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Presentation Fzk

Apr 08, 2018

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Hanis Aqilah
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    Heat capacity

    D E FIN IT IO N O F H E A T C A PA

    E xa m p le o f q u e stio n

    E Q U A T IO N

    H e a t ca p a city fo r certa in su b s

    u

    id is d e fin e d a s th e h e a t re q u ire d to ra ise u n it m a ss of su b sta n ce b y o n e d e g r

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    Heat capacity

    E Q U A T IO N

    E xa m p le o f q u e stio n

    D E FIN IT IO N O F H EA T C A PA C

    H e a t ca p a city fo r certa in su b s

    = ,Q H ea t su p p lied to sub stan ce= ,m M a ss o f th e su b sta n c e= ,c S p e cific h e a t ca p a city

    = .T Te m pe ra tu re rise

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    Heat capacity

    H e a t ca p a city fo r certa in su b s

    E xa m p le o f q u e stio n

    D E FIN IT IO N O F H EA T C A PA C

    E Q U A T IO N

    Specific Heat Capacities of Some

    Substances[C (J K-1 g-1 or J oC-1 g-1)]aluminiu

    mC = 0.90 water C= 4.18

    carbon C = 0.72 ethanol

    (ethylalcohol)

    C = 2.44

    copper C = 0.39 sulfuricacid(liquid)

    C = 1.42

    lead C = 0.13 sodium

    chloridesolid

    C = 0.85

    mercury C = 0.14 potassiumhydroxidesolid

    C = 1.18

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    Heat capacity

    .E xa m p le o f q u e stion

    E Q U A T IO N

    D E FIN IT IO N O F H EA T C A PA C

    H e a t ca p a city fo r ce rta in su b s

    d

    to in cre a se th e te m p e ra tu re o f 2 5 0 g o f w ater fro m 2 0 o

    C to 5 6 o

    . =C q m x C x

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    Temperature is ameasure of theaverage amount ofkinetic energypossessed by theparticles in a sampleof matter. The morethe particles vibrate,translate and rotate,the greater thetemperature of theobject.

    It is the temperaturedifference betweenthe two neighboringobjects that causesthis heat transfer. The heat transfercontinues until the

    two objects havereached thermal

    H E A T T R A N S F E R

    D e fin itio n o f te m p e ra tu r

    C o n d u ctio n

    C on v e ctio n

    R a d ia tio n

    H

    ea

    t

    tr

    an

    sf

    er

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    Conductive heatflow involvesthe transfer ofheat from onelocation toanother in theabsence of anymaterial flow.

    There isnothing

    physical ormaterialmoving fromthe hot waterto the cold

    water. Onlyenergy is

    H E A T T R A N S F E R

    C o n d u ctio n

    D e fin itio n o f te m p e ra tu r

    C on v e ctio n

    .R a d ia tio n

    H

    ea

    t

    tr

    an

    sf

    er

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    The net effect ofthese elasticcollisions is thatthere is atransfer of

    kinetic energyacross theboundary to theparticles on theopposite side.

    The more

    energeticparticles will losea little kineticenergy and theless energeticparticles willgain a littlekinetic energy

    H E A T T R A N S F E R

    C o n d u ctio n

    D e fin itio n o f te m p e ra tu r

    C on v e ctio n

    .R a d ia tio n

    H

    ea

    t

    tr

    an

    sf

    er

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    In conduction,there is no nettransfer ofphysical stuffbetween the

    objects. Nothingmaterial movesacross theboundary. Thechanges intemperature are

    wholly explainedas the result ofthe gains andlosses of kineticenergy duringcollisions.

    Heat transfer

    H E A T T R A N S F E R

    C o n d u ctio n

    D e fin itio n o f te m p e ra tu r

    C on v e ctio n

    .R a d ia tio n

    H

    ea

    t

    tr

    an

    sf

    er

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    Convection is theprocess ofheat transferfrom onelocation to thenext by themovement offluids.

    The moving fluidcarries energywith it. Thefluid flowsfrom a hightemperaturelocation to a

    lowtemperature

    H E A T T R A N S F E R

    .C on v e ctio n

    C o n d u ctio n

    D e fin itio n o f te m p e ra tu r

    R a d ia tio n

    H

    ea

    t

    tr

    an

    sf

    er

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    Radiation is the transferof heat by means ofelectromagneticwaves. To radiatemeans to send out orspread from a central

    location.

    All objects radiate energyin the form ofelectromagneticwaves. The rate atwhich this energy is

    released isproportional to theKelvin temperature(T) raised to thefourth power.

    Radiation rate = kT4

    H E A T T R A N S F E R

    .C on v e ctio n

    C o n d u ctio n

    D e fin itio n o f te m p e ra tu r

    R a d ia tio n

    H

    ea

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    tr

    an

    sf

    er

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    The energy radiated froman object is usually acollection or range ofwavelengths. This isusually referred to asan emission spectrum

    Hotter objects tend to

    emit shorterwavelength, higherfrequency radiation

    Thermal radiation is aform of heat transferbecause theelectromagneticradiation emittedfrom the sourcecarries energy awayfrom the source tosurrounding (ordistant) objects. Thisenergy is absorbed by

    those objects, causingthe average kineticenergy of their

    H E A T T R A N S F E R

    .C on v e ctio n

    C o n d u ctio n

    D e fin itio n o f te m p e ra tu r

    R a d ia tio n

    H

    ea

    t

    tr

    an

    sf

    er