γ) is weight per unit volume (lb/ft3) = ρg Specific Gravity Specific Gravity (S) is the ratio of the weight (or mass) or a substance to the weight (or mass) of water. where the subscript "s" denotes of a given substance and the subscript "w" denotes of water. Given S of a substance, you can easily calculate ρ and γ using the equations Specific Volume Specific Volume is the volume per unit mass (usually in ft3/lbm) Viscosity Viscosity (υ) is a measure of a fluid's ability to resist shearing force (usually in 2 lbf·sec/ft ) υ is a proportionality constant and is also known as absolute viscosity or dynamic viscosity. Viscosity is often given in the SI unit of Poise. To convert to English units use the relationship Kinematic Viscosity where γ = kinematic viscosity (ft2/s) 2 υ = dynamic viscosity (lbf·sec/ft ) ρ = mass density (slugs/ft3) Note: See CERM Appendix 14.A (page A-13) for a listing of water properties at various temperatures. Absolute and Gauge Pressure Absolute Pressure (psia) = Atmospheric Pressure + Gauge Pressure (psig) Atmospheric Pressure changes with weather conditions and altitude though is usually assumed to be 14.7 psi at sea level.
    [Show full text]
  • Hydropower Engineering Ii Lecture Note Compiled By
    Arbaminch University, Department of Hydraulic Eng’g HYDROPOWER ENGINEERING II LECTURE NOTE COMPILED BY: YONAS GEBRETSADIK LECTURER IN HYDRAULIC ENGINEERING DEPARTMENT OF HYDRAULIC ENGINEERING ARBA MINCH WATER TECHNOLOGY INSTITUTE ARBA MINCH UNIVERSITY JANUARY 2011 Hydropower Engineering-II Lecture Note/2010/2011 1 Arbaminch University, Department of Hydraulic Eng’g TABLE OF CONTENTS 1. HYDRAULIC TURBINES ............................................................................................................................. 5 1.1 GENERAL ............................................................................................................................................. 5 1.2 CLASSIFICATION .................................................................................................................................. 5 1.3 CHARACTERISTICS OF TURBINES ......................................................................................................... 6 1.4 PROCEDURE IN PRELIMINARY SELECTION OF TURBINES ...................................................................... 7 1.5 TURBINE SCROLL CASE ....................................................................................................................... 9 1.6 DRAFT TUBES .................................................................................................................................... 10 1.7 CAVITATION IN TURBINE & TURBINE SETTING ................................................................................. 11 1.8 GENERATORS AND TURBINE
    [Show full text]
  • Innovative and Low Cost Technologies Utilized in Sewerage
    ENVIRONMENTAL HEALTH PROGRAM INNOVATIVE AND LOW COST TECHNOLOGIES UTILIZED IN SEWERAGE TECHNICAL SERIES No. 29 PAN AMERICAN H EAU H ORGANIZATION Pan American Sanitary Bureau, Regional Office of the WORLD HhALTH ORGANIZATION ENVIRONMENTAL HEALTH PROGRAM u, •:'< i .:••;: .•: a. ! 4 INNOVATIVE AND LOW COST TECHNOLOGIES UTILIZED IN SEWERAGE AUTHOR José M. Azevedo Netto EDITED Raymond Reid WASHINGTON, D.C., MARCH 1992 PROLOGUE This publication is the product of the last contract of the late Jose Martiniano de Azevedo Netto with the Pan American Health Organization and is a significant example of a relationship of more than 40 years duration —a relationship that was characterized always with a touch of daring, and clever, innovative approaches to the solution of environmental health problems and risks. The contribution of Azevedo Netto to sanitary engineering goes far beyond his countless books, papers and articles. Thousands of public health and sanitary engineering professionals in Latin America have been affected and influenced by his inspiring and dedicated teachings and instruction. Azevedo Netto was born in Brazil in 1918, graduated as a civil engineer from the University of Sao Paulo, and earned his masters degree in sanitary engineering from Harvard University and his doctorate in public health from the University of Sao Paulo. The professional life of Professor Azevedo Netto, as he liked to be called, took him to all continents as a teacher and as technical advisor to governments and institutions such as Pan American Health Organization, the World Bank, Inter- American Development Bank and others. A founding member of the Inter-American and the Brazilian Associations of Sanitary and Environmental Engineering, Azevedo Netto raised the consciousness of the importance of sanitary engineering to improvement of peoples' health and quality of life.
    [Show full text]
  • Oft/Milar/ON in SEWER. DESIGN Flold Cjjflr.T
    · COST EFFECTIVENESS IN SEWER DESIGN by Gary J. Diorio, P.E. SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS for the Degree of Master of Science in the Civil Engineering Program ~{).~. ADVISER DATE DEAN of the Graduate School DATE Youngstown State University December, 1986 COST EFFECTIVENESS IN SEWER DESIGN © 1986 GARY J. DIORIO, P.E. All Rights Reserved i ABSTRACT COST EFFECTIVENESS IN SEWER DESIGN GARY J. DIORIO, P.E. MASTER OF SCIENCE YOUNGSTOWN STATE UNIVERSITY Probably the most important challenge facing an engineer today is to ensure that his design is competitive in terms of costs. Besides being technically sound, the designer's objectives are to provide a cost effective solution. This thesis presents a computer program to be used as a guide for the design of storm sewers to ensure a cost effective solution. The computer program is compiled to generate overland flows to inlets by use of a combination of the Rational Method and the Soil Conservation Method. The cost effective solution is found by applying the cost function according to the constraints set forth in the program. The program ~ constraints involve minimum slopes to ensure proper velocities in the pipe, proper pipe sizes to ensure a technically sound design, and to provide a minimum depth of sewer throughout the entire length. A case study is also included and analyzed to provide reliability data for the computer program. The design process, including cost computation, is laborious to the extent that it discourages the effort to explore all situations to arrive at a cost effective design. The purpose of this thesis is to provide the designer with the following: ii 1.
    [Show full text]
  • Guide for Selecting Manning's Roughness Coefficients
    GUIDE FOR SELECTING MANNING’S ROUGHNESS Turner-Fairbank Highway COEFFICIENTS FOR NATURAL CHANNELS Research Center 6300 Georgetown Pike AND FLOOD PLAINS McLean, Virginia 22101 Report No. 3 t u FHWA-TS-84-204 U.S. Department of Transportation Final Report April 1984 -1 HishrwaV AdministrWon Archived ‘This document is available to the U.S. public through the National Technical Information Service, Springfield, Virginia 2216 FOREWORD This Technology Sharing Report provides procedures for determining Manning's roughness coefficient for densely vegetated flood plains. The guidelines should be of interest to hydraulic and bridge engineers. Environmental specialists concerned with flood plains and wetlands may also find this report useful. The report was prepared by the United States Geological Survey, Water Resources Division, with technical guidance from the FHWA Office of Engineering and Highway Operations Research and Development. Sufficient copies of the publication are being distributed to provide a minimum of one copy to each FHWA region office, division office, and to each State highway agency. Additional copies of the report can be obtained from the National Technical Information Service, Springfield, Virginia 22161. DirectdrJ Office of / Director, Office of Engineering and Highway Implementation Operations R&D NOTICE This document is disseminated under the sponsorship of the Department of Transportation in the interest of information exchange. The United States Government assumes no liability for its contents or use thereof. The contents of this report reflect the views of the contractor, who is responsible for the accuracy of the data presented herein. The contents do not necessarily reflect the official views or policy of the Department of Transportation.
    [Show full text]
  • Calculating Resistance to Flow in Open Channels 1. Introduction
    Alternative Hydraulics Paper 2, 5 April 2010 Calculating resistance to flow in open channels John D. Fenton http://johndfenton.com/Alternative-Hydraulics.html [email protected] Abstract The Darcy-Weisbach formulation of flow resistance has advantages over the Gauckler-Manning- Strickler form. It is more fundamental, and research results for it should be able to be used in practice. A formula for the dimensionless resistance coefficient was presented by Yen (1991, equa- tion 30), which bridges between the limits of smooth flow and fully rough flow, to give a general formula for calculating resistance as a function of relative roughness and Reynolds number, appli- cable for a channel Reynolds number R>30 000 and relative roughness ε<0.05. In this paper, the author shows how a closely similar formula was obtained which is in terms of natural loga- rithms, which are simpler if further operations such as differentiation have to be performed. The formulae are shown to agree with predictions from the Gauckler-Manning-Strickler form, and with a modified form for open channels, have advantages that the equations are simpler and terms are more physically-obvious, as well as using dimensionless coefficients with a greater connectedness to other fluid mechanics studies. 1. Introduction The ASCE Task Force on Friction Factors in Open Channels (1963) expressed its belief in the general utility of using the Darcy-Weisbach formulation for resistance to flow in open channels, noting that it was more fundamental, and was based on more fundamental research. The
    [Show full text]
  • PDF, Bottom Friction Models for Shallow Water Equations: Manning's
    Journal of Physics: Conference Series PAPER • OPEN ACCESS Related content - Model reduction of unstable systems using Bottom friction models for shallow water balanced truncation method and its application to shallow water equations Kiki Mustaqim, Didik Khusnul Arif, Erna equations: Manning’s roughness coefficient and Apriliani et al. small-scale bottom heterogeneity - An averaging method for the weakly unstable shallow water equations in a flat inclined channel To cite this article: Tatyana Dyakonova and Alexander Khoperskov 2018 J. Phys.: Conf. Ser. 973 Richard Spindler 012032 - Computational multicore on two-layer 1D shallow water equations for erodible dambreak C A Simanjuntak, B A R H Bagustara and P H Gunawan View the article online for updates and enhancements. Recent citations - Numerical hydrodynamic model of the Lower Volga A Yu Klikunova and A V Khoperskov - Flow resistance in a variable cross section channel within the numerical model of shallow water T Dyakonova and A Khoperskov This content was downloaded from IP address 170.106.35.234 on 23/09/2021 at 14:15 AMSCM IOP Publishing IOP Conf. Series: Journal of Physics: Conf. Series1234567890 973 (2018) ‘’“” 012032 doi :10.1088/1742-6596/973/1/012032 Bottom friction models for shallow water equations: Manning's roughness coefficient and small-scale bottom heterogeneity Tatyana Dyakonova, Alexander Khoperskov Volgograd State University, Department of Information Systems and Computer Simulation, Volgograd, 400062, Russia E-mail: [email protected] Abstract. The correct description of the surface water dynamics in the model of shallow water requires accounting for friction. To simulate a channel flow in the Chezy model the constant Manning roughness coefficient is frequently used.
    [Show full text]
  • Sediment Transport in Open Channel Flows
    Introduction to Sediment Transport in Open Channel Flows Image source: http://earthsci.org/processes/geopro/stream/stream.html Arturo S. Leon, Ph.D., P.E., D.WRE Movies Scour at bridge model pier https://www.youtube.com/watch?v=48S_k6qAmsY&feature=emb_logo Utah Flash Flood https://www.youtube.com/watch?v=mXlr_Bgb-s0 Santa Clara Pueblo Flash Flood https://www.youtube.com/watch?v=nKOQzkRi4BQ Sediment Transport ● We study sediment transport to predict the risks of scouring of bridges, to estimate the siltation of a reservoir, etc. ● Most, if not all, natural channels have mobile beds ● Most mobile beds are in dynamic equilibrium: on average: sediment in = sediment out ● This dynamic equilibrium can be disturbed by . short-term extreme events (e.g., flash floods) . man-made infrastructure (e.g., dams) Source: https://www.flow3d.com/modeling-capabilities/sediment-transport-model/ Sediment Transport Fundamental Questions: ● Does sediment transport occur? (Threshold of motion). ● If so, then at what rate? (Sediment load) ● What net effect does it have on the bed? (Scour/accretion) The main types of sediment load (volume of sediment per unit of time) are Bed load and Suspended load. The sum is total load z = h Velocity Concentration Profile Profile Suspended z = z load ref Bed load Bed form motion: Dune Antidune Source: Lecture notes on Hydraulic, David Apsley Bed form motion (Cont.) Dune Antidune Source: https://armfield.co.uk/product/s8-mkii-sediment-transport-demonstration-channel/ Relevant Properties ● Particle ● Flow ‐Diameter, ‐Bed shear
    [Show full text]
  • Comparing the Calculation Method of the Manning Roughness Coefficient in Open Channels
    International Journal of Engineering Research & Technology (IJERT) ISSN: 2278-0181 Vol. 4 Issue 06, June-2015 Comparing the Calculation Method of the Manning Roughness Coefficient in Open Channels Hari Wibowo 2 2 1Student of Doktoral Program on University of Suripin , Robert Kodoatie , 2 Diponegoro, Civil Engineering Department, University of Diponegoro 50241Semarang, Central Java,Indonesia 1 Water Resources Engineering Department, 50241Semarang University of Tanjungpura, 78115 Pontianak, West Borneo, Indonesia Isdiyana3 3RiverBalai, Water ResourcesResearchCenter , Balitbang the Ministry ofPublic Works Abstract—In hydraulic engineering, Manning roughness Philippe Gauckler in 1867, and then re-developed by the coefficient is an important parameter in designing hydraulic Irlandia engineer Robert Manning in 1890 (Bahramifar et al., structures and simulation models. This equation is applied to 2013). both uniform open channel flow, which is used to calculate the The study of the roughness coefficient has been much average flow velocity. The procedure for selecting the value of Manning n is subjective and requires assessment and skills research done previously, including Cowan (1956) which developed primarily through experience. examines pengenai hydraulic calculations, the roughness ManyempiricalformulaMenningthat was developedin order coefficient andAgricutural Engineering. Arcement and toobtainthe valuekoefsieinManning roughness. Fromseveral Schneider (1984) make modifications to the formulation studiesincludingthe formulationCowan(1956),
    [Show full text]
  • Steady Flow Analysis of Pipe Networks: an Instructional Manual
    Utah State University DigitalCommons@USU Reports Utah Water Research Laboratory January 1974 Steady Flow Analysis of Pipe Networks: An Instructional Manual Roland W. Jeppson Follow this and additional works at: https://digitalcommons.usu.edu/water_rep Part of the Civil and Environmental Engineering Commons, and the Water Resource Management Commons Recommended Citation Jeppson, Roland W., "Steady Flow Analysis of Pipe Networks: An Instructional Manual" (1974). Reports. Paper 300. https://digitalcommons.usu.edu/water_rep/300 This Report is brought to you for free and open access by the Utah Water Research Laboratory at DigitalCommons@USU. It has been accepted for inclusion in Reports by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. STEADY FLOW ANALYSIS OF PIPE NETWORKS­ An Instructional Manual by Roland W. Jeppson Developed with support from the Quality of Rural Life Program funded by the Kellogg Foundation and Utah State University Copyright ® 1974 by Roland W. Jeppson This manual, or parts thereof, may not be reproduced in any form without permission of the author. Department of Civil and Environmental Engineering and Utah Water Research Laboratory Utah State University Logan. Utah 84322 $6.50 September 1974 TABLE OF CONTENTS Chapter Page FUNDAMENTALS OF FLUID MECHANICS Introduction . Fluid Properties Density. I Specific weight I Viscosity 1 Example Problems Dealing with Fluid Properties 2 Conservation Laws 3 In trodu cti on 3 Continuity. 3 Example Problems Applying Continuity 4 Conservation of Energy (Bernoulli Equation) 6 Example Problems Dealing with Conservation Laws 9 Momentum Principle in Fluid Mechanics 12 II FRICTIONAL HEAD LOSSES 13 Introduction . 13 Darcy-Weisbach Equation.
    [Show full text]
  • 5.2.4 Open Channels Gate Is Operated by Raising Or Lowering to Allow Water to Pass Beneath the Gate Plate
    128 Laymans Guidebook Chapter 5. Hydraulic structures 129 Photo 5.17 Photo 5.19 Globe and rotary valves (figure 5.28) have lower head losses than the slide and load. Because the hydrostatic load passes through the trunnions, the lifting force butterfly gate valves and are also commonly used in spite of their higher price. required by the hoisting mechanism is minimised. The head losses in gates and valves are relatively high, especially when are operated as regulating devices. The radial gates (figure 5.29), conceptually different, are a method of forming a For further details refer to Chapter 2, Section 2.2.4 and the enclosed bibliography. moveable overflow crest and allow a close control of headwater and tailwater. In photo 5.19 it can be seen the housing of the sector on a concrete pier. The radial 5.2.4 Open channels gate is operated by raising or lowering to allow water to pass beneath the gate plate. The curved plate that forms the upstream face is concentric with the trunnions 5.2.4.1 Design and dimensioning of the gate. The trunnions are anchored in the piers and carry the full hydrostatic The flow conveyed by a canal is a function of its cross-sectional profile, its slope, and its roughness. Natural channels are normally very irregular in shape, and their surface roughness changes with distance and time. The application of hydraulic theory to natural channels is more complex than for artificial channels where the cross-section is regular in shape and the surface roughness of the construction materials - earth, concrete, steel or wood - is well documented, so that the application of hydraulic theories yields reasonably accurate results.
    [Show full text]
  • FDM 13-30 Channels and Road Ditches
    Facilities Development Manual Wisconsin Department of Transportation Chapter 13 Drainage Section 30 Channels and Road Ditches FDM 13-30-1 Channel Types and Characteristics October 22, 2012 1.1 Channel Types Roadside drainage channels perform the vital functions of collecting surface water runoff from the highway and carrying it to natural channels, providing snow storage and filtering sediment from runoff. They should provide the most efficient, stable, and effective disposal system for highway surface runoff, consistent with cost, importance of the road, economy of maintenance, and legal requirements. A standard drainage channel rarely provides the most satisfactory drainage for all sections of the highway, although it is the most efficient for most locations. 1.2 Roadside Ditches Side ditches are provided in cut sections to remove runoff from cut slopes, pavement, and adjacent areas draining into the highway right-of-way. Side ditches typically are triangular in cross section and dimensioned in accordance with appropriate design standards. The depth may be varied to keep a desirable minimum longitudinal slope of 0.5 percent and to keep the runoff from the design year storm below the top of the highway subgrade (refer to FDM13-10 Attachment 1.1). The minimum depth of a ditch is 1 ft below the subgrade shoulder point to ensure positive drainage of the subgrade. Refer to FDM11-15-1 for cross section elements for rural highways and freeways. 1.3 Median Ditches The shape, slope, bottom width, and gradient of a median may be varied as required to suit conditions. The following median geometrics are given in Chapter 11: 1.
    [Show full text]