Lecture 7-River Dynamics 1 Flashcards
Hydraulics of river flow equation
Q=Av=wdv
Q = discharge
A = area (width x depth)
v = average velocity
What determines the flow velocity?
Fluid mechanics (all the forces that are pushing, pulling and acting on water)
Why are rivers important to study in a hydrological sense?
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)
When does flow occur:
fluid subjected to mechanical potential energy gradient
- gravity (gravitational potential energy)
- hydrostatic pressure (hydrostatic potential energy)
mechanical potential energy gradient (break it down)
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
gravity (force)
- 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
hydrostatic pressure (force)
- 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 - Direction:
- at any point, pressure is equal in all directions (only determined by weight above)
other forces retard flow or alter course due to (1):
boundary conditions
Force formula
Force = mass x acceleration (operate as a point)
Force formula
Force = mass x acceleration (operate as a point)
where:
Acceleration = dV / dt (change of velocity over change of time)
Hydrostatic potential energy formula
Epp = 𝛄By
Epp = Potential energy of hydrostatic pressure
where y = vertical distance from the surface
Gravitational potential energy formula
Epg = 𝛄Bz Epg = Potential energy gradient 𝛄 = weight density B = volume z = height above datum
Potential energy formula
Ep = Epg + Epp
basically add together hydrostatic potential energy + gravitational potential energy
Forces in open-channel flows:
- 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 •
Forces in open-channel flows:
- 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 •
Hydrostatic pressure gradient formula
Fp / M = g⧍Y / X
Y=depth
X = distance between them
(can act in either direction)
Frictional forces
-Viscosity
Frictional forces
- Viscosity
- Turbulence
Viscosity
-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
—————–>
————–>
———–>
——–>
—–>
–>
__________
Turbulence
- related to eddy viscosity
- depends on the characteristics of the flow (depth and velocity)
Minor forces that happen perpendicular to flow
- surface tension
- centrifugal
- coriolis
Surface tension
- pull on water as it tries to keep bonded together
- only significant in very small water volumes
Centrifugal
- related to curvature of the path
- when going around a bend, will change speed and trajectory
Coriolis
- related to rotation of the earth
- left is S. Hemisphere, right in N. Hemisphere