Thermodynamic state variables and equation of state

Leave a sealed bottle of soda in a hot car and it can bulge, hiss, even burst — nothing was added to it, nothing was taken away, yet its pressure climbed high enough to strain the plastic. A bicycle tyre pumped up in the cool morning reads a few kPa higher by a scorching afternoon, with not one more molecule of air inside. Something changed the state of that trapped gas, and thermodynamics gives us a precise, quantitative language for exactly what changed and how the changes are linked. That language starts with state variables — a short list of measurable numbers (pressure, volume, temperature, amount of gas) that between them completely describe the condition of a gas sitting in equilibrium, regardless of what happened to it earlier. You do not need to know whether the tyre was pumped fast or slow, whether the soda bottle was shaken or left still — only its current PP, VV, TT, nn matter. And remarkably, these four numbers are not free to roam independently: for a fixed amount of an ideal gas they are locked together by a single algebraic relation, the equation of state PV=nRTPV = nRT. Fix any two and the other two are no longer yours to choose. This article builds that idea from the ground up: what makes a quantity a state variable rather than a path-dependent one, why some variables double when you double the gas (extensive) while others do not (intensive), how the equation of state PV=nRTPV = nRT ties PP, VV, TT, nn together for an ideal gas, and how to read a point — and a process — off a PP–VV diagram. It is the quiet workhorse behind every gas-law calculation in the rest of the thermodynamics unit, from isothermal expansions to adiabatic compressions.

Key takeaways
  • A thermodynamic state variable (pressure PP, volume VV, temperature TT, amount nn) depends only on the current condition of the gas, never on the path taken to reach it.
  • State variables split into two kinds: extensive (scale with the amount of gas — VV, UU, mass) and intensive (independent of the amount — PP, TT, density).
  • The equation of state for an ideal gas is PV=nRTPV = nRT, with R=8.31 J mol−1K−1R = 8.31\ \text{J mol}^{-1}\text{K}^{-1}; equivalently PV=mMRTPV = \dfrac{m}{M}RT using mass mm and molar mass MM.
  • For a fixed amount of gas, PP, VV, TT are not independent — only two can be chosen freely, the equation of state fixes the third, giving the combined gas law P1V1T1=P2V2T2\dfrac{P_1V_1}{T_1} = \dfrac{P_2V_2}{T_2}.
  • A gas's state is a single point on a PP–VV diagram; a thermodynamic process is a path between two such points, and different paths between the same two points can involve different heat and work even though ΔU\Delta U depends only on the endpoints.
  • Real gases obey PV=nRTPV = nRT only approximately (worse at high pressure, low temperature) but CBSE Class 11 treats all gases as ideal throughout this unit.
  • Key idea: a gas in equilibrium is fully pinned down by the state variables P, V, T, n through the single relation PV = nRT, so fixing any two of P, V, T for a given amount of gas automatically fixes the third.
The core insight

For a fixed amount of ideal gas the state variables pressure, volume and temperature are chained together by PV=nRTPV = nRT, so only two of the three can ever be chosen independently, and every point on a PP–VV diagram represents one complete, unique equilibrium state of the gas.

Where it fits in the syllabus

This topic sits inside the CBSE Class 11 Physics Thermodynamics chapter, right after thermal equilibrium, the zeroth law and the first law (ΔQ=ΔU+ΔW\Delta Q = \Delta U + \Delta W), and just before the chapter turns to naming specific processes — isothermal, adiabatic, isochoric, isobaric and cyclic. The ideal gas equation of state PV=nRTPV = nRT itself is developed in full, from kinetic theory, in the separate Kinetic Theory chapter, but the Thermodynamics chapter uses it constantly as a tool: every PP–VV diagram, every "find the work done as the gas expands" question, leans on this single relation. You are expected to identify PP, VV, TT, nn as the basic state variables, tell extensive from intensive variables, and apply PV=nRTPV = nRT and the combined gas law fluently before tackling the process-specific work and heat calculations that follow.

The physical picture

A gas sample settles into equilibrium when its pressure, volume and temperature stop changing on their own — stir it, heat it unevenly, and wait, and eventually every part of the gas agrees on a single PP, a single TT. Once it has settled, the gas is completely described by a short list of numbers:

  • Pressure PP — the force per unit area the gas exerts on its container walls, SI unit pascal (Pa), 1 Pa=1 N/m21\ \text{Pa} = 1\ \text{N/m}^2.
  • Volume VV — the space the gas occupies, SI unit cubic metre (m³); the litre (1 L=10−3 m31\ \text{L} = 10^{-3}\ \text{m}^3) is a common lab unit.
  • Temperature TT — measured in kelvin (K) for all gas-law work; it tracks the average kinetic energy of the molecules (developed fully in Kinetic Theory).
  • Amount of substance nn — the number of moles of gas present, or equivalently the mass mm divided by the molar mass MM.

These four are called state variables or state functions precisely because each one has a definite value once the gas has settled into equilibrium — it does not matter whether the gas arrived there by slow heating, sudden compression, or any other route. Contrast this with quantities like heat QQ and work WW, which are not state variables: they depend on the path taken between two states, not just on the states themselves. State variables further split by how they respond to scaling up the system. Take two identical boxes of the same gas at the same PP and TT, and merge them into one box (doubling the amount of gas at the same PP, TT):

  • Extensive variables double when you merge the two boxes — volume VV, internal energy UU, and total mass all double. They depend on how much gas you have.
  • Intensive variables stay the same when you merge the boxes — pressure PP, temperature TT, and density ρ\rho are unchanged. They describe the condition of the gas, not its quantity.

An equation of state is the mathematical rule connecting a system's state variables in equilibrium. For an ideal gas — the model CBSE Class 11 uses throughout this unit — that rule is

PV=nRTPV = nRT

where: PP is pressure (Pa), VV is volume (m³), nn is the number of moles, TT is absolute temperature (K), and R=8.31 J mol−1K−1R = 8.31\ \text{J mol}^{-1}\text{K}^{-1} is the universal gas constant, the same number for every ideal gas regardless of what it is made of. Written in terms of the total mass mm and molar mass MM of the gas (using n=m/Mn = m/M), the same law reads

PV=mMRTPV = \frac{m}{M}RT

where: this second form is convenient when you are told a mass of gas rather than a mole count. The physical reading of PV=nRTPV = nRT is that once you fix nn (the amount of gas you have sealed in), only two of PP, VV, TT are yours to set independently — the third is then forced. Push the piston in (lower VV) at constant TT and PP must rise; heat the gas (raise TT) in a rigid box and PP must rise; and so on. This is exactly what makes the state of a fixed amount of gas representable as a single point on a PP–VV diagram, with the temperature implied by that point through the equation of state.

Figure
A pressure volume plane with two marked points representing two equilibrium states of a gas, joined by a curved path labelled as the process, with dashed guide lines showing that each point fixes a definite pressure and volume
A state is a point; a process is a path between two points volume V pressure P state 1: P1, V1, T1 state 2: P2, V2, T2 the process — a chosen path a different path, same endpoints Both paths give the same delta U (endpoints only), but different Q and W (path matters).

Because PP, VV, TT are state variables, only the endpoints of a path on this diagram matter for computing the change in internal energy ΔU\Delta U — but the shape of the path itself determines how much heat QQ flows and how much work WW is done, a distinction the first law of thermodynamics will make precise. Real gases follow PV=nRTPV = nRT only approximately, deviating more at high pressure and low temperature where molecules start to interact and take up appreciable volume — but CBSE Class 11 treats every gas in this unit as ideal.

Derivation AGetting the combined gas law from the equation of state

The goal is to show that for a fixed amount of gas — the same sealed sample, no gas added or removed — the equation of state PV=nRTPV = nRT forces a simple relation between any two equilibrium states of that gas, P1V1T1=P2V2T2\dfrac{P_1V_1}{T_1} = \dfrac{P_2V_2}{T_2}, using nothing beyond the algebra of rearranging PV=nRTPV = nRT and the fact that nn and RR do not change between the two states. This combined gas law is the single most-used tool for "gas goes from state 1 to state 2" problems in the whole chapter.

Step 1. Write the equation of state for the initial state 1, with pressure P1P_1, volume V1V_1, temperature T1T_1, and the fixed amount of gas nn. Rearranging, P1V1T1=nR\dfrac{P_1V_1}{T_1} = nR.

Step 2. Write the same equation of state for the final state 2, reached after any process — heating, compression, expansion, any path at all — with pressure P2P_2, volume V2V_2, temperature T2T_2, and the same nn (no gas was added or removed). Rearranging identically, P2V2T2=nR\dfrac{P_2V_2}{T_2} = nR.

Step 3. Compare the two right-hand sides. Both equal nRnR, and nn, RR are unchanged between the two states — RR is a universal constant and nn is fixed by the problem (a sealed sample). So the two left-hand sides must be equal to each other: P1V1T1=P2V2T2\dfrac{P_1V_1}{T_1} = \dfrac{P_2V_2}{T_2}.

Step 4. Read the result. This combined gas law lets you find any one unknown among P2P_2, V2V_2, T2T_2 given the other two and the full initial state, without ever needing to compute nn or RR explicitly — though computing nn separately, as in the worked example below, is a good way to double-check the answer, since nn must come out the same from either state.

Worked examples

Board level - volume of a gas from its state variables

A cylinder contains 2 moles of an ideal gas at pressure 2×1052\times10^5 Pa and temperature 300 K. Find the volume occupied by the gas. (R=8.31 J mol−1K−1R = 8.31\ \text{J mol}^{-1}\text{K}^{-1}.)

Step 1. Identify the state variables given: n=2 moln = 2\ \text{mol}, P=2×105 PaP = 2\times10^5\ \text{Pa}, T=300 KT = 300\ \text{K}. The unknown is VV, and since all three other quantities in PV=nRTPV = nRT are known, the equation of state alone is enough — no combined gas law needed.

Step 2. Rearrange PV=nRTPV = nRT for volume: V=nRTPV = \dfrac{nRT}{P}.

Step 3. Substitute the numbers: V=2×8.31×3002×105=49862×105V = \dfrac{2 \times 8.31 \times 300}{2\times10^5} = \dfrac{4986}{2\times10^5}.

Step 4. Compute and convert to a familiar unit: V=0.02493 m3≈2.49×10−2 m3V = 0.02493\ \text{m}^3 \approx 2.49\times10^{-2}\ \text{m}^3. Since 1 m3=1000 L1\ \text{m}^3 = 1000\ \text{L}, this is about 24.9 litres — roughly the volume of a large cooking-gas cylinder, which is a useful sanity check on the order of magnitude.

Competitive level - verifying the equation of state across two states

A fixed mass of gas is initially at P1=1.2×105P_1 = 1.2\times10^5 Pa, V1=3×10−3 m3V_1 = 3\times10^{-3}\ \text{m}^3, T1=290T_1 = 290 K. It is heated and allowed to expand until its final state is P2=1.5×105P_2 = 1.5\times10^5 Pa, V2=4×10−3 m3V_2 = 4\times10^{-3}\ \text{m}^3. Find the final temperature T2T_2, and verify that the same equation of state is satisfied at both states with the same nn.

Step 1. Since the number of moles is fixed (no gas added or removed), apply the combined gas law derived above: P1V1T1=P2V2T2\dfrac{P_1V_1}{T_1} = \dfrac{P_2V_2}{T_2}, so T2=T1×P2V2P1V1T_2 = T_1 \times \dfrac{P_2V_2}{P_1V_1}.

Step 2. Substitute the numbers: T2=290×(1.5×105)(4×10−3)(1.2×105)(3×10−3)=290×600360T_2 = 290 \times \dfrac{(1.5\times10^5)(4\times10^{-3})}{(1.2\times10^5)(3\times10^{-3})} = 290 \times \dfrac{600}{360}.

Step 3. Compute: T2=290×1.667=483.3 KT_2 = 290 \times 1.667 = 483.3\ \text{K}. This is the temperature the gas must reach for its pressure and volume to end up at the stated final values.

Step 4. Cross-check by finding nn independently from each state. From state 1: n=P1V1RT1=(1.2×105)(3×10−3)8.31×290=3602409.9=0.1494 moln = \dfrac{P_1V_1}{RT_1} = \dfrac{(1.2\times10^5)(3\times10^{-3})}{8.31\times290} = \dfrac{360}{2409.9} = 0.1494\ \text{mol}. From state 2, using the just-found T2T_2: n=P2V2RT2=(1.5×105)(4×10−3)8.31×483.3=6004016.2=0.1494 moln = \dfrac{P_2V_2}{RT_2} = \dfrac{(1.5\times10^5)(4\times10^{-3})}{8.31\times483.3} = \dfrac{600}{4016.2} = 0.1494\ \text{mol}. The two values of nn agree exactly, so T2=483.3 KT_2 = 483.3\ \text{K}, and both states obey PV=nRTPV = nRT with the same fixed n≈0.1494 moln \approx 0.1494\ \text{mol}, as they must. Timing note: In an exam, do not compute nn twice as done here for verification — that is a check, not a requirement. For a straight numerical answer, apply the combined gas law directly (Steps 1–3) and stop; that should take under two minutes, leaving the verification step only for when the question explicitly asks you to confirm consistency or find nn.

Common traps

  • Forgetting to convert temperature to kelvin. The equation of state requires absolute temperature throughout; plugging in a Celsius value directly (e.g. using 2727 instead of 300 K300\ \text{K}) is one of the most common marks-losing errors in this topic.
  • Treating PP, VV, TT as three independent dials. For a fixed amount of gas, only two of the three can be chosen freely — the third is always forced by PV=nRTPV = nRT. A question that seems to give you three independent conditions on the same fixed sample is either testing this trap or giving redundant (consistent) information.
  • Mixing up extensive and intensive variables. Pressure and temperature do not change just because you have "more system" at fixed conditions elsewhere — but they absolutely do change if you add gas at fixed VV and TT (doubling nn at fixed V,TV, T doubles PP, by PV=nRTPV = nRT). The trap is applying "intensive means unaffected by anything" too broadly; it only means unaffected by scaling the system size at the same conditions.
  • Unit mismatches. R=8.31 J mol−1K−1R = 8.31\ \text{J mol}^{-1}\text{K}^{-1} demands pressure in pascals and volume in m³; using litres or atmospheres without converting first is a very common arithmetic slip, especially under time pressure.
  • Confusing a state variable with a path-dependent quantity. ΔU\Delta U depends only on the initial and final states (since UU is a state variable), but QQ and WW depend on the specific path taken between those states — do not assume that because P1V1T1P_1V_1T_1 and P2V2T2P_2V_2T_2 match between two problems, the heat and work involved must also match.

You should be able to…

  • List the basic thermodynamic state variables (PP, VV, TT, nn) and explain why they are called state variables.
  • Classify a given quantity as extensive or intensive by imagining what happens when you double the amount of the system.
  • State and apply the ideal gas equation of state PV=nRTPV = nRT, in both mole and mass forms.
  • Derive and apply the combined gas law P1V1T1=P2V2T2\dfrac{P_1V_1}{T_1} = \dfrac{P_2V_2}{T_2} for a fixed amount of gas moving between two states.
  • Explain why PP, VV, TT cannot all vary independently for a fixed amount of ideal gas.
  • Represent a gas's equilibrium state as a point on a PP–VV diagram, and a process as a path between two such points, distinguishing state variables (path-independent) from heat and work (path-dependent).

Ask the tutor: Want more practice converting between litres/atm and SI units in PV=nRTPV = nRT, or a walkthrough of how this equation of state sets up the isothermal and adiabatic processes coming up next? Ask the AI tutor for extra worked problems.

Why is PV = nRT called an equation of state and not just a formula

Because it does not describe one particular event or process — it describes every possible equilibrium condition a fixed amount of ideal gas can be in, all at once. Given any two of PP, VV, TT for a known nn, the equation immediately tells you the third, for that gas sitting quietly in equilibrium, regardless of how it got there. A "formula" in the everyday sense (like the volume of a cylinder) just computes one quantity from others; an equation of state is special because it is a constraint that every equilibrium state of the system must obey, which is exactly why it lets you represent states as points on a PP–VV diagram.

If pressure and temperature are intensive, does that mean they never change?

No — intensive only describes how a variable responds to scaling the size of the system at the same physical conditions, not whether it can change at all. If you merge two identical boxes of gas at the same PP and TT, the pressure and temperature of the combined system stay the same as before (that is what makes them intensive) — but if you heat that same gas, or compress it, or add more gas to the same container, pressure and temperature absolutely do change, exactly as PV=nRTPV = nRT predicts. Extensive versus intensive is about doubling the amount of system at fixed conditions, not about whether a process can alter the variable.

Why does the equation of state only work exactly for ideal gases, and how far off are real gases

An ideal gas is a simplifying model that assumes the gas molecules themselves take up negligible volume compared to the container and do not attract or repel each other except during brief collisions. Real gases — air, oxygen, carbon dioxide — approximately satisfy those assumptions at everyday pressures and temperatures, which is why PV=nRTPV = nRT works well enough for CBSE-level problems on cylinders, tyres, and lab gas samples. The approximation breaks down at very high pressure (molecules are squeezed close enough that their own volume matters) or very low temperature (molecules move slowly enough for intermolecular attraction to matter, eventually leading to liquefaction) — situations studied with corrected equations of state in more advanced courses, beyond the Class 11 syllabus.

How is the equation of state different from the combined gas law I learned earlier

They are really the same physics viewed two ways. The equation of state PV=nRTPV = nRT is the fundamental relation, valid for any single equilibrium state of a given amount of gas. The combined gas law P1V1T1=P2V2T2\dfrac{P_1V_1}{T_1} = \dfrac{P_2V_2}{T_2}, derived above, is what you get by applying PV=nRTPV = nRT to two states of the same fixed amount of gas and eliminating nn and RR between them — it is simply the equation of state applied twice and compared. Use PV=nRTPV = nRT when you know (or want to find) nn or RR explicitly, and use the combined gas law when you are relating two states of a sealed sample and do not care about nn at all.

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