Mass Density - General Physics I - Lecture Slides, Slides of Physics

The fundamental aspects of these Lecture Slides are : Mass Density, Continuous Piece, Liquid, Solid, Occupies, Dimensionless Measure, Specific Gravity, Ratio, Substance, Pressure

Typology: Slides

2012/2013

Uploaded on 07/26/2013

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A small, continuous piece of a
substance (solid, liquid or gas) of
mass ΔM occupies a volume ΔV.
Its mass density ρ is given by
the quotient !!
ρ = ΔM / ΔV .!
A dimensionless measure of
density, the specific gravity, is
the ratio of the density of an
object or substance (labeled X)
with respect to water ρX /ρwater.!
mass density!
Source: Undetermined
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A small, continuous piece of a substance (solid, liquid or gas) of mass Δ M occupies a volume Δ V.

Its mass density ρ is given by

the quotient

ρ = Δ M / Δ V.

A dimensionless measure of density, the specific gravity , is the ratio of the density of an object or substance (labeled X)

with respect to water ρ

X

water

mass density

Source: Undetermined

Collisions of particles (molecules or atoms) within a gas or liquid generate a force against a surface that is in contact with it. Fun Facts about air molecules: (77% nitrogen, 21% oxygen, 1-2%water, 1% other)

  • typical speed v = 450m/s (1000 mi/hr!)
  • travel 8x10–8^ m between collisions with another molecule
  • 6 billion collisions per second on each square inch of your skin

pressure

Gravity is the ultimate cause of hydrostatic pressure. Hydrostatic refers to non-accelerating fluids, particularly fluids at rest. Just as a stack of bricks must be strong enough to support its own weight, so the pressure in a fluid must vary with depth, so that the fluid below can support the weight of the fluid above.

A distance h below the surface of a liquid with density ρ, the

pressure is increased from the surface value by an amount

Δ P = ρ g h.

What we measure as atmospheric pressure is merely the weight per unit area of the column of atmosphere extending upward from the Earth’s surface. It is often quoted in terms of the equivalent height of a column of mercury (specific gravity =13.6)

1 atmosphere = 101 kPa = 760 mm (29.92 in)

hydrostatic pressure and gravity

For a description of historical experiments on pressure and fluids, see http://galileo.imss.firenze.it/vuoto/eesper.html Otto von Guericke completed, around 1655, a pump which could extract the air from air-tight containers. With this new instrument, von Guericke was able to perform, at Magdeburg, in 1657, a spectacular experiment with the aid of a large number of his townsfolk. He demonstrated that the weight of air pushed together two perfectly sealed hemispheres, which had a vacuum created between them by the pneumatic pump, with such force that it needed two teams of 16 horses to separate them. Von Guericke understood that the weight of air was a force which could be put to work, to lift weights, for example. He thus initiated a line of research which led to the steam engine of James Watt (1736-1819) Source: Gaspar Schott, Mechanica hydraulico-pneumatica, Würzburg 1657

Pascal’s Principle

This concept is the basic operating principle of all hydraulic equipment. An external pressure applied to a fluid within a closed container is transmitted undiminished throughout the entire fluid. CC: BY-NC timailius (flickr) http://creativecommons.org/licenses/by-nc/2.0/deed.en CC: BY-NC-SA s__I (flickr) http://creativecommons.org/licenses/by-nc-sa/2.0/deed.en

Archimedes’ Principle

A small section within a fluid feels a higher pressure on its bottom than on its top. This difference in pressure produces an upward bouyant force

• F

b

= Δ P A

• = (ρ g h ) A = ρ V g

• = m

f

g

( m f is the mass of the displaced fluid) The magnitude of the buoyant force depends only on the mass of displaced fluid m f and is independent of the object’s geometry.

Objects immersed in a fluid at rest experience a buoyant force F

b directed against gravity with magnitude equal to the weight of the fluid displaced by the object.

You sit in a boat on a man-made lake filled with a fixed volume of water. Accompanying you is the pair of large rocks from the momentum chapter. This time, instead of throwing the rocks sideways, you drop them over the side and let them sink into the water. What happens to the water level of the lake after the rocks have sunk to the bottom?

1) It goes up.

2) It goes down.

3) It stays the same.

You place a small beaker of water on a scale and notice

that its weight is 300g. If you now push your finger into

the water, what happens to the reading on the scale?

1) It increases.

2) It decreases.

3) It stays the same.