Phys 629: Selected Topics in Physics I (Spring 2020) — Fluid Mechanics & Acoustics in the Ocean
Instructor: Dr. Zheguang Zou (zou@olemiss.edu)
Lectures: Monday, Wednesday, Friday 9:00-9:50am @ Google Meet (http://meet.google.com/rej-rjte-ejp)
Office Hours: Online, by appointment
Website: https://zou.olemiss.edu/phys629
Syllabus | Lectures | Homework
Fluid Mechanics
Lecture 01 - Introduction & Fluid Properties (1/22)
- What is a fluid?
- DEF. — deforms contineously when acted on by a shearing stress of any magnitue.
- sheering stress
- tangential force
- "Heaviness"
- density
- specific volume
- specific weight
- specific gravity
Lecture 02 - Fluid Properties (cont.) (1/24)
- Compressibility
- bluk modulus
- compressible vs. incompressible fluids
- isothermal vs. isentropic processes
- sound speed
- "Stickiness"
- viscosity
- no-slip condition
- shear stress
- rate of shearing strain
- Newtonian vs. Non-Newtonian
- shear thinning vs. shear thickening
Related Videos:
- Test the Viscosity of a Liquid
- Shear Thickening vs. Shear Thinning
- Shear Thickening Fluids
- Fun with Non-Newtonian Fluid (shear thicking)
- Why is ketchup so hard to pour?
Lecture 03 - Fluid Properties (cont.) (1/27)
- Surface Tension
- \sigma = F/L
- mechanism: due to imbalance of molecular force
- Why droplets are spherical? — To minimize the surface area
- contact line
- contact angle
- high/low wetting = small/large contact angle
- capillary rise (wetting) vs. capillary fall (non-wetting)
- cohesive force (liquid) vs. adhesive force (solid-liquid)
Related Videos:
- Floating Razor Blade
- Water strider - Walking on water
- What is Surface Tension?
- Soil Basics: Capillary Rise
Lecture 04 - Fluid Statics (1/29)
- Pressure at a Point
- Pascal's law: the pressure at a point in a fluid at rest, or in motion, is independent of direction as long as there are no shearing stresses present.
- Basic Equation for Pressure Fields
- surface force; body force
- gradient operator
- pressure gradient
- general equation of motion
- Pressure Variation at Rest
- depends on depth only (shape or size doesn't matter)
- pressure head
Related Videos:
Lecture 05 - Fluid Statics (cont.) (1/31)
- Hydraulics
- hydraulic lift, hydraulic press
- requirements: imcompressible fluid; no air
- Pressure Measurement
- absolute pressure
- gauge pressure
- standard atmosphere pressure: 101.325 kPa (or 14.7 psi)
- underwater pressure: ~ 1 atmophere pressure every 10 m
- piezometer, U-tube, etc.
- Buoyancy
- Archemedes' Priciple
- stability of floating objects
Related Videos:
Lecture 06 - Fluid Statics (cont.) (2/7)
- Pressure Variation in Linear Motion
- linear acceleration
- curvature: line
- example: a bottle of Coke in an accelerating car
- Pressure Variation in Rotation
- angular acceleration
- gradient in cylindrical coordinates
- curvature: parabolic shape
Related Videos:
Lecture 07 - Elementary Fluid Dynamics & Bernoulli Equation (2/10)
- Fluid Particle
- Velocity Vector
- Streamlines
- DEF. = lines that are tangent to velocity vector
- two acceleration components
- a_s: along a streamline
- a_n: normal to a streamline
- Ideal Flows
- inviscid (no viscosity)
- steady (no change over time)
- imcompressible (density doesn't change)
- Bernoulli Equation (along a streamline)
Related Videos:
Lecture 08 - Bernoulli Equation (cont.) (2/12)
- Bernoulli Equation (normal to a streamline)
- Static, Dynamic, Hydrostatic Pressures
- Stagnation
- stagnation point
- stagnation streamline
- Conservation of Mass (continuity equation)
- Pitot-Static Tube: to measure flow velocity
- Free Jet
Related Videos:
- Stagnation Point in a Flow
- Illustration of Stagnation Point
- Pitot-Static Tube
- Pitot-Static Systems in a Airplane
Lecture 09 - Bernoulli Equation (cont.) & Fluid Kinematics (2/14)
- Cavitation
- pressure and boiling point
- Flow Descriptions
- Eulerian: one fixed position
- Lagrangian: one particle
- Pathline (vs. Streamline)
- Velocity Components (u, v, w)
- Material Derivative (D/Dt)
- as "seen" by a material point
- local term
- convective term
- System, Control Volume, Control Surface
Related Videos:
Lecture 10 - Fluid Kinematics (cont.) (2/17)
- Flow Rate
- volume flow rate
- mass flow rate
- in vector form: the area vector is always pointing outwards from the volume
- Extensive vs. Intensive Property
- B = mb
- unit of b = [unit of B]/kg
- Reynolds Transport Theorem
- link between system & control volume
- net outflow = outflow - inflow
Related Videos:
Lecture 11 - Fluid Kinematics (cont.) & Finite Control Volume Analysis (2/19)
- Reynolds Transport Theorem and Material Derivative
- a collection of fluid particles vs. a fluid particle
- in fact, dB/dt = DB/Dt
- Conservation Laws (applying Reynolds Transport Theorem)
- Conservation of Mass
- Conservation of Momentum (Newton's Second Law of Motion)
- Conservation of Energy (First Law of Thermodynamics)
- Absolute Velocity and Relative Velocity
- V (abs velocity) = W (relative) + V_cv (velocity of control volume)
Related Videos:
Lecture 12 - Differential Analysis (2/26)
- Linear Deformation
- imcompressible condition
- Angular Deformation
- irrotational condition
- vorticity
- Conservation of Mass (differential form)
Related Videos:
Lecture 13 - Differential Analysis (cont.) (2/28)
- Stress
- normal stress
- shearing stress
- Eulers Equation of Motion (without viscosity)
- assupmtion: imcompressible, no viscosity
- Navier-Strokes Equation (with viscosity)
- assumption: imcompressible, constant viscosity
Related Videos:
Lecture 14 - Differential Analysis (cont.) & Dimensionless (3/2)
- Navier Strokes Equation
- Reynolds Number
- inertial force vs. viscous force
- Laminar flows (Re < 2000)
- Turbulent flows (Re > 4100)
- Mach Number
- inertial force vs. compressible force
- imcompressible (Ma < 0.3)
- Bond Number
- gravitational force vs. surface tension
Related Videos:
Ocean Dynamics
Lecture 15 - Introduction & Physical Settings (3/4)
- Physical Settings of the Earth
- Earth Radius: Re = 6378 km, Rp = 6357 km
- Latitude: 1 deg = 111 km
- Longitude: 1 deg = 111 cos(Latitude) km
- Nautical Mile (nm): 1 nm = 1.852 km
- Continental Margin
- continental shelf, slope, rise
- Ocean Basin
- abyssal plains, hills, seamounts, trenches
- Mid-Ocean Ridges
- Aspect Ratio: ~1:1000
- the ocean is shallow if compared to its width
Lecture 16 - The World Ocean (3/6)
- Oceans
- Pacific Ocean: largest, 1/3 of earth surface, oldest ocean
- Atlantic Ocean: 2nd largest, 1/5 of earth surface, youngest ocean
- Indian Ocean: 3rd largest, currents change direction twice a year due to monsoon
- Artic Ocean: smallest, shallowest, 50% being continental shelf
- Southern Ocean: not existed before 2000, defined by antartica circumpolar currents
- Scales
- time scale: 0.1 s to 10^4 years
- sptial scale: 1 mm to 10^4 km
- Some Ocean Phenomona
- capillary-gravity waves
- surface wind waves
- internal waves
- eddies
Related Videos:
Lecture 17- Physical Properties of Seawater
- Pressure
- hydrostatic balance
- 1 bar = 10^5 Pa = 1 atmosphere pressure
- 1 dbar = 0.1 bar = pressure caused by water of 1 m depth
- Temperature
- absolute temperature (Kelvin)
- adiabatic process
- potential temperature
- take out the temperature raise due to compression
- Salinity
- the measure of how many grams of salt in 1 kg seawater (
- unit: parts per thousand (ppt)
- morden measurement: based on conductivity
- unit: psu (practical salinity unit)
- CTD (conductivity, temperature, depth) profiler
- the measure of how many grams of salt in 1 kg seawater (
Related Videos:
Lecture 18- Physical Properties of Seawater (Cont.)
- Density
- seawater density: often write out last two digits
- depends on temperature, salinity and pressure
- potential density
- density calculated from the potential temperature
- Temperature-Salinity (T-S) Diagram
- water parcel remains its temperature and sanlity characterists once sink from the surface
- Thermohaline Circulation
Related Videos:
Lecture 19 - Ocean Circulations (4/1)
- Two Types of Ocean Circulations
- Thermohaline Circulation
- deep ocean
- density-driven
- low-latitude vs. high-latitude profiles
- pycnocline, thermocline
- Wind-Driven Circulation
- atmospheric circulation
- Coriolis effect
- deflection of moving fluids
- northern hemisphere
- ocean gyres
Related Videos:
Lecture 20 - Ocean Circulations (Cont.) (4/3)
- Ekman Theory
- Ekman spiral
- Ekman transport: net water transport due to surface wind
- directions of wind, surface current, and net water transport
- Upwelling and Downwelling
- coastal regions
- equator upwelling
- biological production
- Geostrophic Balance
- horizontal pressure gradient force
- coriolis force
- geostrophic flow along isobars
- Sea Surface Height
- invert geostrophic currents
- satellite altimetry
- eddies
- warm core rings and cold core rings
Related Videos:
- Ekman Theory: Wind, Surface Currents, Upwelling and Downwelling
- Sea Surface Height from Satellite Altimetry
- How do ocean currents work?
Lecture 21 - Tides (4/6)
- Tidal Force
- Two Water Bulges
- gravitational force and centrifugal force
- high tide and low tide
- Tidal Patterns
- semidiurnal tides
- diurnal tides
- mixed tides
- Spring and Neap Tides
- the alignment of sun and moon
- spring tide: full moon or new moon
- neap tide: first-quarter moon or third quater moon
- Lunar Day
- period: 24 hr 50 mins
- Tidal Prediction
Related Videos:
Lecture 22 - Tides (Cont.) (4/8)
- Tides in a Narrow Basin
- deflected to the right (left) in the northern (southern) hemisphere due to Coriolis Effect
- tidal time and range
- Tides in an Open Basin
- slossing water
- amphidromic system
- tidal spider
- amphidromic point (AP)
- Tidal Bores
- A large wave caused by the constriction of the spring tide as it enters a long, narrow, shallow inlet
- the biggest tidal bore in the world: Qiantang River, China
- Tidal Currents
- flood: seawater moves landward
- ebb: seawater moves seaward
- slack: tidal current is about to reverse direction
- Estuaries
- interaction between freshwater and seawater
- stratification patterns
Related Videos:
Lecture 23 - Waves (4/13)
- Wave Parameters
- wavelength, wavenumber
- wave period, angular frequency
- wave speed
- dispersion
- Water Motion
- Deep Water Waves
- water depth > 1/2 wavelength
- Waves can feel the bottom
- circular motion
- Shallow Water Waves
- water depth < 1/20 wavelength
- Waves cannot feel the bottom
- elliptical motion
- Wind-Driven Ocean Waves
- generation: wind speed, fetch, duration
- sea: "confused", irregular state, strong wave interefence
- swell: regular state, dispersion
- surf: get to coastal area
- wave breaking
- wave refraction
Related Videos:
Lecture 24 - Waves (Cont.) (4/15)
- Tsunami
- Japanese: "harbor waves"
- caused by an earthquake, submarine landslide, or other disturbance
- big wave, high energy
- shallow water wave (wavelength >> water depth)
- speed: extremely fast
- Internal Waves
- stratification in the ocean
- waves inside the ocean interior
- surface signature
- stability
- Buoyancy Frequency
Related Video:
Lecture 25 - Waves (Cont.) 4/20
- Internal Waves
- buoyancy frequency, N
- internal interfacial waves
- Internal waves in continuously stratified ocean
- inertial currents
- Coriolis frequency
- generation
- Kelvin Waves
- Coriolis effect
- at the equator
- Rossby Waves
- planetary, relative and total vorticity
- conservation of total vorticity
- Wave Type, Restoring Force, and Dispersion Relation
Related Videos:
Ocean Acoustics
Lecture 26 - Basics of Sound Propagation (4/22)
- Sound Speed
- lower compressibility, higher sound speed
- increase with temperature, salinity and pressure
- Refraction
- Snell's Law
- "lazy": bending to smaller sound speed
- Sound Speed Profiles
- positive: down-refracting
- netactive: up-refracting
- Multipath Effect
- direct path, surface reflection, bottom reflection
- Transmission Loss
- sphereical spreading ~ R^2
- cylindrical spreading ~ R (shallow-water)
Lecture 27 - Basics of Sound Propagation & Time-Varying Environment (4/24)
- Attenuation
- absorption
- scattering
- Rayleigh Parameters
- P < 1, coherent reflection
- P > 1, incoherent scattering
- Doppler Effect
- Ambient Noise
- Variability
- daily: tidal dynamics
- seasonal: seasonal temperature, global dynamics
- Ocean dynamics
- Internal Waves
- Biological Effect
Lecture 28 - Sound Propagation in the Ocean (4/27)
- Acoustic Modeling
- ray-tracing model
- parablic equation (PE) model
- Acoustic Channel
- multipath effect
- direct path
- surface reflections
Lecture 29 - Environmental Variability on Acoustics (4/29)
- Ocean Stratification
- temperature, salinity and density
- Estuariane Stratification
- ebbing vs. flooding
Lecture 30 - Environmental Variability on Acoustics (5/1)
- Direct-path Fading Phenomenon
- Richardson Number
- Case Study: HFA97