Understanding Gas Pressure and Atmospheric Pressure

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    UNDERSTANDING GASPRESSURE &

    ATMOSPHERIC PRESSURE

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    Gas Pressure

    200 kPa 500 kPa 400 kPa 1100 kPa+ + = ? kPa

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    Gas Pressure

    The gas pressure in a

    container is caused bythe collision of gas

    molecules with the wallof the container.

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    How to measure gas

    pressure?

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    Bourdon Gauge

    Bourdon gauge(consists of a semi-

    circular or C-shapedcopper tube thattends to straighten ifmore and more gas

    is pumped(compressed) intoit).

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    Manometer

    Manometer (consistsof a U-tube about 1

    m in height. About50% of the volumeof the U-tube is filledwith liquid such as

    mercury or water).

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    ManometerWith both legs of a U-tube

    manometer open to the

    atmosphere or subjected to the

    same pressure, the liquidmaintains the same level in

    each leg, establishing a zero

    reference.

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    Manometer

    With a greater pressureapplied to the left side ofa U-tube manometer, theliquid lowers in the left legand rises in the right leg.

    The liquid moves until theunit weight of the liquid,as indicated by h, exactlybalances the pressure.

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    Manometer

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    A manometermeasures thepressure of agas in acontainer

    Gas pressureis the forceexerted by thecollisions of

    gas particleswith a surface

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    Variations on the U-Tube Manometer

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    ATMOSPHERIC PRESSURE

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    Earths Atmosphere

    About 10 kmthick

    Consists mostlyof molecularnitrogen (N2)

    and oxygen (O2)

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    The air is made up of molecules.

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    Gravity pulls the air

    molecules toward the earth,

    giving them weight. Theweight of the air molecules all

    around us is called the

    atmospheric pressure.The atmospheric pressure is

    caused by the downward

    force exerted by the air, or theweight of the atmosphere on

    the Earths surface.

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    1 atmosphere = 76 mm Hg = 10 mwater = 1.0 x 105Pa

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    High altitudes = lower pressure

    Low altitudes = higher pressure

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    The greater altitude from the sea level,the smaller the atmospheric pressure.

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    INSTRUMENTS FORMEASURING ATMOSPHERIC

    PRESSURE

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    to

    measure

    airpressure.

    A Barometer

    is

    used

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    The AneroidBarometer

    No fragile tubes!

    No toxic chemicals!

    No batteries!

    Never needs winding!

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    An aneroid barometer

    uses a cell which has

    had most of the airremoved.

    As the air pressure

    around the cell

    increases, it presseson the cell, which

    causes the needle to

    move.

    MILLIBARS

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    In 1643, Evangelista Torricelli

    invented the barometer

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    Torricellis barometer

    used a glass column

    suspended in a bowl of

    mercury. The pressure

    of the air molecules

    pushed the mercury upinto the glass tube.

    The weight of the mercury in

    the tube was equal to the

    weight of the air pressing

    down on the mercury in the

    dish.

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    Asatmospheric

    pressure

    increases

    The mercury in

    the tube rises.

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    The Mercury Barometer

    Good: Bad:

    Simple to construct

    Highly accurate

    Glass tube is fragile

    Mercury is verytoxic!

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    Example 1:

    The atmospheric pressure is 760 mm Hg. What

    is the value of the atmosphericpressure inPascal?

    [ Density of mercury, (Hg) = 13 600 kg m-3 ]

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    Changing Pressure

    A rising barometer= increasing air pressure.

    This usually means:

    Rising barometer readings indicate that a

    high pressure system is approaching.Higher atmospheric pressure is usuallyassociated with fair weather and clearingskies.

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    Changing Pressure

    A falling barometer= decreasing air pressure.

    This usually means:

    Falling barometer readings usuallyindicate the approach of an area of

    low pressure. Low pressure readingsare usually associated with stormsystems. Tornadoes and hurricanescan produce very low barometricreadings.