Thermodynamics

Laws

0.

1.

2.

3.

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Thermal equilibrium

Energy conservation

ΔInternal energy = ΔW+ΔQ

Entropy

System disorder

More disorder ↑ entropy

ALWAYS ↑ overall

Absolute zero

Impossible to reach

w/ finite steps

Temperature, kinetic

Kinetic

Temperature

R/ w/

Particle model

All matter

particles

constant motion

have kinetic energy

collisions btw/ elastic

potential energy

depends

distance between particles

stored in

springs connecting particles

Particles

solids

bound

liquids

loosely bound

gases

bonds broken

energy possessed

body

due to motion

Avg.

Random kinetic energy

particles in a body

heated material

avg. kinetic energy ↑

material heated

+heat energy added

increase proportion

vibrating atoms

∴ temp ↑

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2 substances mixed

heat gain/loss =

result

same temp

particles

heat

amount balanced

still collide

Specific heat capacity

Heat capacity

ratio

required heat (Q)

for ΔT

physical property

structure

Energy required

↑T

1kg by 1°C

w/out phase change

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Same energy input

1/2 mass ↑Tx2

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c

SHC

ΔQ

m

mass

ΔT

Units

body heated

substance heated

quantity

energy supplied

Δ temperature

joules/kg/kelvin

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Energy transfer models

Heat energy

moves

region high T

to low

Convection

Also 'thermals'

Conduction

Radiation

Heat transfer

Particle collision

no net movement

particles

Hotter further vibrate

collisions

energy transfer

Thermal conductivity

energy flow/ second

area 1sqm

thickness 1m

per °T

difference between

material ends (2)

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Units

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Heat conductors

Solids best

heat insulators poor

Calculations

Energy/second

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Temperature difference

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Flow

Hot to cold

final value ↓ initial

∴ always -

Final Equation

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Symbols

Energy change

ΔQ

Always -

Area (variable)

A

Distance travelled

d

Thermal conductivity

k

Must be specified

different each substance

∵ physical structure

cause

T difference

between air masses

Heat energy

transfer

via

bulk particle movement

particle flow

away

warmer to cooler

current produced

Fluids ONLY

Heated expand

less dense

more buoyant

cold contract

more dense

less buoyant

float

sink

occur

warm & cold

fluid masses intersect

atmosphere

oceans

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Rate

affected by

T difference

between

heat source

convective fluid

Effectiveness

heat transfer

dependant

heat source placement

mass movement

particles

w/in a system

distance

Can be considerable

does not

involve particles

need a medium

Electromagnetic radiation

all objects emit

except at 0K

Source

moving charged particles

faster movement, hotter substance

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occurs through

electromagnetic waves

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