Specific heat ratio: Difference between revisions
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== Definitions of specific heat and heat capacity == | == Definitions of specific heat and heat capacity == | ||
The ''specific heat'' (or ''specific heat capacity''), is the amount of heat energy required to increase the temperature of a unit quantity of a substance by a certain temperature interval. For example, the heat required to raise the temperature of water by 1 [[Kelvin (unit)|kelvin]] is 4.184 [[Joule (unit)|joule]]s. The specific heat capacity is usually expressed as Jg<sup>-1</sup>K<sup>-1</sup>. It may also be expressed on a molar basis as Jmol<sup>-1</sup>K<sup>-1</sup>. | The ''specific heat'' (or ''specific heat capacity''), is the amount of heat energy required to increase the temperature of a unit quantity of a substance by a certain temperature interval. For example, the heat required to raise the temperature of 1 gram of water by 1 [[Kelvin (unit)|kelvin]] is 4.184 [[Joule (unit)|joule]]s. The specific heat capacity is usually expressed as Jg<sup>-1</sup>K<sup>-1</sup>. It may also be expressed on a molar basis as Jmol<sup>-1</sup>K<sup>-1</sup>. | ||
The ''heat capacity'' (as distinct from ''specific heat'') is the amount of heat energy required to increase the temperature of a substance by a certain temperature interval. Heat capacity is an extensive property because its value is proportional to the amount of the substance. For example, a kilogram of water has a greater heat capacity than 100 grams of water. The heat capacity is usually expressed as JK<sup>-1</sup>. | The ''heat capacity'' (as distinct from ''specific heat'') is the amount of heat energy required to increase the temperature of a substance by a certain temperature interval. Heat capacity is an extensive property because its value is proportional to the amount of the substance. For example, a kilogram of water has a greater heat capacity than 100 grams of water. The heat capacity is usually expressed as JK<sup>-1</sup>. |
Revision as of 13:24, 9 April 2009
Specific heat ratio of various gases[1][2][3] | ||||||
---|---|---|---|---|---|---|
Gas | °C | k | Gas | °C | k | |
H2 | −181 | 1.597 | Dry Air |
20 | 1.40 | |
−76 | 1.453 | 100 | 1.401 | |||
20 | 1.41 | 200 | 1.398 | |||
100 | 1.404 | 400 | 1.393 | |||
400 | 1.387 | CO2 | 0 | 1.310 | ||
1000 | 1.358 | 20 | 1.30 | |||
2000 | 1.318 | 100 | 1.281 | |||
He | 20 | 1.66 | 400 | 1.235 | ||
N2 | −181 | 1.47 | NH3 | 15 | 1.310 | |
15 | 1.404 | CO | 20 | 1.40 | ||
Cl2 | 20 | 1.34 | O2 | −181 | 1.45 | |
Ar | −180 | 1.76 | −76 | 1.415 | ||
20 | 1.67 | 20 | 1.40 | |||
CH4 | −115 | 1.41 | 100 | 1.399 | ||
−74 | 1.35 | 200 | 1.397 | |||
20 | 1.32 | 400 | 1.394 |
The specific heat ratio of a gas is the ratio of the specific heat at constant pressure, , to the specific heat at constant volume, . It is sometimes referred to as the adiabatic index or the heat capacity ratio or the isentropic expansion factor.
Either (Roman letter k), (gamma) or (kappa) may be used to denote the specific heat ratio:
where:
- = the specific heat of a gas
- = refers to constant pressure conditions
- = refers to constant volume conditions
Ideal gas relations
For an ideal gas, the heat capacity is constant with temperature. Accordingly we can express the enthalpy as and the internal energy as . Thus, it can also be said that the specific heat ratio of an ideal gas is the ratio between the enthalpy to the internal energy:[3]
The specific heats at constant pressure, , of various gases are relatively easy to find in the technical literature. However, it can be difficult to find values of the specific heats at constant volume, . When needed, given , the following equation can be used to determine :[3]
where is the molar gas constant (also known as the Universal gas constant). This equation can be re-arranged to obtain:
Relation with degrees of freedom
The specific heat ratio ( ) for an ideal gas can be related to the degrees of freedom ( ) of a molecule by:
Thus for a monatomic gas, with three degrees of freedom:
and for a diatomic gas, with five degrees of freedom (at room temperature):
- .
Earth's atmospheric air is primarily made up of diatomic gases with a composition of ~78% nitrogen (N2) and ~21% oxygen (O2). At 20 °C and an absolute pressure of 101.325 kPa, the atmospheric air can be considered to be an ideal gas. A diatomic molecule has five degrees of freedom (three translational and two rotational degrees of freedom, the vibrational degree of freedom is not involved except at high temperatures). This results in a value of:
which is consistent with the value of 1.40 listed for oxygen in the above table.
The specific heats of real gases (as differentiated from ideal gases) are not constant with temperature. As temperature increases, higher energy rotational and vibrational states become accessible to molecular gases, thus increasing the number of degrees of freedom and lowering .
For a real gas, and usually increase with increasing temperature and decreases. Some correlations exist to provide values of as a function of the temperature.
Isentropic compression or expansion of ideal gases
The specific heat ratio plays an important part in the isentropic process of an ideal gas (i.e., a process that occurs at constant entropy):[3]
- (1)
where, is the absolute pressure and is the volume. The subscripts 1 and 2 refer to conditions before and after the process, or at any time during that process.
Using the ideal gas law, , equation (1) can be re-arranged to:
- (2)
where is the absolute temperature. Re-arranging further:
- (3)
we obtain the equation for the temperature change that occurs when an ideal gas is isentropically compressed or expanded:[3][4]
- (4)
Equation (4) is widely used to model ideal gas compression or expansion processes in internal combustion engines, gas compressors and gas turbines.
Determination of values
Values for are readily available, but values for are not as available and often need to be determined. Values based on the ideal gas relation of are in many cases not sufficiently accurate for practical engineering calculations. If at all possible, an experimental value should be used.
A rigorous value can be calculated by determining from the residual property functions (also referred to as departure functions)[5][6][7] using this relation:[8]
Equations of state (EOS) (such as the Peng-Robinson equation of state) can be used to solve this relation and to provide values of that match experimental values very closely.
Definitions of specific heat and heat capacity
The specific heat (or specific heat capacity), is the amount of heat energy required to increase the temperature of a unit quantity of a substance by a certain temperature interval. For example, the heat required to raise the temperature of 1 gram of water by 1 kelvin is 4.184 joules. The specific heat capacity is usually expressed as Jg-1K-1. It may also be expressed on a molar basis as Jmol-1K-1.
The heat capacity (as distinct from specific heat) is the amount of heat energy required to increase the temperature of a substance by a certain temperature interval. Heat capacity is an extensive property because its value is proportional to the amount of the substance. For example, a kilogram of water has a greater heat capacity than 100 grams of water. The heat capacity is usually expressed as JK-1.
Specific heat capacities and heat capacities have the same symbols of and . The specific heat ratio, , has the same numeric value whether based on specific heats or heat capacities.
References
- ↑ Frank M. White (1999). Fluid Mechanics, Fourth Edition. McGraw-Hill. ISBN 0-07-0697167.
- ↑ Norbert A. Lange (Editor) (1969). Lange's Handbook of Chemistry, 10th Edition. McGraw-Hill, page 1524.
- ↑ 3.0 3.1 3.2 3.3 3.4 Stephan R. Turns (2006). Thermodynamics: Concepts and Application, First Edition. Cambridge University Press. ISBN 0-521-85042-8.
- ↑ Don. W. Green, James O Maloney and Robert H. Perry (Editors) (1984). Perry's Chemical Engineers' Handbook, Sixth Edition. McGraw-Hill, page 6-17. ISBN 0-07-049479-7.
- ↑ K.Y. Narayanan (2001). A Textbook of Chemical Engineering Thermodynamics. Prentice-Hall India. ISBN 81-203-1732-7.
- ↑ Y.V.C. Rao (1997). Chemical Engineering Thermodynamics, First Edition. Universities Press. ISBN 81-7371-048-1.
- ↑ Thermodynamics of Pure Substances Lecture by Mark Gibbs, University of Edinburgh, Scotland.
- ↑ Isochoric heat capacity (pdf page 61 of 308)
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