• Study Resource
  • Explore
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Lecture Notes for First Quiz - Atmospheric and Oceanic Sciences
Lecture Notes for First Quiz - Atmospheric and Oceanic Sciences

... thermal (kappa) and mechanical (nu) dissipation tend to reduce flow complexity Temperature and density perturbations are of opposite sign Reduced gravity Coefficient of expansion At the critical value Ra=1708, buoyancy overcomes viscous dissipation and the fluid begins to move. “Benard convection: A ...
B12a - damtp - University of Cambridge
B12a - damtp - University of Cambridge

... 2. A film of viscous fluid of uniform thickness h flows steadily under the influence of gravity down a rigid vertical wall. Assume that the surrounding air exerts no stress on the fluid. Calculate the velocity profile and find the volume flux (per unit width) of fluid down the wall. 3. A long, horiz ...
Lecture 5
Lecture 5

Fluid Dynamics
Fluid Dynamics

Hydraulic Fracturing: Of Magic and Engineering
Hydraulic Fracturing: Of Magic and Engineering

... properties) being laterally homogenous away from the wellbore. Many field microseismic data sets have shown this assumption to be incorrect! ...
MECHANISM CLUSTER First Year B.Eng/M.Eng 2007 Solutions to
MECHANISM CLUSTER First Year B.Eng/M.Eng 2007 Solutions to

... of height 3d. The cylinder is placed across the flow in the middle of the test section. The reading of a Pitot-static tube in a uniform flow at the inlet of the test section is 150mm of water. A velocity profile is measured at the outlet of the test section. It consists of a viscous wake which thick ...
this article as PDF
this article as PDF

... the flow rate in real time to the mine's control system. The first Greyline meters were installed in January 2013 and since then 44 AVFM 5.0 Area-Velocity Flow Meters have been deployed in the project. Engineers at Minera Escondida now have a better understanding and greater control of mass balance, ...
CVE 240 – Fluid Mechanics
CVE 240 – Fluid Mechanics

Balanced Flow
Balanced Flow

... constant latitude (f not changing), the radius of curvature must also be constant. So any air parcels that are moving will flow in a circular fashion, anti-cyclonically in the Northern Hemisphere. We know it must be anti-cyclonic motion since the Coriolis Force pulls air to the right in the NH. For ...
PIPELINE SYSTEMS
PIPELINE SYSTEMS

... In many pipe systems there is more than one pipe involved. The governing mechanisms for the flow in multiple pipe systems are the same as for the single pipe systems discussed in earlier lectures (n5,n6). However, because of the numerous unknowns involved, additional complexities may arise in solvin ...
Product Data Sheet: Damcos DPI-B - direct hydraulic open/closed
Product Data Sheet: Damcos DPI-B - direct hydraulic open/closed

Sample Paper
Sample Paper

... (a) Viscosity of water is about two orders of magnitude more than that of air (b) Kinematic viscosity of water is less than kinematic viscosity of air (c) Both air and water are Newtonian fluids whereas blood is a non-Newtonian fluid (d) Viscosity of both air and water change with temperature 2. If ...
Comments on the turbulence lecture
Comments on the turbulence lecture

PSAA Curriculum
PSAA Curriculum

Chap 5 Instruments
Chap 5 Instruments

Document
Document

... 1. What conclusion can be made from the above result? 2. If we are to carry out an MEB on the system (ΣF is significant), what result should we expect? What is ΣF is negligible? ...
Using Dimensions
Using Dimensions

Modelling Two
Modelling Two

4. Analysis of Standing Vertical Jumps Using a
4. Analysis of Standing Vertical Jumps Using a

... otherwise you will lose the cursors. If you find that you have lost a cursor, rescale the time axis to the original settings (0.00 to 5.00 seconds). Minor software bug #1: Changing the time axis scale will reset the force axis scale to the original setting (0 to 4000 N). Minor software bug #2: When ...
A Measure of Stream Turbulence
A Measure of Stream Turbulence

CVE 240 – Fluid Mechanics
CVE 240 – Fluid Mechanics

... outlet ports, and the velocity v is uniformly distributed (constant) across each ...
- Iowa Research Online
- Iowa Research Online

Lecture 4
Lecture 4

Types of Flow
Types of Flow

... considered to have incompressible flows. ...
Newtonian, Non-Newtonian Fluids and Viscosity
Newtonian, Non-Newtonian Fluids and Viscosity

< 1 2 3 4 5 6 >

Hydraulic jumps in rectangular channels



Hydraulic jump in a rectangular channel, also known as classical jump, is a natural phenomenon that occurs whenever flow changes from supercritical to subcritical flow. In this transition, the water surface rises abruptly, surface rollers are formed, intense mixing occurs, air is entrained, and often a large amount of energy is dissipated. In other words, a hydraulic jump happens when a higher velocity, v1, supercritical flow upstream is met by a subcritical downstream flow with a decreased velocity, v2, and sufficient depth. Numeric models created using the Standard Step Method or HEC-RAS are used to track supercritical and subcritical flows to determine where in a specific reach a hydraulic jump will form. There are common hydraulic jumps that occur in everyday situations such as during the use of a household sink. There are also man-made hydraulic jumps created by devices like weirs or sluice gates. In general, a hydraulic jump may be used to dissipate energy, to mix chemicals, or to act as an aeration device.To produce equations describing the jump, since there is an unknown energy loss, there is a need to apply conservation of momentum. To develop this equation, a general situation in which there may or may not be an energy loss between upstream and downstream, and there may or may not be some obstacle on which there is a drag force Pf is considered. however, for a simple or classic hydraulic jump the force per unit width(Pf) equals 0. From there the momentum equation, and the conjugate depths equation can be derived.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report