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)
- 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.
- 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.
- 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.
- 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.
- Solve algebraically before plugging numbers (reduces mistakes).
B. Partial pressures (mixtures) procedure
- Determine which law applies:
- For mixtures of ideal gases: Dalton’s law: P_{\text{tot}} = \sum_i P_i.
- If you know moles, use mole fraction:
- x_i = \frac{n_i}{n_{\text{tot}}} and P_i = x_i P_{\text{tot}}.
- 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)
| Relationship | Formula | When to use | Notes |
|---|---|---|---|
| Ideal Gas Law | PV = nRT | Universal go-to for ideal gases | Works best at low P, high T; use consistent units |
| Molecular form | PV = Nk_B T | When given molecules, not moles | N = nN_A |
| Combined Gas Law | \frac{P_1V_1}{T_1} = \frac{P_2V_2}{T_2} | Sealed sample (constant n) with multiple changes | Derived from Boyle/Charles/Gay-Lussac |
| Boyle’s Law | P_1V_1=P_2V_2 | Constant T and n | Inverse: P \propto \frac{1}{V} |
| Charles’s Law | \frac{V_1}{T_1}=\frac{V_2}{T_2} | Constant P and n | Direct: V \propto T |
| Gay-Lussac’s Law | \frac{P_1}{T_1}=\frac{P_2}{T_2} | Constant V and n | Direct: P \propto T |
| Avogadro’s Law | \frac{V_1}{n_1}=\frac{V_2}{n_2} | Constant P and T | Direct: V \propto n |
Constants + unit anchors (know these cold)
| Constant | Value | Use |
|---|---|---|
| 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 constant | k_B = 1.381\times 10^{-23}\,\text{J/K} | Microscopic form PV=Nk_BT |
| Avogadro’s number | N_A = 6.022\times 10^{23}\,\text{mol}^{-1} | Converts n \leftrightarrow N |
| Atmosphere to pascal | 1\,\text{atm} = 1.013\times 10^5\,\text{Pa} | Pressure conversion |
| Liter to cubic meter | 1\,\text{L} = 10^{-3}\,\text{m}^3 | Volume conversion |
Gas mixtures (Dalton’s law)
| Rule | Formula | When to use | Notes |
|---|---|---|---|
| Dalton’s law | P_{\text{tot}} = \sum_i P_i | Mixture of nonreacting ideal gases | Each gas “acts alone” |
| Partial pressure via mole fraction | P_i = x_i P_{\text{tot}}, x_i = \frac{n_i}{n_{\text{tot}}} | Given moles/ratios | Same T and V for all gases in mixture |
| Gas over water correction | P_{\text{dry}}=P_{\text{tot}}-P_{\text{H}_2\text{O}} | Collection over water | P_{\text{H}_2\text{O}} depends on temperature |
Kinetic theory connections (often tested conceptually + quantitatively)
| Idea | Formula | What it tells you | Notes |
|---|---|---|---|
| Mean translational KE (per molecule) | \langle K \rangle = \frac{3}{2}k_BT | Temperature measures average molecular KE | Independent of gas type |
| Mean translational KE (per mole) | \langle K \rangle_{\text{mol}} = \frac{3}{2}RT | Same idea, per mole | Useful with n |
| RMS speed | v_{\text{rms}}=\sqrt{\frac{3k_BT}{m}}=\sqrt{\frac{3RT}{M}} | Typical molecular speed | m = mass per molecule, M = molar mass in \text{kg/mol} |
| Pressure–speed relation | P=\frac{1}{3}\rho v_{\text{rms}}^2 | Links macroscopic P to microscopic motion | \rho is mass density |
Internal energy for ideal gases (ties gas laws to thermodynamics)
| Gas model | Internal energy U | When used | Notes |
|---|---|---|---|
| Ideal gas (general) | U=\frac{f}{2}nRT | If degrees of freedom f given/assumed | Depends only on T for ideal gas |
| Monatomic ideal gas | U=\frac{3}{2}nRT | Common AP assumption | f=3 |
| Diatomic (room temp approx.) | U\approx\frac{5}{2}nRT | Sometimes used | Rotational 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).
| Process | Condition | Key relation | Notes |
|---|---|---|---|
| Isothermal | T constant | PV=\text{const} | Same as Boyle for ideal gas |
| Isobaric | P constant | \frac{V}{T}=\text{const} | Same as Charles |
| Isochoric | V constant | \frac{P}{T}=\text{const} | Same as Gay-Lussac |
| Adiabatic (ideal gas) | Q=0 | PV^{\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
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.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).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.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.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).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}.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.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 / mnemonic | What it helps you remember | When to use it |
|---|---|---|
| “K for Kelvin” | Always use absolute temperature | Any gas law problem |
| “B-C-G” (Boyle–Charles–Gay-Lussac) | Which variable pairs with T depending on what’s constant | Quick identification of simple laws |
| “Same T → same average KE” | \langle K \rangle = \frac{3}{2}k_BT depends only on T | Kinetic theory / conceptual MCQ |
| “Lighter → faster” | v_{\text{rms}}\propto 1/\sqrt{M} | RMS speed comparisons |
| “Parts add to whole” | P_{\text{tot}}=\sum P_i | Dalton’s law mixture problems |
| Ratio sanity check | If V decreases and T fixed, P must increase | Avoid 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.