s and FE X. A. Flow measurement B. properties C. statics D. impulse, and momentum equations E. Pipe and other internal flow 7% of FE Morning Session I

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Fundamentals of Engineering (FE) Exam General Section Steven Burian Civil & Environmental Engineering October 26, 2010

s and FE X. A. Flow measurement B. properties C. statics D. impulse, and momentum equations E. Pipe and other internal flow 7% of FE Morning Session IV. A. Bernoulli equation and mechanical energy balance B. Hydrostatic pressure C. Dimensionless numbers (e.g., Reynolds Number) D. Laminar and turbulent flow E. Velocity head F. Friction losses (e.g., pipes, p valves, fittings) G. Pipe networks H. Compressible and incompressible flow I. Flow measurement (e.g., orifices, Venturi meters) J. Pumps, turbines, and compressors K. Non-Newtonian Newtonian flow L. Flow through packed beds 10% of FE Afternoon Session

FE Statics s! s are substances in either the liquid or gas phase! s cannot support shear, and they deform continuously to minimize applied shear forces

FE Statics

FE Statics Viscosity! Shear stress (!): force required to slide one unit area layer of a substance over another! Viscosity ("): measure of a fluid s resistance to flow when acted upon by an external force (i.e., ease with which a fluid pours)! As a fluid moves a shear stress is developed in it; magnitude is dependent on viscosity of fluid

F/A is the fluid shear stress (!) and the constant of proportionality p is the absolute viscosity ("): FE Statics! # " du dy Newtonian fluids: strains are proportional to the applied shear stress Non-Newtonian Newtonian fluids: fluid shear stress can be computed using the power law The kinematic viscosity is the ratio of the absolute viscosity to mass density: $ % # "

FE Statics

FE Statics Surface Tension! The skin that seems to form on the free surface of a fluid is caused by intermolecular cohesive forces and is known as surface tension, &! Surface tension can be interpreted as the tensile force between two points a unit distance apart on the surface

FE Statics Capillarity! Capillary action is caused by surface tension between the liquid and a vertical solid surface! In water, adhesive forces between liquid molecules and surface are greater than cohesive forces between water molecules; adhesive forces cause water to attach itself to and climb solid vertical surface

FE Pressure Statics! Hydrostatic pressure is the pressure a fluid exerts on an immersed object or on container walls! Pressure is equal to the force per unit area of the surface: F P # A

FE Statics Pressure! Gage pressure: measured relative to a reference pressure - typically local atmospheric pressure! Absolute pressure: measured relative to a perfect vacuum! Absolute, gage, and atmospheric pressure are related as follows: P abs = P gage + P atm

FE Pressure Statics P 1 gage P 1 abs P 2 abs P 2 gage Munson et al. (2002)

FE Hydrostatic Pressure Statics 'P P = change in pressure ( = specific weight of fluid 'h h = change in depth in fluid 'P P = ('h ***Incompressible fluid at rest

FE Statics Manometry! Manometers measure pressure or pressure differences! Differential manometers: both ends connected to pressure sources! Open manometers: one end open to the atmosphere

FE Solving Manometer Problems Statics 1. Select a convenient starting point (usually at one of the endpoints) 2. Using 'P P = (h, write expressions for changes in pressure from starting point to point at opposite end of manometer system. Watch algebraic signs! 3. Equate expression from step 2 to pressure at final point 4. Substitute known values and solve for desired quantity

FE Barometers Statics

FE Buoyancy Statics! The buoyant force exerted by a fluid is equal to the weight of the fluid displaced and is directed vertically upward (Archimedes Principle): F b = (VV d where F b = the buoyant force ( = specific weight of the fluid V d = displaced volume of the fluid

FE Displaced Volume Statics Displaced volume

FE Statics Solving Buoyancy Problems! If the object is at rest in the fluid, use the equation of static equilibrium in the vertical direction, )F y = 0! The buoyant force passes vertically through the centroid of the displaced volume of fluid. This point is called the center of buoyancy.

FE Forces on Surfaces Statics! Pressure on a horizontal plane surface is uniform over the surface! Resultant t force of pressure distribution ib ti acts through center of pressure of surface and is: R # PA R = resultant vertical force P = pressure on the horizontal surface A = area of submerged horizontal surface

FE Forces on Surfaces Statics

FE Free Surface Forces on Surfaces O * Statics h C h y y c x R df y R A R y " " I xc y R + Ay # P A # h A c avg ( c y da Centroid, c Center of Pressure, CP I xyc x R # + Ay # c c c x

FE Statics Laminar and Turbulent Flow Laminar Flow:! Relatively low velocities! No mixing or a very small degree of mixing! appears to flow in continuous layers with no interaction between the layers Turbulent Flow:! Relatively high velocities! High degree of mixing! motion appears chaotic

FE Flow Distribution Statics

FE Reynolds Number Statics

FE Statics Reynolds Number Circular Pipe Flow Re < 2000 laminar flow 2000 < Re < 4000 transition region Re > 4000 turbulent flow Open Channel Re < 500 laminar flow 500 < Re < 2000 transition region Re > 2000 turbulent flow

FE One-Dimensional Flows Statics

FE Compressible Flows Statics Continuity: m! # m! 1 m 2 $ A v # $ A v 1 1 1 2 2 Ideal Gas Law: 2 P # $RT [P is pressure] [R is the gas constant] [T is temperature]

FE Statics Incompressible s Continuity Equation: A # v A v 1 1 2 2

FE Bernoulli Equation Statics

FE Mechanical Energy Equation Statics

FE Friction Loss Statics Valid for laminar and turbulent flow

FE Moody Chart Statics

FE Statics Friction Loss Hazen-Williams Equation: v # 0.63 0.849 CR S 0.54 v = velocity [m/s] C = roughness coefficient [varies from 140 to 100] R = hydraulic radius = A/WP [m] S = slope of HGL = h L /L [dimensionless] Valid for turbulent t flow of water

FE Minor Loss h # h + L f h f,fitting Statics h f,fitting # C 2 v 2g [C = loss coefficient (or resistance coefficient)]

FE HGL and EGL Statics

FE Statics HGL and EGL Velocity Head (v 2 /2g) Pressure Head (P/() Total Head or Energy Grade Line (EGL) Hydraulic Grade Line HGL Elevation Head (z) Z = 0

FE Statics Pump-Turbines Net head added to system by mechanical device 2 1 P v P 1 + z + + h, h # 2 + z + 1 s L 2 ( 2g ( v 2 2 2g

FE Open Channel & Pipe Flow Statics

FE Impulse- Statics

FE Statics Impulse- ) F # Q $ v, Q $ v x 2 2 2x ) F # $, $ y z 1 1 1x Q v Q v 2 2 2y 1 1 1y ) F # Q $ v, Q $ v 2 2 2z 1 1 1z Sum of the external forces Net rate of momentum entering control volume

FE Drag Force Statics

FE Drag Coefficient Statics

FE Pipe Networks Statics

Good Luck!!! Steve Burian Department of Civil & Environmental Engineering burian@eng.utah.edu