Lecture 7-River Dynamics 1 Flashcards

1
Q

Hydraulics of river flow equation

A

Q=Av=wdv
Q = discharge
A = area (width x depth)
v = average velocity

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2
Q

What determines the flow velocity?

A

Fluid mechanics (all the forces that are pushing, pulling and acting on water)

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3
Q

Why are rivers important to study in a hydrological sense?

A

They are a combination of everything happening upstream:
-groundwater
-soil water movement
-precipitation
-evaporation
all of this ends up combined in rivers which then moves through water through the catchment
-health of rivers tells us about the health of the system
-also one of the most hazardous components of the system (floods)

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4
Q

When does flow occur:

A

fluid subjected to mechanical potential energy gradient

  • gravity (gravitational potential energy)
  • hydrostatic pressure (hydrostatic potential energy)
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5
Q

mechanical potential energy gradient (break it down)

A

gradient: difference between two things over a length/time (relative differences)
energy: forces which push/pull
potential: baseline but not always realised (what forces are more/less important)
mechanical: how objects will relate to each other

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6
Q

gravity (force)

A
  • 9.81 m s^(-2)
  • relative difference: gradient when comparing two points at different heights relative to a datum
  • goes from high to low to balance
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7
Q

hydrostatic pressure (force)

A
  1. Magnitude:
    - force related to the weight of water and air above
    - Pressure = Pw + Pa
    - Pw = water pressure determined by the weight density of water and the height of water above
    - Pa = air pressure above
    - Hydrostatic pressure is a component of potential energy
    - need to know relative difference when comparing two points
  2. Direction:
    - at any point, pressure is equal in all directions (only determined by weight above)
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8
Q

other forces retard flow or alter course due to (1):

A

boundary conditions

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9
Q

Force formula

A

Force = mass x acceleration (operate as a point)

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10
Q

Force formula

A

Force = mass x acceleration (operate as a point)
where:
Acceleration = dV / dt (change of velocity over change of time)

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11
Q

Hydrostatic potential energy formula

A

Epp = 𝛄By
Epp = Potential energy of hydrostatic pressure
where y = vertical distance from the surface

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12
Q

Gravitational potential energy formula

A
Epg = 𝛄Bz
Epg = Potential energy gradient
𝛄 = weight density
B = volume
z = height above datum
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13
Q

Potential energy formula

A

Ep = Epg + Epp

basically add together hydrostatic potential energy + gravitational potential energy

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14
Q

Forces in open-channel flows:

A
  • Induce/maintain: act in the direction of flow →
  • Resist: act opposite to flow ←
  • Turncoat: act with or against flow depending on specific conditions ↔
  • Act perpendicular to flow •
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15
Q

Forces in open-channel flows:

A
  • Induce/maintain: act in the direction of flow →
  • Resist: act opposite to flow ←
  • Turncoat: act with or against flow depending on specific conditions ↔
  • Act perpendicular to flow •
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16
Q

Hydrostatic pressure gradient formula

A

Fp / M = g⧍Y / X
Y=depth
X = distance between them
(can act in either direction)

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17
Q

Frictional forces

A

-Viscosity

18
Q

Frictional forces

A
  • Viscosity

- Turbulence

19
Q

Viscosity

A

-friction of a fluid that resists forces tending to cause flow (shear stress resisting motion)
-no-slip condition
-water at the bed has the same velocity as the bed, as we get further up the bed as less influence
-water at the surfacing is moving fastest
-think deck of cards
—————–>
————–>
———–>
——–>
—–>
–>
__________

20
Q

Turbulence

A
  • related to eddy viscosity

- depends on the characteristics of the flow (depth and velocity)

21
Q

Minor forces that happen perpendicular to flow

A
  • surface tension
  • centrifugal
  • coriolis
22
Q

Surface tension

A
  • pull on water as it tries to keep bonded together

- only significant in very small water volumes

23
Q

Centrifugal

A
  • related to curvature of the path

- when going around a bend, will change speed and trajectory

24
Q

Coriolis

A
  • related to rotation of the earth

- left is S. Hemisphere, right in N. Hemisphere

25
Forces summary and overall equation
-Accelerate motion: gravity, pressure gradient -Resist motion: pressure gradient, viscosity, turbulence -Right angle to motion: surface tension, coriolis, centrifugal These components expressed as a formula: Fg-Fv-Ft+Fp-Fp-Fs-Fr-Fc = M * (dV/dt) Simplified to: Fg - Fv - Ft = M * (dV/dt)
26
Forces summary
- Accelerate motion: gravity, pressure gradient - Resist motion: pressure gradient, viscosity, turbulence - Right angle to motion: surface tension, coriolis, centrifugal
27
Overall forces equation
``` Including all forces expressed as a formula: Fg-Fv-Ft+Fp-Fp-Fs-Fr-Fc = M * (dV/dt) Simplified to: Fg - Fv - Ft = M * (dV/dt) (gravity, viscosity and turbulence) ```
28
Why to classify flow types
- think about which forces are more/less important in different scenarios (ex: surface tension and viscosity have bigger effect on very small flows) - helps how we go about calculating velocity and then discharge down the track
29
Laminar flow zone
consistent velocity through the profile
30
Turbulent flow zone
with a decent body of water there will be mixing between layers, water at the surface moves faster, have laminar flow at the bed
31
Boundary layer and momentum transfer time steps
1. free-stream velocity 2. free-stream enters boundary 3. transition 4. turbulent boundary layer fully developed (loss of momentum due to boundary layer, each state has a different velocity distribution/profile)
32
Free-stream velocity
No vertical gradient (no shear stress, so viscosity is not important) (no base, laminar flow)
33
Free-stream enters boundary
``` No slip property → Water next to boundary → has v=0 → boundary layer development → velocity profile development ```
34
Transition
water starts mixing, different velocities start to develop
35
Turbulent boundary layer fully developed
Water at the surface moves fastest v>0 (faster than previous time steps, water below) laminar flow only at the base (most streams/rivers!)
36
Flow classification, 2 main types:
- laminar vs turbulent | - dependent on the relative forces operating on water body
37
Flow classification 3 steps:
- relative magnitude of gravity, viscous and turbulent forces (difference) - rate of change of mean velocity or mean depth with respect to time (temporal) - rate of change of mean velocity or mean depth in downstream direction (spatial)
38
Reynolds equation
Re = VR / u R = A/P to calculate relative magnitude of forces Re <500: viscous dominates, so flow is laminar Re >500: turbulent forces dominate Re>2000: fully turbulent
39
Froude number
Fr = V/√gY what's more important gravity or turbulence Fr < 1: gravity exceeds flow velocity (wave can travel upstream) subcritical = tranquil Fr > 1: turbulent forces greater, supercritical = rapid Fr = 1: critical
40
Changes in space and time
- steady flow - uniform flow - varied flow - unsteady flow