Introduction.

Slides:



Advertisements
Similar presentations
GEOLOGY 1B: CLASTIC SEDIMENTS
Advertisements

Aero-Hydrodynamic Characteristics
Free Convection: General Considerations and Results for Vertical and Horizontal Plates Chapter 9 Sections 9.1 through 9.6.2, 9.9.
The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL Fluid Dynamics with Erosion Brandon Lloyd COMP 259 May 2003.
Transport phenomena in chemical processes part III Michał Araszkiewicz PhD.
VIII. Viscous Flow and Head Loss. Contents 1. Introduction 2. Laminar and Turbulent Flows 3. Friction and Head Losses 4. Head Loss in Laminar Flows 5.
A.Erosion – The transportation of weathered sediments 1. Agents of Erosion or Transport Systems: a. Running water b. Wind c. Glaciers d. Waves & Tidal.
1 Physics of turbulence muna Al_khaswneh Dr.Ahmad Al-salaymeh.
CE 1501 Selected Topic: Open Channel Flow Reading: Munson, et al., Chapter 10.
Weathering and Erosion. Weathering Weathering - the process that breaks down rocks into smaller pieces.
Agents, Forces, and Results. Seminole_Canyon.JPG ntian_Clay_Beds_-_geograph.org.uk_-
FUNDAMENTAL EQUATIONS, CONCEPTS AND IMPLEMENTATION
Governing equations: Navier-Stokes equations, Two-dimensional shallow-water equations, Saint-Venant equations, compressible water hammer flow equations.
Physical Features of Estuaries. Basic Information Estuaries vary in origin, size and type Estuaries vary in origin, size and type Also called: lagoons,
Fluid Flow in Rivers Outline 1.Flow uniformity and steadiness 2.Newtonian fluids 3.Laminar and turbulent flow 4.Mixing-length concept 5.Turbulent boundary.
Unit 1: Fluid Dynamics An Introduction to Mechanical Engineering: Part Two Fluid dynamics Learning summary By the end of this chapter you should have learnt.
Garden Watering 1 Garden Watering. Garden Watering 2 Question: Water pours weakly from an open hose but sprays hard when you cover most of the end with.
Fluid Dynamics Stream Ecosystems. Fluid Dynamics Lecture Plan First consider fluids, stress relationships and fluid types Then consider factors affecting.
External Flows An internal flow is surrounded by solid boundaries that can restrict the development of its boundary layer, for example, a pipe flow. An.
EROSION- The transport of weathered materials…. Major Erosive Agents: Running Water GLACIERS WIND OCEAN CURRENTS AND WAVES MASS WASTING (GRAVITY!)
Chapter 5 - PBL MT 454 Material Based on Chapter 5 The Planetary Boundary Layer.
Conservation of Salt: Conservation of Heat: Equation of State: Conservation of Mass or Continuity: Equations that allow a quantitative look at the OCEAN.
Agents, Forces, and Results. Seminole_Canyon.JPG ntian_Clay_Beds_-_geograph.org.uk_-
Fluid Mechanics Credit Hours 4(3+1)
Viscosità Equazioni di Navier Stokes. Viscous stresses are surface forces per unit area. (Similar to pressure) (Viscous stresses)
Transport process In molecular transport processes in general we are concerned with the transfer or movement of a given property or entire by molecular.
Environmental Engineering Lecture Note Week 10 (Transport Processes) Joonhong Park Yonsei CEE Department CEE3330 Y2013 WEEK3.
Estuarine Circulation and the Knudsen Relation Puget Sound Oceanography 2011.
Constructive & Destructive Forces
Erosion and Deposition
Reynolds Number (Re) Viscosity: resistance of a liquid to change of form. Inertia: resistance of an object (body) to a change in its state of motion.
Erosion and Deposition
Erosion and Deposition
Chapter 4 Fluid Mechanics Frank White
Date of download: 10/22/2017 Copyright © ASME. All rights reserved.
Erosion and Deposition
Erosion.
Weathering, Erosion and Deposition
Summary of Chapter 4 Equations
Erosion and Deposition
Erosion and Deposition
Grab the sheet from the front and the brochure
Erosion and Deposition
Erosion and Deposition
Particle (s) motion.
External Flows An internal flow is surrounded by solid boundaries that can restrict the development of its boundary layer, for example, a pipe flow. An.
9-4 Mechanisms of Plate Motion
CHAPTER 6 Viscous Flow in Pipes
BASICS OF TURBULENT FLOW
Welcome to Earth Science
Erosion and Deposition
Transition of the laminar boundary layer on a flat plate into a fully turbulent boundary layer (not to scale). Trip Wires:
Fluid Friction in Pipes
Erosion.
External Forces Affecting Earth
Erosion Weathered rock particles are transported Agents of erosion
Section 2: Erosion and Deposition
Where Does the “Stuff” Go?
Forces That Shape the Earth’s Surface
Introduction.
Wind Erosion Sandblasting (abrasion) – occurs when winds blow sand or silt grains against rocks and other objects Lower portions of rocks become more eroded.
Unit 4: Lesson 2 Erosion and Deposition
Erosion and Deposition
Turbulent Kinetic Energy (TKE)
Coastal Erosion Workshop
Turbulent properties:
Erosion and Deposition
Internal Forces that Shape the Earth (Plate Actions)
Where Does the “Stuff” Go?
Membrane Transport Selectively permeable: The cell membrane acts like a wall around the cell but it does have pores that act like doors Filtration: process.
Presentation transcript:

Introduction

Conservation of momentum inertia pressure/gravity viscous

Flows and force balances 1. Slow flow in a slot 2. Oscillating slow flow 3. Small-amplitude waves 4. Fast flow away from an object 5. Fast flow near an object a. inertia ~ pressure/gravity b. viscous ~ inertia ~ pressure c. viscous ~ inertia d. viscous ~ pressure

Viscous flow in a slot or pipe Flow driven by a pressure gradient Flow driven by a moving wall

Viscous slot flow: extensions Glacier movement Groundwater Flow in the mantle

Viscous slot flow: extensions Particle settling Swimming of organisms Sediment transport

Turbulent flow in a slot or pipe Transition to turbulence “Law of the wall”

Turbulent pipe flow: extensions Open channel flow Glacier movement Municipal hydraulics Flow in vegetated channels

Unsteady viscous flow U U Impulsively started plate Oscillating plate

Unsteady viscous flow: extensions River mixing

Waves Surface waves of small amplitude

Waves: extensions Wave spectra Internal waves Solitary waves

Boundary layers

Boundary layers: extensions Gravity currents and salt wedges Biofilms Jets & plumes Diffusive BL in a lake