Key Gas Law Equations to Know for AP Physics 2 (2025) (AP)

What You Need to Know

Gas-law questions in AP Physics 2 are mostly about connecting macroscopic variables—pressure P, volume V, temperature T, amount of gas n (moles) or N (molecules)—and using those relationships to predict what changes when the gas is heated, compressed, mixed, or moved through a thermodynamic process.

The “big idea” you lean on repeatedly:

  • Ideal Gas Model (works well for low-density gases):
    PV = nRT = Nk_B T

If you know when you can treat n as constant (sealed container) vs changing (adding/removing gas), and you keep units consistent (especially **Kelvin** for T), you’ll be able to handle most AP-style gas-law setups.

Critical reminder: Temperature in gas laws is always absolute temperature: T_{K} = T_{\circ C} + 273.15.


Step-by-Step Breakdown

A. Choosing the right gas-law equation (fast decision tree)

  1. List what’s given and what changes: identify P_1, V_1, T_1, n_1 and P_2, V_2, T_2, n_2.
  2. Decide if the amount of gas is constant:
    • Sealed container (no leaks, no gas added): n constant.
    • Open system, adding gas, chemical reaction producing gas: n changes.
  3. Pick the simplest law:
    • If T constant (isothermal): use Boyle’s: P_1 V_1 = P_2 V_2.
    • If P constant (isobaric): use Charles’s: \frac{V_1}{T_1} = \frac{V_2}{T_2}.
    • If V constant (isochoric): use Gay-Lussac’s: \frac{P_1}{T_1} = \frac{P_2}{T_2}.
    • If n constant but multiple variables change: use combined gas law:
      \frac{P_1 V_1}{T_1} = \frac{P_2 V_2}{T_2}
    • If n not constant (or you want a one-step universal setup): use ideal gas law:
      PV = nRT.
  4. Convert units early:
    • T to Kelvin.
    • P to Pa if you’re using R = 8.314\,\text{J/(mol·K)}.
    • V to \text{m}^3 for SI.
  5. Solve algebraically before plugging numbers (reduces mistakes).

B. Partial pressures (mixtures) procedure

  1. Determine which law applies:
    • For mixtures of ideal gases: Dalton’s law: P_{\text{tot}} = \sum_i P_i.
  2. If you know moles, use mole fraction:
    • x_i = \frac{n_i}{n_{\text{tot}}} and P_i = x_i P_{\text{tot}}.
  3. If gas is collected over water (common lab context):
    • P_{\text{gas}} = P_{\text{tot}} - P_{\text{H}_2\text{O}}.

Quick worked mini-example (method in action)

A sealed syringe: V_1 = 30\,\text{mL}, P_1 = 1.0\,\text{atm}, compressed to V_2 = 10\,\text{mL} at constant T. Find P_2.

  • Constant T and constant n → Boyle’s law: P_1V_1=P_2V_2.
  • Solve: P_2 = P_1\frac{V_1}{V_2} = (1.0\,\text{atm})\frac{30}{10} = 3.0\,\text{atm}.

Key Formulas, Rules & Facts

Core gas laws (macroscopic relationships)

RelationshipFormulaWhen to useNotes
Ideal Gas LawPV = nRTUniversal go-to for ideal gasesWorks best at low P, high T; use consistent units
Molecular formPV = Nk_B TWhen given molecules, not molesN = nN_A
Combined Gas Law\frac{P_1V_1}{T_1} = \frac{P_2V_2}{T_2}Sealed sample (constant n) with multiple changesDerived from Boyle/Charles/Gay-Lussac
Boyle’s LawP_1V_1=P_2V_2Constant T and nInverse: P \propto \frac{1}{V}
Charles’s Law\frac{V_1}{T_1}=\frac{V_2}{T_2}Constant P and nDirect: V \propto T
Gay-Lussac’s Law\frac{P_1}{T_1}=\frac{P_2}{T_2}Constant V and nDirect: P \propto T
Avogadro’s Law\frac{V_1}{n_1}=\frac{V_2}{n_2}Constant P and TDirect: V \propto n

Constants + unit anchors (know these cold)

ConstantValueUse
Ideal gas constant (SI)R = 8.314\,\text{J/(mol·K)}Best with P in Pa and V in \text{m}^3
Ideal gas constant (atm·L)R = 0.08206\,\text{L·atm/(mol·K)}Only if everything is in atm and L
Boltzmann constantk_B = 1.381\times 10^{-23}\,\text{J/K}Microscopic form PV=Nk_BT
Avogadro’s numberN_A = 6.022\times 10^{23}\,\text{mol}^{-1}Converts n \leftrightarrow N
Atmosphere to pascal1\,\text{atm} = 1.013\times 10^5\,\text{Pa}Pressure conversion
Liter to cubic meter1\,\text{L} = 10^{-3}\,\text{m}^3Volume conversion

Gas mixtures (Dalton’s law)

RuleFormulaWhen to useNotes
Dalton’s lawP_{\text{tot}} = \sum_i P_iMixture of nonreacting ideal gasesEach gas “acts alone”
Partial pressure via mole fractionP_i = x_i P_{\text{tot}}, x_i = \frac{n_i}{n_{\text{tot}}}Given moles/ratiosSame T and V for all gases in mixture
Gas over water correctionP_{\text{dry}}=P_{\text{tot}}-P_{\text{H}_2\text{O}}Collection over waterP_{\text{H}_2\text{O}} depends on temperature

Kinetic theory connections (often tested conceptually + quantitatively)

IdeaFormulaWhat it tells youNotes
Mean translational KE (per molecule)\langle K \rangle = \frac{3}{2}k_BTTemperature measures average molecular KEIndependent of gas type
Mean translational KE (per mole)\langle K \rangle_{\text{mol}} = \frac{3}{2}RTSame idea, per moleUseful with n
RMS speedv_{\text{rms}}=\sqrt{\frac{3k_BT}{m}}=\sqrt{\frac{3RT}{M}}Typical molecular speedm = mass per molecule, M = molar mass in \text{kg/mol}
Pressure–speed relationP=\frac{1}{3}\rho v_{\text{rms}}^2Links macroscopic P to microscopic motion\rho is mass density

Internal energy for ideal gases (ties gas laws to thermodynamics)

Gas modelInternal energy UWhen usedNotes
Ideal gas (general)U=\frac{f}{2}nRTIf degrees of freedom f given/assumedDepends only on T for ideal gas
Monatomic ideal gasU=\frac{3}{2}nRTCommon AP assumptionf=3
Diatomic (room temp approx.)U\approx\frac{5}{2}nRTSometimes usedRotational modes active, vibrational often ignored

Common “process” equations that pair with ideal gas law

These show up when a problem describes a thermodynamic path (even if it calls it “gas law” reasoning).

ProcessConditionKey relationNotes
IsothermalT constantPV=\text{const}Same as Boyle for ideal gas
IsobaricP constant\frac{V}{T}=\text{const}Same as Charles
IsochoricV constant\frac{P}{T}=\text{const}Same as Gay-Lussac
Adiabatic (ideal gas)Q=0PV^{\gamma}=\text{const}Typically beyond “simple” gas laws, but shows up in AP thermodynamics; \gamma=\frac{C_P}{C_V}

If you’re not explicitly told the process (isothermal, etc.), don’t assume it—use what’s stated about what is held constant.


Examples & Applications

Example 1: Combined gas law (sealed sample)

A sealed can of air: P_1=2.0\times 10^5\,\text{Pa}, T_1=300\,\text{K}. It’s heated to T_2=450\,\text{K} with constant volume. Find P_2.

  • Constant V and n → \frac{P}{T}=\text{const}.
  • P_2 = P_1\frac{T_2}{T_1} = (2.0\times 10^5)\frac{450}{300} = 3.0\times 10^5\,\text{Pa}.

AP-style insight: at fixed V, pressure scales linearly with absolute temperature.

Example 2: Ideal gas law to find moles (units trap)

A scuba tank has V=12\,\text{L}, P=2.0\times 10^7\,\text{Pa}, T=300\,\text{K}. How many moles of air? (Treat as ideal.)

  • Convert volume: V = 12\times 10^{-3}\,\text{m}^3.
  • Use PV=nRT:
    n=\frac{PV}{RT}=\frac{(2.0\times 10^7)(12\times 10^{-3})}{(8.314)(300)}\approx 96\,\text{mol}.

Exam angle: The hard part is usually not algebra—it’s consistent SI units.

Example 3: Dalton’s law + mole fraction

A container at T and V holds n_{\text{He}}=1.0\,\text{mol} and n_{\text{Ne}}=3.0\,\text{mol}. Total pressure is P_{\text{tot}}=400\,\text{kPa}. Find P_{\text{He}}.

  • Mole fraction: x_{\text{He}}=\frac{1.0}{1.0+3.0}=0.25.
  • Partial pressure: P_{\text{He}}=x_{\text{He}}P_{\text{tot}}=(0.25)(400\,\text{kPa})=100\,\text{kPa}.

AP-style insight: partial pressures depend on mole fractions, not molar masses.

Example 4: RMS speed comparison (temperature + molar mass)

At the same T, compare v_{\text{rms}} for helium (molar mass M_{\text{He}}=0.004\,\text{kg/mol}) and nitrogen (M_{\text{N}_2}=0.028\,\text{kg/mol}).

  • v_{\text{rms}}\propto \frac{1}{\sqrt{M}} at fixed T.
  • Ratio:
    \frac{v_{\text{rms,He}}}{v_{\text{rms,N}_2}}=\sqrt{\frac{M_{\text{N}_2}}{M_{\text{He}}}}=\sqrt{\frac{0.028}{0.004}}=\sqrt{7}\approx 2.65.

Common exam prompt: “Which gas has higher typical molecular speed at the same temperature?” (Lighter molar mass → faster.)


Common Mistakes & Traps

  1. Forgetting Kelvin (using T_{\circ C} directly)
    What goes wrong: You’ll predict the wrong proportional changes (sometimes even negative temperatures).
    Fix: Always convert with T_K = T_{\circ C}+273.15.

  2. Mixing unit systems for R
    What goes wrong: Using R=8.314 with P in atm and V in L gives nonsense.
    Fix: Either go full SI (Pa, \text{m}^3, K, R=8.314) or full atm·L (atm, L, K, R=0.08206).

  3. Using the combined gas law when n changes
    What goes wrong: \frac{PV}{T} is only constant if n is constant.
    Fix: If gas can enter/leave or moles change, use PV=nRT with explicit n.

  4. Assuming “constant pressure” just because the container is open
    What goes wrong: In an open container, the gas can exchange with the environment, but the details matter; pressure may be atmospheric, but the amount of gas may change.
    Fix: Write what you know: if truly open to atmosphere, you can often take P\approx P_{\text{atm}}, but then n is not fixed.

  5. Confusing partial pressure with “fraction of volume” in non-identical conditions
    What goes wrong: P_i=x_iP_{\text{tot}} assumes a well-mixed ideal gas at common T and V.
    Fix: Only use mole fraction relations when the mixture shares the same container (same T, V).

  6. Using molar mass in \text{g/mol} inside v_{\text{rms}}
    What goes wrong: A factor of \sqrt{1000} error in speed.
    Fix: In v_{\text{rms}}=\sqrt{\frac{3RT}{M}}, M must be in \text{kg/mol}.

  7. Thinking “higher pressure means higher temperature” (without constraints)
    What goes wrong: Pressure can increase due to decreased volume at constant temperature (Boyle).
    Fix: Always state which variables are held constant before inferring relationships.

  8. Sign errors and conceptual slips with “compression” and “expansion”
    What goes wrong: You might invert ratios like \frac{V_1}{V_2}.
    Fix: Do a quick sanity check: compressing means V_2


Memory Aids & Quick Tricks

Trick / mnemonicWhat it helps you rememberWhen to use it
K for KelvinAlways use absolute temperatureAny gas law problem
B-C-G” (Boyle–Charles–Gay-Lussac)Which variable pairs with T depending on what’s constantQuick identification of simple laws
Same T → same average KE\langle K \rangle = \frac{3}{2}k_BT depends only on TKinetic theory / conceptual MCQ
Lighter → fasterv_{\text{rms}}\propto 1/\sqrt{M}RMS speed comparisons
Parts add to wholeP_{\text{tot}}=\sum P_iDalton’s law mixture problems
Ratio sanity checkIf V decreases and T fixed, P must increaseAvoid algebra flips in Boyle/combined

Quick Review Checklist

  • You can write and use PV=nRT and know what each symbol means.
  • You automatically convert to Kelvin: T_K=T_{\circ C}+273.15.
  • You keep units consistent with your chosen R (SI vs atm·L).
  • You know when \frac{PV}{T} is constant: only when n is constant.
  • You can recognize special cases:
    • Isothermal: P_1V_1=P_2V_2
    • Isochoric: \frac{P_1}{T_1}=\frac{P_2}{T_2}
    • Isobaric: \frac{V_1}{T_1}=\frac{V_2}{T_2}
  • You can do mixture problems with Dalton’s law: P_{\text{tot}}=\sum P_i and P_i=x_iP_{\text{tot}}.
  • You can connect microscopic and macroscopic ideas:
    • \langle K \rangle = \frac{3}{2}k_BT
    • v_{\text{rms}}=\sqrt{\frac{3RT}{M}} (with M in \text{kg/mol})
  • You do a quick sanity check: compress → P up (if T constant), heat at constant V → P up.

You’ve got this—gas laws are mostly pattern recognition plus clean units.