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| {{Thermodynamics|cTopic=[[Thermodynamic system|Systems]]}}
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| An ''isobaric process''' is a [[thermodynamic process]] in which the pressure stays constant: Δ''P'' = 0. The term derives from the Greek ''iso-,'' (equal), and ''baros'' (weight). The heat transferred to the system does work but also changes the internal energy of the system:
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| [[Image:Isobaric process plain.svg|thumb|250px|The yellow area represents the work done]]
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| :<math> Q = \Delta U + W\, </math>
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| According to the [[first law of thermodynamics]], where ''W'' is work done ''on'' the system, ''U'' is internal energy, and ''Q'' is heat. Pressure-volume work by the closed system is defined as:
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| :<math>W = \int \! p \,dV \,</math>
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| where Δ means change over the whole process, whereas d denotes a differential. Since pressure is constant, this means that
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| :<math> W = p \Delta V\, </math>.
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| Applying the [[ideal gas law]], this becomes
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| :<math> W = n\,R\,\Delta T</math>
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| assuming that the quantity of gas stays constant, e.g., there is no [[phase transition]] during a [[chemical reaction]]. According to the [[equipartition theorem]], the change in internal energy is related to the temperature of the system by
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| :<math> \Delta U = n\,c_V\,\Delta T</math>,
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| where <math>c_V</math> is specific heat at a constant volume.
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| Substituting the last two equations into the first equation produces:
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| :<math> Q = n\,c_V\,\Delta T + n\,R\,\Delta T </math>
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| ::<math> = n\,(c_V + R)\,\Delta T </math>
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| ::<math> = n\,c_P\,\Delta T </math>,
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| where <math>c_P</math> is specific heat at a constant pressure.
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| ==Specific heat capacity==
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| To find the molar specific heat capacity of the gas involved, the following equations apply for any general gas that is calorically perfect. The property <math>\gamma</math> is either called the adiabatic index or the [[heat capacity ratio]]. Some published sources might ''k'' instead of <math>\gamma</math>.
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| Molar isochoric specific heat:
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| :<math>c_V = \frac{R}{\gamma - 1}</math>. | |
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| Molar isobaric specific heat:
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| :<math>c_p = \frac{\gamma R}{\gamma - 1}</math>.
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| The values for <math>\gamma</math> are <math>\gamma = 1.4</math> for diatomic gasses like [[Atmosphere of Earth#Composition|air and its major components]], and <math>\gamma = \frac{5}{3}</math> for monatomic gasses like the [[noble gas]]ses. The formulas for specific heats would reduce in these special cases:
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| Monatomic:
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| :<math>c_V = \frac{3 R}{2}</math> and <math>c_P = \frac{5 R}{2}</math>
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| Diatomic:
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| :<math>c_V = \frac{5 R}{2}</math> and <math>c_P = \frac{7 R}{2}</math>
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| An isobaric process is shown on a P-V diagram as a straight horizontal line, connecting the initial and final thermostatic states. If the process moves towards the right, then it is an expansion. If the process moves towards the left, then it is a compression.
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| ==Sign convention for work==
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| The motivation for the specific [[sign convention]]s of [[thermodynamics]] comes from early development of heat engines. When designing a heat engine, the goal is to have the system produce and deliver work output. The source of energy in a heat engine, is a heat input.
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| If the volume compresses (delta V = final volume - initial volume < 0), then W < 0. That is, during isobaric compression the gas does negative work, or the environment does positive work. Restated, the environment does positive work on the gas.
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| If the volume expands (delta V = final volume - initial volume > 0), then W > 0. That is, during isobaric expansion the gas does positive work, or equivalently, the environment does negative work. Restated, the gas does positive work on the environment.
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| If heat is added to the system, then Q > 0. That is, during isobaric expansion/heating, positive heat is added to the gas, or equivalently, the environment receives negative heat. Restated, the gas receives positive heat from the environment.
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| If the system rejects heat, then Q < 0. That is, during isobaric compression/cooling, negative heat is added to the gas, or equivalently, the environment receives positive heat. Restated, the environment receives positive heat from the gas.
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| ==Defining enthalpy==
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| An [[isochoric process]] is described by the equation <math> Q = \Delta U </math>. It would be convenient to have a similar equation for isobaric processes. Substituting the second equation into the first yields
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| :<math> Q = \Delta U + \Delta (p\,V) = \Delta (U + p\,V) </math> | |
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| The quantity ''U + p V'' is a state function so that it can be given a name. It is called [[enthalpy]], and is denoted as ''H''. Therefore an isobaric process can be more succinctly described as
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| :<math> Q = \Delta H \,</math>.
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| Enthalpy and isobaric specific heat capacity are very useful mathematical constructs, since when analyzing a process in an [[Thermodynamic_system#Open_system|open system]], the situation of zero work occurs when the fluid flows at constant pressure. In an open system, enthalpy is the quantity which is useful to use to keep track of energy content of the fluid.
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| ==Variable density viewpoint==
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| A given quantity (mass ''m'') of gas in a changing volume produces a change in [[density#Changes in density|density]] ρ. In this context the ideal gas law is written
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| : R(''T'' ρ) = M ''P''
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| where ''T'' is [[thermodynamic temperature]] and ''M'' is [[molar mass]]. When R and M are taken as constant, then pressure ''P'' can stay constant as the density-temperature quadrant (ρ,''T'' ) undergoes a [[squeeze mapping]].<ref>Peter Olver (1999), ''Classical Invariant Theory'', p. 217</ref>
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| ==See also==
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| * [[Adiabatic process]]
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| * [[Cyclic process]]
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| * [[Isochoric process]]
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| * [[Isothermal process]]
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| * [[Polytropic process]]
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| * [[Isoenthalpic process]]
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| ==References==
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| {{reflist}}
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| [[Category:Thermodynamic processes]]
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| [[Category:Atmospheric thermodynamics]]
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