Engineering Bernoulli Equation
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Future Directions of Computational Fluid Dynamics
Future Directions of Computational Fluid Dynamics F. D. Witherden∗ and A. Jameson† Stanford University, Stanford, CA, 94305 For the past fifteen years computational fluid dynamics (CFD) has been on a plateau. Due to the inability of current-generation approaches to accurately predict the dynamics of turbulent separated flows, reliable use of CFD has been restricted to a small regionof the operating design space. In this paper we make the case for large eddy simulations as a means of expanding the envelope of CFD. As part of this we outline several key challenges which must be overcome in order to enable its adoption within industry. Specific issues that we will address include the impact of heterogeneous massively parallel computing hardware, the need for new and novel numerical algorithms, and the increasingly complex nature of methods and their respective implementations. I. Introduction Computational fluid dynamics (CFD) is a relatively young discipline, having emerged during the last50 years. During this period advances in CFD have been paced by advances in the available computational hardware, which have enabled its application to progressively more complex engineering and scientific prob- lems. At this point CFD has revolutionized the design process in the aerospace industry, and its use is pervasive in many other fields of engineering ranging from automobiles to ships to wind energy. Itisalso a key tool for scientific investigation of the physics of fluid motion, and in other branches of sciencesuch as astrophysics. Additionally, throughout its history CFD has been an important incubator for the formu- lation and development of numerical algorithms which have been seminal to advances in other branches of computational physics. -
Potential Flow Theory
2.016 Hydrodynamics Reading #4 2.016 Hydrodynamics Prof. A.H. Techet Potential Flow Theory “When a flow is both frictionless and irrotational, pleasant things happen.” –F.M. White, Fluid Mechanics 4th ed. We can treat external flows around bodies as invicid (i.e. frictionless) and irrotational (i.e. the fluid particles are not rotating). This is because the viscous effects are limited to a thin layer next to the body called the boundary layer. In graduate classes like 2.25, you’ll learn how to solve for the invicid flow and then correct this within the boundary layer by considering viscosity. For now, let’s just learn how to solve for the invicid flow. We can define a potential function,!(x, z,t) , as a continuous function that satisfies the basic laws of fluid mechanics: conservation of mass and momentum, assuming incompressible, inviscid and irrotational flow. There is a vector identity (prove it for yourself!) that states for any scalar, ", " # "$ = 0 By definition, for irrotational flow, r ! " #V = 0 Therefore ! r V = "# ! where ! = !(x, y, z,t) is the velocity potential function. Such that the components of velocity in Cartesian coordinates, as functions of space and time, are ! "! "! "! u = , v = and w = (4.1) dx dy dz version 1.0 updated 9/22/2005 -1- ©2005 A. Techet 2.016 Hydrodynamics Reading #4 Laplace Equation The velocity must still satisfy the conservation of mass equation. We can substitute in the relationship between potential and velocity and arrive at the Laplace Equation, which we will revisit in our discussion on linear waves. -
Manual for Lab #2
CE 321 INTRODUCTION TO FLUID MECHANICS Fall 2009 LABORATORY 3: THE BERNOULLI EQUATION OBJECTIVES To investigate the validity of Bernoulli's Equation as applied to the flow of water in a tapering horizontal tube to determine if the total pressure head remains constant along the length of the tube as the equation predicts. To determine if the variations in static pressure head along the length of the tube can be predicted with Bernoulli’s equation APPROACH Establish a constant flow rate (Q) through the tube and measure it. Use a pitot probe and static probe to measure the total pressure head h Tm and static pressure head h Sm at six locations along the length of the tube. The values of h Tm will show if total pressure head remains constant along the length of the tube as required by the Bernoulli Equation. Using the flow rate and cross sectional area of the tube, calculate the velocity head h Vc at each location. Use Bernoulli’s Equation, h Tm and h Vc to predict the variations in static pressure head h St expected along the tube. Compare the calculated and measured values of static pressure head to determine if the variations in fluid pressure along the length of the tube can be predicted with Bernoulli’s Equation. EQUIPMENT Hydraulic bench with Bernoulli apparatus, stop watch THEORY Considering flow at any two positions on the central streamline of the tube (Fig. 1), Bernoulli's equation may be written as V 2 p V 2 p 1 + 1 + z = 2 + 2 + z (1) 2g γ 1 2g γ 2 1 Bernoulli’s equation indicates that the sum of the velocity head (V 2/2g), pressure head (p/ γ), and elevation (z) are constant along the central streamline. -
Chapter 1 PROPERTIES of FLUID & PRESSURE MEASUREMENT
Fluid Mechanics & Machinery Chapter 1 PROPERTIES OF FLUID & PRESSURE MEASUREMENT Course Contents 1. Introduction 2. Properties of Fluid 2.1 Density 2.2 Specific gravity 2.3 Specific volume 2.4 Specific Weight 2.5 Dynamic viscosity 2.6 Kinematic viscosity 2.7 Surface tension 2.8 Capillarity 2.9 Vapor Pressure 2.10 Compressibility 3. Fluid Pressure & Pressure Measurement 3.1 Fluid pressure, Pressure head, Pascal‟s law 3.2 Concept of absolute vacuum, gauge pressure, atmospheric pressure, absolute pressure. 3.3 Pressure measuring Devices 3.4 Simple and differential manometers, 3.5 Bourdon pressure gauge. 4. Total pressure, center of pressure 4.1 Total pressure, center of pressure 4.2 Horizontal Plane Surface Submerged in Liquid 4.3 Vertical Plane Surface Submerged in Liquid 4.4 Inclined Plane Surface Submerged in Liquid MR. R. R. DHOTRE (8888944788) Page 1 Fluid Mechanics & Machinery 1. Introduction Fluid mechanics is a branch of engineering science which deals with the behavior of fluids (liquid or gases) at rest as well as in motion. 2. Properties of Fluids 2.1 Density or Mass Density -Density or mass density of fluid is defined as the ratio of the mass of the fluid to its volume. Mass per unit volume of a fluid is called density. -It is denoted by the symbol „ρ‟ (rho). -The unit of mass density is kg per cubic meter i.e. kg/m3. -Mathematically, ρ = -The value of density of water is 1000 kg/m3, density of Mercury is 13600 kg/m3. 2.2 Specific Weight or Weight Density -Specific weight or weight density of a fluid is defined as the ratio of weight of a fluid to its volume. -
Density and Specific Weight Estimation for the Liquids and Solid Materials
Laboratory experiments Experiment no 2 – Density and specific weight estimation for the liquids and solid materials. 1. Theory Density is a physical property shared by all forms of matter (solids, liquids, and gases). In this lab investigation, we are mainly concerned with determining the density of solid objects; both regular-shaped and irregular-shaped. In general regular-shaped solid objects are those that have straight sides that can be measured using a metric ruler. These shapes include but are not limited to cubes and rectangular prisms. In general, irregular-shaped solid objects are those that do not have straight sides that cannot be measured with a metric ruler or slide caliper. The density of a material is defined as its mass per unit volume. The symbol of density is ρ (the Greek letter rho). m kg (1) V m3 The specific weight (also known as the unit weight) is the weight per unit volume of a material. The symbol of specific weight is γ (the Greek letter Gamma). W N (2) V m3 On the surface of the Earth, the weight W of an object is related to its mass m by: W = m · g, (3) where g is the acceleration due to the Earth's gravity, equal to about 9.81 ms-2. Using eq. 1, 2 and 3 we will obtain dependence between specific weight of the body and its density: g (4) Apparatus: Vernier caliper, balance with specific gravity platform (additional table in our case), 250 ml graduate beaker. Unknowns: a) Various solid samples (regular and irregular shaped) b) Light liquid sample (alcohol-water mixture) or heavy liquid sample (salt-water mixture). -
Hydraulics Manual Glossary G - 3
Glossary G - 1 GLOSSARY OF HIGHWAY-RELATED DRAINAGE TERMS (Reprinted from the 1999 edition of the American Association of State Highway and Transportation Officials Model Drainage Manual) G.1 Introduction This Glossary is divided into three parts: · Introduction, · Glossary, and · References. It is not intended that all the terms in this Glossary be rigorously accurate or complete. Realistically, this is impossible. Depending on the circumstance, a particular term may have several meanings; this can never change. The primary purpose of this Glossary is to define the terms found in the Highway Drainage Guidelines and Model Drainage Manual in a manner that makes them easier to interpret and understand. A lesser purpose is to provide a compendium of terms that will be useful for both the novice as well as the more experienced hydraulics engineer. This Glossary may also help those who are unfamiliar with highway drainage design to become more understanding and appreciative of this complex science as well as facilitate communication between the highway hydraulics engineer and others. Where readily available, the source of a definition has been referenced. For clarity or format purposes, cited definitions may have some additional verbiage contained in double brackets [ ]. Conversely, three “dots” (...) are used to indicate where some parts of a cited definition were eliminated. Also, as might be expected, different sources were found to use different hyphenation and terminology practices for the same words. Insignificant changes in this regard were made to some cited references and elsewhere to gain uniformity for the terms contained in this Glossary: as an example, “groundwater” vice “ground-water” or “ground water,” and “cross section area” vice “cross-sectional area.” Cited definitions were taken primarily from two sources: W.B. -
Potential Flow
1.0 POTENTIAL FLOW One of the most important applications of potential flow theory is to aerodynamics and marine hydrodynamics. Key assumption. 1. Incompressibility – The density and specific weight are to be taken as constant. 2. Irrotationality – This implies a nonviscous fluid where particles are initially moving without rotation. 3. Steady flow – All properties and flow parameters are independent of time. (a) (b) Fig. 1.1 Examples of complicated immersed flows: (a) flow near a solid boundary; (b) flow around an automobile. In this section we will be concerned with the mathematical description of the motion of fluid elements moving in a flow field. A small fluid element in the shape of a cube which is initially in one position will move to another position during a short time interval as illustrated in Fig.1.1. Fig. 1.2 1.1 Continuity Equation v u = velocity component x direction y v y y y v = velocity component y direction u u x u x x x v x Continuity Equation Flow inwards = Flow outwards u v uy vx u xy v yx x y u v 0 - 2D x y u v w 0 - 3D x y z 1.2 Stream Function, (psi) y B Stream Line B A A u x -v The stream is continuity d vdx udy if (x, y) d dx dy x y u and v x y Integrated the equations dx dy C x y vdx udy C Continuity equation in 2 2 y x 0 or x y xy yx if 0 not continuity Vorticity equation, (rotational flow) 2 1 v u ; angular velocity (rad/s) 2 x y v u x y or substitute with 2 2 x 2 y 2 Irrotational flow, 0 Rotational flow. -
Darcy's Law and Hydraulic Head
Darcy’s Law and Hydraulic Head 1. Hydraulic Head hh12− QK= A h L p1 h1 h2 h1 and h2 are hydraulic heads associated with hp2 points 1 and 2. Q The hydraulic head, or z1 total head, is a measure z2 of the potential of the datum water fluid at the measurement point. “Potential of a fluid at a specific point is the work required to transform a unit of mass of fluid from an arbitrarily chosen state to the state under consideration.” Three Types of Potentials A. Pressure potential work required to raise the water pressure 1 P 1 P m P W1 = VdP = dP = ∫0 ∫0 m m ρ w ρ w ρw : density of water assumed to be independent of pressure V: volume z = z P = P v = v Current state z = 0 P = 0 v = 0 Reference state B. Elevation potential work required to raise the elevation 1 Z W ==mgdz gz 2 m ∫0 C. Kinetic potential work required to raise the velocity (dz = vdt) 2 11ZZdv vv W ==madz m dz == vdv 3 m ∫∫∫00m dt 02 Total potential: Total [hydraulic] head: P v 2 Φ P v 2 h == ++z Φ= +gz + g ρ g 2g ρw 2 w Unit [L2T-1] Unit [L] 2 Total head or P v hydraulic head: h =++z ρw g 2g Kinetic term pressure elevation [L] head [L] Piezometer P1 P2 ρg ρg h1 h2 z1 z2 datum A fluid moves from where the total head is higher to where it is lower. For an ideal fluid (frictionless and incompressible), the total head would stay constant. -
Fluid Mechanics
I. FLUID MECHANICS I.1 Basic Concepts & Definitions: Fluid Mechanics - Study of fluids at rest, in motion, and the effects of fluids on boundaries. Note: This definition outlines the key topics in the study of fluids: (1) fluid statics (fluids at rest), (2) momentum and energy analyses (fluids in motion), and (3) viscous effects and all sections considering pressure forces (effects of fluids on boundaries). Fluid - A substance which moves and deforms continuously as a result of an applied shear stress. The definition also clearly shows that viscous effects are not considered in the study of fluid statics. Two important properties in the study of fluid mechanics are: Pressure and Velocity These are defined as follows: Pressure - The normal stress on any plane through a fluid element at rest. Key Point: The direction of pressure forces will always be perpendicular to the surface of interest. Velocity - The rate of change of position at a point in a flow field. It is used not only to specify flow field characteristics but also to specify flow rate, momentum, and viscous effects for a fluid in motion. I-1 I.4 Dimensions and Units This text will use both the International System of Units (S.I.) and British Gravitational System (B.G.). A key feature of both is that neither system uses gc. Rather, in both systems the combination of units for mass * acceleration yields the unit of force, i.e. Newton’s second law yields 2 2 S.I. - 1 Newton (N) = 1 kg m/s B.G. - 1 lbf = 1 slug ft/s This will be particularly useful in the following: Concept Expression Units momentum m! V kg/s * m/s = kg m/s2 = N slug/s * ft/s = slug ft/s2 = lbf manometry ρ g h kg/m3*m/s2*m = (kg m/s2)/ m2 =N/m2 slug/ft3*ft/s2*ft = (slug ft/s2)/ft2 = lbf/ft2 dynamic viscosity µ N s /m2 = (kg m/s2) s /m2 = kg/m s lbf s /ft2 = (slug ft/s2) s /ft2 = slug/ft s Key Point: In the B.G. -
Introduction to Computational Fluid Dynamics by the Finite Volume Method
Introduction to Computational Fluid Dynamics by the Finite Volume Method Ali Ramezani, Goran Stipcich and Imanol Garcia BCAM - Basque Center for Applied Mathematics April 12–15, 2016 Overview on Computational Fluid Dynamics (CFD) 1. Overview on Computational Fluid Dynamics (CFD) 2 / 110 Overview on Computational Fluid Dynamics (CFD) What is CFD? I Fluids: mainly liquids and gases I The governing equations are known, but not their analytical solution: thus, we approximate it I By CFD we typically denote the set of numerical techniques used for the approximate solution (prevision) of the motion of fluids and the associated phenomena (heat exchange, combustion, fluid-structure interaction . ) I The solution of the governing differential (or integro-differential) equations is approximated by a discretization of space and time I From the continuum we move to the discrete level I The CFD is deeply connected to the improvement of computers in the last decades 3 / 110 Overview on Computational Fluid Dynamics (CFD) Applications of CFD I Any field where the fluid motion plays a relevant role: Industry Physics Medicine Meteorology Architecture Environment 4 / 110 Overview on Computational Fluid Dynamics (CFD) Applications of CFD II Moreover, the research front is particularly active: Basic research on fluid New numerical methods mechanics (e.g. transition to turbulence) Application oriented (e.g. renewable energy, competition . ) 5 / 110 Overview on Computational Fluid Dynamics (CFD) CFD: limits and potential I Method Advantages Disadvantages Experimental 1. More realistic 1. Need for instrumentation 2. Allows “complex” problems 2. Scale effects 3. Difficulty in measurements & perturbations 4. Operational costs Theoretical 1. Simple information 1. -
The Components of Total Head
THE COMPONENTS OF TOTAL HEAD This chapter will introduce some of the terminology used in pumping systems. The components of Total Head will be examined one by one. Some of the more difficult to determine components, such as equipment and friction head, will be examined in more detail. I hope this will help get our heads together. 3.0 THE COMPONENTS OF TOTAL HEAD Total Head is the measure of a pump's ability to push fluids through a system. Total Head is proportional to the difference in pressure at the discharge vs. the suction of the pump. It is more useful to use the difference in pressure vs. the discharge pressure as a principal characteristic since this makes it independent of the pressure level at the pump suction and therefore independent of a particular system configuration. For this reason, the Total Head is used as the Y-axis coordinate on all pump performance curves (see Figure 4-3). The system equation for a typical single inlet — single outlet system (see equation [2- 12]) is: 1 2 2 DHP = DHF1-2 + DHEQ1-2 + (v2 -v1 )+z2 +H2 -(z1 +H1) 2g [3-1] DHP = DHF + DHEQ + DHv + DHTS [3-1a] DHP = DHF +DHEQ +DHv + DHDS + DHSS [3-1b] Equations [3-1a] and [3-1b] represent different ways of writing equation [3-1], using terms that are common in the pump industry. This chapter will explain each one of these terms in details. 3.1 TOTAL STATIC HEAD (DHTS) The total static head is the difference between the discharge static head and the suction static head, or the difference in elevation at the outlet including the pressure head at the outlet, and the elevation at the inlet including the pressure head at the inlet, as described in equation [3-2a]. -
Glossary of Terms — Page 1 Air Gap: See Backflow Prevention Device
Glossary of Irrigation Terms Version 7/1/17 Edited by Eugene W. Rochester, CID Certification Consultant This document is in continuing development. You are encouraged to submit definitions along with their source to [email protected]. The terms in this glossary are presented in an effort to provide a foundation for common understanding in communications covering irrigation. The following provides additional information: • Items located within brackets, [ ], indicate the IA-preferred abbreviation or acronym for the term specified. • Items located within braces, { }, indicate quantitative IA-preferred units for the term specified. • General definitions of terms not used in mathematical equations are not flagged in any way. • Three dots (…) at the end of a definition indicate that the definition has been truncated. • Terms with strike-through are non-preferred usage. • References are provided for the convenience of the reader and do not infer original reference. Additional soil science terms may be found at www.soils.org/publications/soils-glossary#. A AC {hertz}: Abbreviation for alternating current. AC pipe: Asbestos-cement pipe was commonly used for buried pipelines. It combines strength with light weight and is immune to rust and corrosion. (James, 1988) (No longer made.) acceleration of gravity. See gravity (acceleration due to). acid precipitation: Atmospheric precipitation that is below pH 7 and is often composed of the hydrolyzed by-products from oxidized halogen, nitrogen, and sulfur substances. (Glossary of Soil Science Terms, 2013) acid soil: Soil with a pH value less than 7.0. (Glossary of Soil Science Terms, 2013) adhesion: Forces of attraction between unlike molecules, e.g. water and solid.