Heat Capacity
Heat Capacity
Some materials require more energy to be added or removed for the same temperature change as other materials. This property is call heat capacity.
Note that large objects (an ocean being warmed by climate change) can store lots of energy for a small change in temperature. Also note that for equal masses, some materials require less energy for a change in temperature. To understand this we use the terms intensive and extensive.
Intensive vs Extensive Properties
Intensive or bulk property
Does not depend on the amount of material
Example: temperature, density
Extensive property
Depends on the amount of material
Example: mass, volume
Heat Capacity
When heat moves from one material to another one temperature rises the other falls
The temperature rise occurs as heat increases the motion of atoms in the material
The rate of change in temperature with added energy is dictated by the heat capacity
Ratio of heat added to temperature change
Heat Capacity
Extensive property (of the material and the amount)
Measured in Joules per degree Kelvin
Specific Heat Capacity
Intensive property (of the material only)
Measured in Joules per mass per degree Kelvin
Table of Specific Heat Values
Partial list from https://en.wikipedia.org/wiki/Heat_capacity
Heat capacity
We have an equation that tells us how the energy absorbed by a material is related to the temperature rise.
Units
In metric units
energy is in joules
mass is often in grams
specific heat is often in joule/gram/Kelvin
the temperature difference is in Kelvin or Celsius
In english units
energy is in BTU
mass is in lbs
specific heat is in BTU/lb/Fahrenheit
the temperature difference is in Fahrenheit
Energy required for tea
How much energy does it take to make a cup of tea? Assume the water starts at 20C and is raised to 95C for a delta T of 75C. Further assume that there is 200 ml of water (200 grams).
Relation to Buildings
Thermal mass is added to a building to store heat
Cool or warm air is passed through a building to deliver or remove heat.
Relation to Weather and Climate
The heat capacity of water affects the climate in some areas
Rate of increase
If we have a source of constant thermal power and assume that all that energy is going into an object, we can calculate the rate of temperature rise of that object.
We divide both sides by time.
Remember that Q is an energy. That means Q over t is a power.
If we rearrange this equation algebraically, we see that
This means that the power divided by the heat capacity gives you an estimate of the rate of temperature increase in an object.
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