Temperature

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Temperature

Temperature
world (these countries included) measures temperature using the Celsius scale and thermodynamic temperature using the kelvin scale, which is just the Celsius scale shifted downwards so that 0 K[1]= −273.15 °C, or absolute zero. Many engineering fields in the U.S., especially high-tech ones, also use the kelvin and degrees Celsius scales. Other engineering fields in the U.S. also rely upon the Rankine scale (a shifted Fahrenheit scale) when working in thermodynamic-related disciplines such as combustion.

Overview

The temperature of an ideal monatomic gas is a measure related to the average kinetic energy of its atoms as they move. In this animation, the size of helium atoms relative to their spacing is shown to scale under 1950 atmospheres of pressure. These room-temperature atoms have a certain, average speed (slowed down here two trillion fold). In physics, temperature is a physical property of a system that underlies the common notions of hot and cold; something that feels hotter generally has the greater temperature. Temperature is one of the principal parameters of thermodynamics. On the macroscopic scale, temperature is the unique physical property that determines the direction of heat flow between two objects placed in thermal contact. If no heat flow occurs, the two objects have the same temperature; otherwise heat flows from the hotter object to the colder object. This is the content of the zeroth law of thermodynamics. On the microscopic scale, temperature can be defined as the average energy in each degree of freedom in the particles in a system- because temperature is a statistical property, a system must contain a few particles for the question as to its temperature to make any sense. For a solid, this energy is found in the vibrations of its atoms about their equilibrium positions. In an ideal monatomic gas, energy is found in the translational motions of the particles; with molecular gases, vibrational and rotational motions also provide thermodynamic degrees of freedom. Temperature is measured with thermometers that may be calibrated to a variety of temperature scales. In most of the world (except for Belize, Myanmar, Liberia and the United States), the Celsius scale is used for most temperature measuring purposes. The entire scientific

Heating a body, such as a segment of protein alpha helix (above), tends to cause its atoms to vibrate more, and to cause it to expand or change phase. Intuitively, temperature is the measurement of how hot or cold something is, although the most immediate way in which we can measure this, by feeling it, is unreliable, resulting in the phenomenon of felt air temperature, which can differ at varying degrees from actual temperature. On the molecular level, temperature is the result of the motion of particles which make up a substance. Temperature increases as the energy of this motion increases. The motion may be the translational motion of the particle, or the internal energy of the particle due to molecular vibration or the excitation of an electron energy level. Although very specialized laboratory equipment is required to directly detect the translational thermal motions, thermal collisions by atoms or molecules with small particles suspended in a fluid

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produces Brownian motion that can be seen with an ordinary microscope. The thermal motions of atoms are very fast and temperatures close to absolute zero are required to directly observe them. For instance, when scientists at the NIST achieved a record-setting cold temperature of 700 nK (1 nK = 10−9 K) in 1994, they used optical lattice laser equipment to adiabatically cool caesium atoms. They then turned off the entrapment lasers and directly measured atom velocities of 7 mm per second in order to calculate their temperature. Molecules, such as O2, have more degrees of freedom than single atoms: they can have rotational and vibrational motions as well as translational motion. An increase in temperature will cause the average translational energy to increase. It will also cause the energy associated with vibrational and rotational modes to increase. Thus a diatomic gas, with extra degrees of freedom rotation and vibration, will require a higher energy input to change the temperature by a certain amount, i.e. it will have a higher heat capacity than a monatomic gas. The process of cooling involves removing energy from a system. When there is no more energy able to be removed, the system is said to be at absolute zero, which is the point on the thermodynamic (absolute) temperature scale where all kinetic motion in the particles comprising matter ceases and they are at complete rest in the “classic” (non-quantum mechanical) sense. By definition, absolute zero is a temperature of precisely 0 kelvins (−273.15 °C or −459.68 °F).

Temperature
difference does exist, heat will tend to move from the higher-temperature system to the lower-temperature system, until they are at thermal equilibrium. This heat transfer may occur via conduction, convection or radiation or combinations of them (see heat for additional discussion of the various mechanisms of heat transfer) and some ions may vary. Temperature is also related to the amount of internal energy and enthalpy of a system: the higher the temperature of a system, the higher its internal energy and enthalpy. Temperature is an intensive property of a system, meaning that it does not depend on the system size, the amount or type of material in the system, the same as for the pressure and density. By contrast, mass, volume, and entropy are extensive properties, and depend on the amount of material in the system.

The role of temperature in nature

Details
Conjugate variables of thermodynamics Pressure Volume (Stress) (Strain) Temperature Entropy Chem. potential Particle no. The formal properties of temperature follow from its mathematical definition (see below for the zeroth law definition and the second law definition) and are studied in thermodynamics and statistical mechanics. Contrary to other thermodynamic quantities such as entropy and heat, whose microscopic definitions are valid even far away from thermodynamic equilibrium, temperature being an average energy per particle can only be defined at thermodynamic equilibrium, or at least local thermodynamic equilibrium (see below). As a system receives heat, its temperature rises; similarly, a loss of heat from the system tends to decrease its temperature (at the—uncommon—exception of negative temperature; see below). When two systems are at the same temperature, no heat transfer occurs between them. When a temperature A map of monthly mean temperatures Temperature plays an important role in almost all fields of science, including physics, geology, chemistry, and biology. Many physical properties of materials including the phase (solid, liquid, gaseous or plasma), density, solubility, vapor pressure, and electrical conductivity depend on the temperature. Temperature also plays an important role in determining the rate and extent to which chemical reactions occur. This is one reason why the human body has several elaborate mechanisms for maintaining the temperature at 37 °C, since temperatures only a few degrees higher can result in harmful reactions with serious consequences. Temperature also controls the type and quantity of thermal radiation emitted from a surface. One application of this effect is the incandescent light bulb, in which a tungsten filament is electrically heated to a temperature at which significant quantities of visible light are emitted. Temperature-dependence of the speed of sound in air c, density of air ρ and acoustic impedance Z vs. temperature °C

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Impact of temperature on speed of sound, air density and acoustic impedance at sea level T in °C −10 −5 0 5 10 15 20 25 30 c in m/s 325.4 328.5 331.5 334.5 337.5 340.5 343.4 346.3 349.2 ρ in kg/m³ 1.341 1.316 1.293 1.269 1.247 1.225 1.204 1.184 1.164 Z in N·s/m³ 436.5 432.4 428.3 424.5 420.7 417.0 413.5 410.0 406.6

Temperature

Temperature measurement
See also: Timeline of temperature and pressure measurement technology See also: International Temperature Scale of 1990 Temperature measurement using modern scientific thermometers and temperature scales goes back at least as far as the early 18th century, when Gabriel Fahrenheit adapted a thermometer (switching to mercury) and a scale both developed by Ole Christensen Rømer. Fahrenheit’s scale is still in use in the USA, with the Celsius scale in use in the rest of the world and the kelvin scale.

Units of temperature
The basic unit of temperature (symbol: T) in the International System of Units (SI) is the kelvin (Symbol: K). The kelvin and Celsius scales are, by international agreement, defined by two points: absolute zero, and the triple point of Vienna Standard Mean Ocean Water (water specially prepared with a specified blend of hydrogen and oxygen isotopes). Absolute zero is defined as being precisely 0 K and −273.15 °C. Absolute zero is where all kinetic motion in the particles comprising matter ceases and they are at complete rest in the “classic” (non-quantum mechanical) sense. At absolute zero, matter contains no thermal energy. Also, the triple point of water is defined as being precisely 273.16 K and 0.01 °C. This definition does three things: 1) it fixes the magnitude of the kelvin unit as being precisely 1 part in 273.16 parts the difference between absolute zero and the triple point of water; 2) it establishes that one kelvin has precisely the same magnitude as a one degree increment on the Celsius scale; and 3) it establishes the difference between the two scales’ null points as being precisely 273.15 kelvins (0 K = −273.15 °C and 273.16 K = 0.01 °C). Formulas for converting from these defining units of temperature to other scales can be found at Temperature conversion formulas. In the field of plasma physics, because of the high temperatures encountered and the electromagnetic

Water freezes at 0 °C. The frost shown here is at -17 °C.

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nature of the phenomena involved, it is customary to express temperature in electronvolts (eV) or kiloelectronvolts (keV), where 1 eV = 11,604 K. In the study of QCD matter one routinely meets temperatures of the order of a few hundred MeV, equivalent to about 1012 K. For everyday applications, it’s very often convenient to use the Celsius scale, in which 0 °C corresponds to the temperature at which water freezes and 100 °C corresponds to the boiling point of water at sea level. In this scale a temperature difference of 1 degree is the same as a 1 K temperature difference, so the scale is essentially the same as the kelvin scale, but offset by the temperature at which water freezes (273.15 K). Thus the following equation can be used to convert from degrees Celsius to kelvins.

Temperature
precision. See Temperature of a Healthy Human (Body Temperature) for more information. Some numbers in this table have been rounded off.

Theoretical foundation
Definition based on zeroth law of thermodynamics
While most people have a basic understanding of the concept of temperature, its formal definition is rather complicated. Before jumping to a formal definition, let us consider the concept of thermal equilibrium. If two systems with fixed volumes are brought together in thermal contact, changes will most likely take place in the properties of both systems. These changes are caused by the transfer of heat between the systems. A state must be reached in which no further changes occur, to put the objects into thermal equilibrium. A basis for the definition of temperature can be obtained from the zeroth law of thermodynamics which states that if two systems, A and B, are in thermal equilibrium and a third system C is in thermal equilibrium with system A then systems B and C will also be in thermal equilibrium (being in thermal equilibrium is a transitive relation; moreover, it is an equivalence relation). This is an empirical fact, based on observation rather than theory. Since A, B, and C are all in thermal equilibrium, it is reasonable to say each of these systems shares a common value of some property. We call this property temperature. Generally, it is not convenient to place any two arbitrary systems in thermal contact to see if they are in thermal equilibrium and thus have the same temperature. Also, it would only provide an ordinal scale. Therefore, it is useful to establish a temperature scale based on the properties of some reference system. Then, a measuring device can be calibrated based on the properties of the reference system and used to measure the temperature of other systems. One such reference system is a fixed quantity of gas. The ideal gas law indicates that the product of the pressure and volume (P · V) of a gas is directly proportional to the temperature[3]: (1) where ’T is temperature, n is the number of moles of gas and R is the gas constant. Thus, one can define a scale for temperature based on the corresponding pressure and volume of the gas: the temperature in kelvins is the pressure in pascals of one mole of gas in a container of one cubic metre, divided by 8.31... In practice, such a gas thermometer is not very convenient, but other measuring instruments can be calibrated to this scale. It is also interesting to note that pressure, volume, and the number of moles of a substance are all inherently greater than or equal to zero. This suggests that

In the United States, the Fahrenheit scale is widely used. On this scale the freezing point of water corresponds to 32 °F and the boiling point to 212 °F. The following formula can be used to convert from Fahrenheit to Celsius:

See temperature conversion formulas for conversions between most temperature scales.

Negative temperatures
In the macroscopic sense relevant to most people, a negative temperature is one below the zero-point of the measurement system used. For example, a temperature of 100 K is equivalent to −173.15 °C. Temperatures of macroscopic systems may have negative values in the Celsius and Fahrenheit, but not in the Kelvin or Rankine scales. However, for some systems and specific definitions of temperature, it is possible to obtain a negative temperature, which is numerically less than absolute zero. However, a system with a negative temperature is not colder than absolute zero, but rather it is, in a sense, hotter than infinite temperature.[2]

Comparison of temperature scales
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The temperature scale is in disuse, and of mere historical interest. 2 Normal human body temperature is 36.8 ±0.7 °C, or 98.2 ±1.3 °F. The commonly given value 98.6 °F is simply the exact conversion of the nineteenth-century German standard of 37 °C. Since it does not list an acceptable range, it could therefore be said to have excess (invalid)

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Comparison of temperature scales Comment Absolute zero Kelvin K    0 Celsius °C −273.15  −89 Fahrenheit Rankine °F °Ra (°R) −459.67 −128     0   331 Delisle °D ¹   284

Temperature

Newton Réaumur Rømer °N ¹ °R (°Ré, °Re) ¹ °Rø (°R) ¹ −135.90  −39  −29  −71

559.725  −90.14 −218.52

Lowest recorded natural  184 temperature on Earth (Vostok, Antarctica - 21 July 1983) Celsius / Fahrenheit’s "cross-over" temperature Fahrenheit’s ice/salt mixture  233.15

−40

–40

419.67

210

–13.2

–32

–13.5

255.37

−17.78    0   15   36.8 ±0.7   58

0   32   59

459.67   491.67   519

176.67   −5.87  −14.22   150   128    0    5   12.1 ±0.2   19    0   12   29.4 ±0.6   46

−1.83    7.5   15   26.8 ±0.4   38

Water freezes (at stand-  273.15 ard pressure) Average surface temper-  288 ature on Earth Average human body temperature ² Highest recorded surface temperature on Earth (Al ’Aziziyah, Libya - 13 September 1922)  310.0 ±0.7  331

98.2 ±1.3   557.9 ±1.3    94.8 ±1.1  136   596    63

Water boils (at standard  373.1339   99.9839  211.97102   671.64102     0 pressure) Titanium melts The surface of the Sun 1941 5800 1668 5526 3034 9980  3494 10440 −2352 −8140

33  550 1823

80 1334 4421

60  883 2909

temperature must also be greater than or equal to zero. As a practical matter it is not possible to use a gas thermometer to measure absolute zero temperature since the gasses tend to condense into a liquid long before the temperature reaches zero. It is possible to extrapolate how many degrees below the present temperature the absolute zero is from the temperature range where Equation 1 works.

, where k = R / n (n= Avogadro number, R= ideal gas constant). In the case of a monoatomic gas, the kinetic energy is:

Temperature in gases
For an ideal gas the kinetic theory of gases uses statistical mechanics to relate the temperature to the average kinetic energy of the atoms in the system. This average energy is independent of particle mass, which seems counter-intuitive. Temperature is related only to the average kinetic energy of the particles in a gas - each particle has its own energy which may or may not correspond to the average; the distribution of energies (and thus speeds) of the particles in any gas are given by the Maxwell-Boltzmann distribution. The temperature of an ideal gas is related to its average kinetic energy via the equation[3]:

(Note that a calculation of the kinetic energy of a more complicated object, such as a molecule, is slightly more involved. Additional degrees of freedom are available, so molecular rotation or vibration must be included.) The second law of thermodynamics states that any two given systems when interacting with each other will later reach the same average energy per particle (and hence the same temperature). In a mixture of particles of various mass, the heaviest particles will move more slowly than lighter counterparts, but will still have the same average energy. A neon atom moves slower relative to a hydrogen molecule of the same kinetic energy; a pollen particle moves in a slow Brownian motion among fast moving water molecules, etc. A visual illustration of this from Oklahoma State University makes the point more clear. Particles with different mass have different

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velocity distributions, but the average kinetic energy is the same because of the ideal gas law.

Temperature
sometimes referred to as the temperature of space. This temperature is thus like a test charge in that it facilitates a measure of the system even though temperature is not strictly defined there.

Temperature in plasmas Temperature of the vacuum

Definition based on second law of thermodynamics
In the previous section temperature was defined in terms of the Zeroth Law of thermodynamics. It is also possible to define temperature in terms of the second law of thermodynamics, which deals with entropy. Entropy is a measure of the disorder in a system. The second law states that any process will result in either no change or a net increase in the entropy of the universe. This can be understood in terms of probability. Consider a series of coin tosses. A perfectly ordered system would be one in which either every toss comes up heads or every toss comes up tails. This means that for a perfectly ordered set of coin tosses, there is only one set of toss outcomes possible: the set in which 100% of tosses came up the same. On the other hand, there are multiple combinations that can result in disordered or mixed systems, where some fraction are heads and the rest tails. A disordered system can be 90% heads and 10% tails, or it could be 40% heads and 60% tails, et cetera. As the number of coin tosses increases, the number of possible combinations corresponding to imperfectly ordered systems increases. For a very large number of coin tosses, the number of combinations corresponding to ~50% heads and ~50% tails dominates and obtaining an outcome significantly different from 50/50 becomes extremely unlikely. Thus the system naturally progresses to a state of maximum disorder or entropy. We previously stated that temperature controls the flow of heat between two systems and we have just shown that the universe, and we would expect any natural system, tends to progress so as to maximize entropy. Thus, we would expect there to be some relationship between temperature and entropy. In order to find this relationship let’s first consider the relationship between heat, work and temperature. A heat engine is a device for converting heat into mechanical work and analysis of the Carnot heat engine provides the necessary relationships we seek. The work from a heat engine corresponds to the difference between the heat put into the system at the high temperature, qH and the heat ejected at the low temperature, qC. The efficiency is the work divided by the heat put into the system or:

(2) where wcy is the work done per cycle. We see that the efficiency depends only on qC/qH. Because qC and qH

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correspond to heat transfer at the temperatures TC and TH, respectively, qC/qH should be some function of these temperatures: (3) Carnot’s theorem states that all reversible engines operating between the same heat reservoirs are equally efficient. Thus, a heat engine operating between T1 and T3 must have the same efficiency as one consisting of two cycles, one between T1 and T2, and the second between T2 and T3. This can only be the case if: (7)

Temperature
corresponds to the entropy of the system, which we described previously. We can rearranging Equation 6 to get a new definition for temperature in terms of entropy and heat:

For a system, where entropy S may be a function S(E) of its energy E, the temperature T is given by: (8) ie. the reciprocal of the temperature is the rate of increase of entropy with respect to energy.

which implies: q13 = f(T1,T3) = f(T1,T2)f(T2,T3) Since the first function is independent of T2, this temperature must cancel on the right side, meaning f(T1,T3) is of the form g(T1)/g(T3) (i.e. f(T1,T3) = f(T1,T2)f(T2,T3) = g(T1)/g(T2)· g(T2)/g(T3) = g(T1)/g(T3)), where g is a function of a single temperature. We can now choose a temperature scale with the property that:

Importance of temperature
The below table demonstrates that the properties of air change significantly with temperature. Table — speed of sound in air c, density of air ρ, acoustic impedance Z vs. temperature

• Absolute zero • Body temperature (Thermoregulation) • Celsius • Color temperature • Dry-bulb temperature • Entropy • Fahrenheit • Heat • Heat conduction • Heat convection • • • • • ISO 1 ITS-90 Kelvin Maxwell’s demon Orders of magnitude (temperature) Planck temperature Rankine scale Relativistic heat conduction • Thermal radiation • Thermodynamic (absolute) temperature • Thermography • Thermometer • Triple point • Virtual temperature • Wet Bulb Globe Temperature • Wet-bulb temperature

(4) Substituting Equation 4 back into Equation 2 gives a relationship for the efficiency in terms of temperature:

(5) Notice that for TC = 0 K the efficiency is 100% and that efficiency becomes greater than 100% below 0 K. Since an efficiency greater than 100% violates the first law of thermodynamics, this implies that 0 K is the minimum possible temperature. In fact the lowest temperature ever obtained in a macroscopic system was 20 nK, which was achieved in 1995 at NIST. Subtracting the right hand side of Equation 5 from the middle portion and rearranging gives:

• • •

Notes
[1] This means "zero kelvin"; the unit kelvin is not used with a degree symbol because it is an absolute scale, i.e. the notation 0 °K is not correct according to international standards Kittel and Kroemer, pp. 462 ^ Vu-Quoc, L., Configuration integral (statistical mechanics), 2008

where the negative sign indicates heat ejected from the system. This relationship suggests the existence of a state function, S, defined by: (6) where the subscript indicates a reversible process. The change of this state function around any cycle is zero, as is necessary for any state function. This function

[2] [3]

References
• Chang, Hasok (2004). Inventing Temperature: Measurement and Scientific Progress. Oxford: Oxford University Press. ISBN 9780195171273.

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Effect of temperature Temperature in °C −25 −20 −15 −10 −5 0 +5 +10 +15 +20 +25 +30 +35 Speed of sound c in m·s−1 315.8 318.9 322.1 325.2 328.3 331.3 334.3 337.3 340.3 343.2 346.1 349.0 351.9 Density of air ρ in kg·m−3 1.423 1.395 1.368 1.342 1.317 1.292 1.269 1.247 1.225 1.204 1.184 1.164 1.146 Acoustic impedance Z in N·s·m−3 449.4 444.9 440.6 436.1 432.0 428.4 424.3 420.6 416.8 413.2 409.8 406.2 403.3

Temperature

• Kittel, Charles; Kroemer, Herbert (1980). Thermal Physics (2nd ed. ed.). W. H. Freeman Company. ISBN 0-7167-1088-9. • Zemansky, Mark Waldo (1964). Temperatures Very Low and Very High. Princeton, N.J.: Van Nostrand.

• An elementary introduction to temperature aimed at a middle school audience • What is Temperature? An introductory discussion of temperature as a manifestation of kinetic theory. • Why do we have so many temperature scales?