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Fluids

Physics, Chapter 10

by Giancoli

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First, a few reminders:

  • atomic mass unit (u) - based on setting carbon-12 equal to 12.000 00 u
  • Avogadro’s number
    • = 6.022 x 1023 particles/mol
  • STP = 0°C at 1 atm
  • D = m/V (in Physics we use ρ = m/V)
  • 1 g/cm3 = 1000 kg/m3 = density of H2O
  • atoms of every kind are nearly the same size (diameter = ~0.1-0.3 nm)

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Liquids as fluids

  • fluid = able to flow
  • viscosity - internal resistance or friction offered to an object moving through a fluid
  • ideal liquids are incompressible and nonviscous
    • real liquids, of course, are slightly compressible and their viscosity varies significantly

  • water is considered “nonviscous” because its particles are so small

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Gases as fluids

  • the density of our atmosphere at sea level is around 1/800th that of H2O
  • each square inch of exposed surface at sea level is struck by 2 x 1024 air molecules per second!
  • at STP, there are approx. 3 x 1019 molecules of air per cubic centimeter
    • that’s around 3 nm per air particle (10 times its radius)
    • each air particle travels at ~450 m/s and has ~6 x 109 collisions per second
    • actual speed depends on air temperature

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Pressure

  • pressure is defined as the scalar value of the force acting perpendicular to, and distributed over, a surface divided by the area of that surface
  • in other words:
    • P = F / A
  • pressure is measured in Pascals
  • 1 Pa = 1 N/m2
  • Pascals are so small that we often use kiloPascals (kPa)
  • “standard pressure”:
    • 1 atmosphere
    • 101,300 Pa
    • 101.3 kPa

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Direction of pressure

  • the force exerted by a fluid at rest acting on any rigid surface is always perpendicular to that surface
  • fluids exert pressure equally in all directions
  • gravity is the ultimate cause of hydrostatic pressure
    • imagine a column of fluid over an object in that fluid

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Pressure equations

or, how we get from P = F / A to Pl = ρgh

Fw = mg

and

ρ = m / V

so:

m = ρV

which means:

Fw = ρVg

which we can plug into:

P = F / A

to make:

P = ρVg / A

since

V = area * height

this means A & V cancel, so:

Pl = ρgh

(because the density of ideal liquids is nearly uniform, use subscript l)

and taking surface pressure into account:

P = Ps + Pl

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“The Hero of Haarlem”

  • a Dutch folk tale tells of a boy named Hans who held back the North Sea by sticking his finger in a hole in a dike that was leaking
  • he really could have done it because Pl = ρgh only relies on depth and density of liquid, not volume
  • pressure is independent of shape of vessel

  • pressure at every point at a given horizontal level in a single body of fluid at rest is the same!