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Heat

Specific Heat Capacity of Common Materials
Substance
(@15C unless noted)
Phase Specific Heat,
cp J/(g·K)
Air gas 1.004-1.012
Aluminium solid 0.897
Ammonia liquid 4.700
Argon gas 0.520
Asphalt solid 0.920
Brick solid 0.840
Carbon dioxide CO2 gas 0.839
Concrete solid 0.880
Copper solid 0.385
Diamond solid 0.509
Ethanol liquid 2.440
Glass solid 0.5-0.9
Gold solid 0.129
Granite solid 0.790
Graphite solid 0.710
Gypsum solid 1.090
Helium gas 5.193
Hydrogen gas 14.300
Iron solid 0.450
Lead solid 0.127
Lithium solid 3.580
Magnesium solid 1.020
Marble solid 0.880
Mercury liquid 0.140
Nitrogen gas 1.040
Oxygen gas 0.918
Paraffin solid 2.500
Polyethylene solid 2.303
Sand solid 0.835
Silica (fused) solid 0.703
Silver solid 0.233
Soil solid 0.800
Tin solid 0.227
Tissue (animal) mixed 2.900
Tungsten solid 0.134
Water @−10 °C solid 2.050
Water @100 °C gas 2.080
Water @25°C liquid 4.181
Wood solid 1.2–2.3
Zinc solid 0.387

Heat

Heat is thermal energy stored as kinetic energy and as potential energy in the modes of vibration. Heat flow is denoted by the letter Q.

Temperature

Temperature (T) is a measure of the average total kinetic energy of particles in matter.

Specific Heat Capacity

Specific heat capacity is the measure of heat required to increase the temperature of a given amount of a material. Specific heat generally changes with temperature. As the temperature approaches absolute zero, the specific heat capacity of a system also approaches zero. Specific heat capacity is normalized by the material's mass so is independent of the quantity of substance.

Q = m cp(Thi-Tlo)


Thermal Mass

The total heat capacity of a sample is the mass times the specific heat. It measures how much thermal energy can be stored in an object.

C= m cp


This is also known as the thermal mass, and is a way of absorbing and storing heat, or damping temperature fluctuations. Objects with higher thermal mass will store more energy for each degree of temperature change.

Heat Transfer

Heat transfer is the flow of thermal energy from a hotter region to a cooler region. When an object is at a different temperature than its surroundings or another object, transfer of thermal energy occurs in such a way that the body and the surroundings reach thermal equilibrium; this means that they are at the same temperature. Heat transfer always occurs from a higher-temperature object to a cooler-temperature one as described by the second law of thermodynamics. The transfer mechanism is mediated through conduction, convection, and/or radiation.

Conduction is the transfer of kinetic energy from particle to particle and is the primary mechanism for heat transfer within solid materials.

Q= (Thi-Tlo)
(L k A)


Convection is the transfer of heat energy by particles physically moving from one location to another.

Q= (Tsurf-Tenv)
(hconv Asurf)


Radiation is the transfer of heat energy through empty space.

Q= (Tsurf-Tsurr
(hr Asurf)

















Created by admin. Last Modification: Friday 09 of April, 2010 08:51:19 GMT-0000 by admin.