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12.1 notes.notebook 1 April 03, 2017 Temperature and Thermal Energy thermodynamics: the study of heat caloric theory: early theory of TE honolulu.hawaii.edu An incorrect theory which serves as a model for scientific growth anguage retains vestiges of concept heat flows, objects soak up heat leads to confusion: we speak of it as a substance while told that it is not metaphor Lavoisier coined the term later in 1787 firmly entrenched by 1780 largely discredited by 1850 conservation of heat was a basic premise heat lost by one object is gained by another this is true and still a basis for calorimetry heat was thought of as a substance fluid = can flow a fluid called caloric Properties of Caloric could not be created nor destroyed all substances contain caloric and absorb or release it flows from hot to cold objects or substances counterbalanced attractive forces of "particles of matter" self repulsion caused it to flow from higher to lower concentration kind of like pressure in a balloon state of matter determined by amount of caloric caloric surrounds the particles of matter causing them to swell caloric occupied space, so gas has lots of caloric KineticMolecular Theory 1) All matter is made up of particles in constant motion with elastic collisions (KE = KE') 2) The: >motion >KE > Temperature bonds: electromagnetic forces particles vibrate back and forth (KE) intermolecular bond resist vibration , therefore particles have PE (elastic/electric) overall energy is called Thermal Energy http://hyperphysics.phyastr.gsu.edu/hbase/acloc.html atomic clock

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Page 1: 12.1 notes.notebook - Wisconsin Lutheran High Schoolgreschner.wiscoscience.com/worksheets/physics/chpt 12/12... · 2017. 4. 3. · Title: 12.1 notes.notebook Subject: SMART Board

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April 03, 2017

Temperature and Thermal Energythermodynamics: the study of heat

caloric theory: early theory of TE

honolulu.hawaii.edu

An incorrect theory which serves as a model for scientific growth  anguage retains vestiges of concept     heat flows, objects soak up heat     leads to confusion:  we speak of it as a substance while told that it is not      metaphor    Lavoisier coined the term later in 1787      firmly entrenched by 1780    largely discredited by 1850 conservation of heat was a basic premise

heat lost by one object is gained by another this is true and still a basis for calorimetry 

heat was thought of as a substancefluid = can flow a  fluid  called caloric 

Properties of Caloriccould not be created nor destroyed all substances contain caloric and absorb or release it flows from hot to cold objects or substances counterbalanced attractive forces of "particles of matter" self repulsion caused it to flow from higher to lower concentration kind of like pressure in a balloon 

state of matter determined by amount of caloriccaloric surrounds the particles of matter causing them to swell caloric occupied space, so gas has lots of caloric

Kinetic­Molecular Theory1)  All matter is made up of particles in constant motion with elastic collisions

    (KE = KE')

2)  The:   >motion >KE > Temperature

bonds: electromagnetic forces

­particles vibrate back and forth (KE)­intermolecular bond resist vibration , therefore            particles have PE (elastic/electric)overall energy is called Thermal Energy

http://hyperphysics.phy­astr.gsu.edu/hbase/acloc.html

atomic clock

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http://lectureonline.cl.msu.edu/~mmp/kap10/cd283.htm

http://mc2.cchem.berkeley.edu/Java/molecules/index.html

Temperature:  measures "hotness" of an object.  Temperature is a measure   of the average energy (KE) of the particles of an object.

https://www.youtube.com/watch?v=v12xG80KcZw

https://www.youtube.com/watch?v=dHJmOH38agY

states of water

Thermal Energy:  total PE + KE associated with the random motion and arrangement of the particles of a material  (Total Internal Energy)Heat: Thermal Energy that's absorbed, given up, or transferred from one body to another.                 Flowing of TE      (thermal contact)

Temperature: physical quantity that is proportionate to the average (translational)          KE of the particles in matter.

­ a measure of a body's ability to give up or absorb TE from another body

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Can't measure KE (motion) directly, so we measure its effect on something else.

         (indirect measurement)

> temp >motion > volume

> temp        >volume

> temp > electrical resistance to current

> temp      > resistance

Temperature Scales

Fahrenheit ­ based on body temperature/brine(Rankine)

Celsius ­ based on freezing and boiling of water

Kelvin ­ based on "absolute zero"

C = (F ­ 32) /1.8 or 5/9(F ­ 32)  F = (C x 1.8) + 32 or 9/5C + 32K = C + 273

http://en.wikipedia.org/wiki/Absolute_zero

http://en.wikipedia.org/wiki/Fahrenheit

http://en.wikipedia.org/wiki/Celcius

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When converting between C and F180 is the magic number using boilingof water

F  CC = 5/9(F ­ 32)  or (F ­ 32) /1.8

F = 9/5C + 32  or (C x 1.8) + 32

212o F = ____o C212o F ­ 32 = 180                        180/1.8 = 100oC

C    F 

100o C= ____o F100o C x 1.8 = 180                        180 + 32 = 212o F

 100F  = _________0C

280C = __________0F 

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100F  = _________0C

280C = __________0F 

C =  (F ­ 32) /1.8C = (100F ­ 32)/1.8C = ­120C

F = (C x 1.8) + 32F = (280C x 1.8) + 32F = 820 F

 820F  = _________0C

380C = __________0F 

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820F  = _________0C

380C = __________0F 

C =  (F ­ 32) /1.8C = (820F ­ 32)/1.8C = 280C

F = (C x 1.8) + 32F = (380C x 1.8) + 32F = 1000 F

 520F  = _________0C

880C = __________0F 

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520F  = _________0C

880C = __________0F 

C =  (F ­ 32) /1.8C = (520F ­ 32)/1.8C = 110C

F = (C x 1.8) + 32F = (880C x 1.8) + 32F = 1900 F

Thermal Energy Transfer

conduction

convection

radiation

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If you put a metal bar into a flame, it gets hot quickly. Soon you can't hold it. If you put a glass bar into a candle, it won'tget too hot to hold. But if you touched the end that was in the flame, you would find that it was really hot!The process in which heat passes through a solid substance is called conduction. Metals are good conductors of heat. Non‐metals are generally bad conductors of heat. Liquids and gases are bad conductors of heat as well. A bad conductor of heat is called an insulator. Your quilt, or winter jacket, traps air which is a good insulator.

conduction

ConvectionConvection occurs only in liquids and gases. We call liquids and gases fluids. It cannot happen in solids. It needs particles to be free to move about. When a liquid is heated, the molecules at the bottom move about with bigger vibrations. They take up more space which means that the density goes down. The less dense fluid rises. It gives its energy to the fluid above, and cools down. It becomes denser and falls back to the bottom. A convection current is set up.

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RadiationRadiation passes heat on as an electromagnetic wave called infra‐red radiation. All the heat from the Sun reaches us as electromagnetic radiation. Our eyes cannot see infra red, but a digital camera can. Here is a picture of a hot plate that appears much brighter than it actually is because of the infra red radiation.

"hot" plate

E = W = Fd

KE = ½mv2

PE = mgh

Q = mcΔtthermal energy

            Note the similarities to the other forms of energy!!!!... amounts ... unique properties of that form of energy ... what's changing ...       mass     g or c v, h, or t

"g" is unique to superior                                                          object ... [ g = Gm1/r2 ]  all object attract all other objects and each has their own "g" value

"c" is unique to molecular/atomic make­up of an                                                          object ... [ c = Q/m∆t ]  all object 

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Specific Heat

Q = mcΔt

specific heat"thermal property of matter"

c = Q/mΔt           c = J/(kg0C)TE kg 10 C

the thermal energy needed to change l kg     of a substance 1 degree C

"c" is 

How much TE does it take to raise 100.g of iron from 170 C to 100.o C?

iron

TE = ?mi = 100 g

0.100 kgt1 = 170Ct2 = 1000C

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How much TE does it take to raise 100.g of iron from 170 C to 100.o C?TE = ? (Q)mi = 100 g

0.100 kgt1 = 170Ct2 = 1000C

Q = mcΔtQ = mc(tf ­ ti)Q = .100 kg[450 J/(kg0C)](100.0C ­ 170C)Q = .100 kg[450 J/(kg0C)](100.0C ­ 170C)Q = 3700 J

PE = mgh = (kg)m/s2(m) = N x m = J

TE = Q = mcΔt = kg[J/(kg0 C)] 0C  = J

c = Q/mΔt = J/(kg0 C)some common "c" valuestext page 279  (eachtextbook will listslightly differentvalues for "c"

copper   385 J/kg0CH20 4180 J/kg0Cmetal   450 J/kg0Clead        135 J/kg0Cice   2060 J/kg0Csteam 2020 J/kg0C

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  QL + Qg = 0Qlost + Qgained = 0

Law of Heat Exchange

100 g of metal at 100.0C100 g of H20 at 600C   mix them together!

Temp

Time

1000C

600C

tim

tiw

tfmtfw

tf

QL

Qg

tfm = ffw = tf

Steel loses TE because 

it's at a higher temperature

Water gains TE because 

it's at a lower temperature remember the inelastic collision when v1' = v2' = v'

thermal equilibrium

100 g of steel at 1000C100 g of water at 600C

What is the final temperature?QL + Qg = 0mcΔts + mcΔtw = 0mc(tf ­ ti)s + mc(tf ­ ti)w = 0(mctfs ­ mctis) + (mctfw ­ mctiw) =0

mcstf ­ mctis + mcwtf ­ mctiw =0mcstf  + mcwtf = mctis + mctiwtf(mcs + mcw) = mctis + mctiwtf = mctis + mctiw          mcs + mcw tf = .1kg(450J/kgC)1000C + .1kg(4180J/kgC)600C

   [.1kg(450J/kgC)] + [.1kg(4180J/kgC)]tf = 4500 J + 25100 J            463J/0Ctf = 63.90C

QL + Qg = 0mcΔts + mcΔtw = 0mc(tf ­ ti)s + mc(tf ­ ti)w = 0

[.1kg(450J/kgC)(63.90C ­ 1000C)] + [.1kg(4180J/kgC)(63.90C ­ 600C)] = 0 ­1625 J + 1630 J = 0   slightly off because of rounding

you mix:

is tfs = tfw ? ...YES, ∴ tfs = tfw = tfadd "mcti" 's from both sides 

expand Δt's

factor out the "mc" 's

divide by "mc" 's

dist. steel

water600C

tf = 63.90C

1000C

QLs  = ­1625 J 

Qgw = ­1630 J 

note the "­" denotes loss of TE

      and "+" denotes gain of TE

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steel

water600C

tf = 63.90C

1000C

QLs  = ­1625 J 

Qgw = ­1630 J 

tis = 1000C

tiw = 600C