Intuition What this page is for
The parent note built the machinery: moles , molar mass, kelvin, and the derived units joule, pascal, litre. This page stress-tests that machinery against every kind of problem it can produce . Before each example you make a Forecast — a guess. Guessing first is how you find the gaps in your own understanding. If your forecast is wrong, that's the most valuable moment on the page.
A reminder of the four tools we lean on, from the parent topic :
n = M m — moles from mass (mass ÷ molar mass)
n = N A N — moles from a raw particle count
T K = T ∘ C + 273.15 — always convert temperature first
Every derived unit is base units in disguise: J = kg m 2 s − 2 , Pa = kg m − 1 s − 2 , 1 L = 1 0 − 3 m 3
Below is every class of situation this topic can throw at you. Each of the 8 examples that follow is tagged with the cell it covers, so the whole grid gets filled.
Cell
Case class
What makes it tricky
Example
A
Straight forward conversion (mass → mol → particles)
keeping mass units consistent
E1
B
Reverse direction (particles → mol → mass)
dividing by N A , not multiplying
E2
C
Unit trap: kg vs g in molar mass
the "molar mass is kg" myth
E3
D
Temperature: negative Celsius, absolute-zero limit
Celsius can be negative; kelvin cannot go below 0
E4
E
Volume scaling: L ↔ m³ ↔ cm³
cube of a length ratio
E5
F
Derived unit built from scratch (pressure, units only)
reading Pa off F / A
E6
G
Everything at once — ideal gas in pure SI (word problem)
convert L, °C, kPa all before plugging in
E7
H
Degenerate / limiting inputs (zero moles, zero kelvin, huge N )
what the formulas say at the edges
E8
Worked example E1 — Cell A: mass → moles → particles
How many molecules are in 8.8 g of carbon dioxide? (M CO 2 = 44 g/mol , N A = 6.022 × 1 0 23 mol − 1 .)
Forecast: Is the answer bigger or smaller than N A ? We have less than one molar mass of gas, so guess: fewer than 6 × 1 0 23 molecules.
n = M m = 44 8.8 = 0.2 mol .
Why this step? M is grams-per-mole, so grams ÷ (grams/mole) cancels grams and leaves moles.
N = n N A = 0.2 × 6.022 × 1 0 23 = 1.2044 × 1 0 23 molecules.
Why this step? One mole is N A particles, so n moles is n times that — pure proportionality.
Verify: 0.2 < 1 , so N < N A ✓ (matches the forecast). Units: mol × mol − 1 = dimensionless count ✓.
Worked example E2 — Cell B: particles → moles → mass (reverse!)
You are told a sample contains 3.011 × 1 0 23 atoms of gold (M Au = 197 g/mol ). What is its mass?
Forecast: 3.011 × 1 0 23 is exactly half of N A . So we expect half a molar mass ≈ 98–99 g.
n = N A N = 6.022 × 1 0 23 3.011 × 1 0 23 = 0.5 mol .
Why this step? Going from a raw count to moles means asking "how many N A -sized bundles?" — so we divide by N A (the classic reverse-direction trap: don't multiply).
m = n M = 0.5 × 197 = 98.5 g .
Why this step? Molar mass is grams per mole, so multiplying by moles gives grams back.
Verify: 98.5 g is half of 197 g ✓ — exactly the forecast. If you had multiplied by N A in step 1 you'd get an absurd 1 0 46 mol, an instant red flag.
Worked example E3 — Cell C: the kg-vs-g molar-mass trap
Compute n for 0.036 kg of water two ways — once keeping everything in grams , once in kg — and show they agree. (M H 2 O = 18 g/mol = 0.018 kg/mol .)
Forecast: The two methods must give the same n — moles is a count, it cannot depend on which mass unit we chose. Guess: same answer both times.
Grams route: m = 0.036 kg = 36 g , M = 18 g/mol .
n = 18 36 = 2 mol .
Why this step? Both m and M are now in grams, so grams cancel cleanly.
Kilograms route: m = 0.036 kg , M = 0.018 kg/mol .
n = 0.018 0.036 = 2 mol .
Why this step? Both m and M are now in kg, so kg cancel cleanly. The rule is not "use kg" — it's "use the SAME mass unit on top and bottom."
Verify: Both give 2 mol ✓. The myth "M must be kg" mixes units (36 g ÷ 0.018 kg/mol ) and gives 2000 — wrong by 1000 × , exactly the g↔kg factor.
Worked example E4 — Cell D: negative Celsius & the absolute-zero limit
(a) Convert − 40 ∘ C to kelvin. (b) Convert − 273.15 ∘ C to kelvin — what does the result mean? (c) Can a temperature of − 300 ∘ C exist?
Forecast: Kelvin is Celsius shifted up by 273.15. So a negative Celsius can still become a positive kelvin. And there should be a floor below which nothing exists.
T K = − 40 + 273.15 = 233.15 K .
Why this step? Same-size steps, shifted zero — we just add the offset. Note the answer is positive , even though °C was negative.
T K = − 273.15 + 273.15 = 0 K .
Why this step? This is absolute zero — zero thermal motion. It's the physical origin the kelvin scale was built around, which is exactly why the gas law uses kelvin.
− 300 ∘ C ⇒ − 300 + 273.15 = − 26.85 K — a negative kelvin.
Why this step? Negative kelvin means less-than-zero thermal motion, which is impossible. So − 300 ∘ C cannot exist ; the coldest possible is − 273.15 ∘ C .
Verify: (a) 233.15 > 0 ✓; (b) = 0 exactly ✓; (c) < 0 , flagged impossible ✓. See Kinetic Theory of Gases for why motion stops at 0 K .
Worked example E5 — Cell E: volume scaling L ↔ m³ ↔ cm³
A flask holds 250 mL . Express this in (a) litres, (b) cubic metres, (c) cubic centimetres, and confirm it is a cube of side ≈ 6.3 cm. See figure.
Forecast: 250 mL is a quarter-litre. In m³ it should be a tiny number (because 1 m 3 = 1000 L ), around 1 0 − 4 .
250 mL = 0.250 L .
Why this step? "milli" = 1 0 − 3 , so 250 mL = 250 × 1 0 − 3 L .
0.250 L = 0.250 × 1 0 − 3 m 3 = 2.5 × 1 0 − 4 m 3 .
Why this step? 1 L = 1 0 − 3 m 3 (a 10 cm cube inside a 1 m cube). Look at the red cube in the figure — it's a tiny corner of the black metre-cube.
0.250 L = 250 cm 3 (since 1 L = 1000 cm 3 ). Side of a cube of this volume: 3 250 = 6.30 cm .
Why this step? Volume is length cubed , so to get the side we take the cube root — the geometric inverse of cubing.
Verify: 6.299 6 3 = 250.0 cm 3 ✓, and 2.5 × 1 0 − 4 m 3 × 1000 = 0.250 L ✓. Tiny in m³ as forecast.
Worked example E6 — Cell F: build the pascal from base units alone
A block of ice pushes down with a force of 150 N on a table contact patch of 30 cm 2 . Find the pressure in Pa, and show the answer's units are kg·m⁻¹·s⁻² directly.
Forecast: Pressure = force ÷ area. Watch the area: 30 cm 2 is not 30 m 2 — converting will make the pressure bigger than a naive guess.
Convert area: 30 cm 2 = 30 × ( 1 0 − 2 m ) 2 = 30 × 1 0 − 4 m 2 = 3.0 × 1 0 − 3 m 2 .
Why this step? 1 cm = 1 0 − 2 m , and area is length squared , so the factor is ( 1 0 − 2 ) 2 = 1 0 − 4 .
p = A F = 3.0 × 1 0 − 3 150 = 5.0 × 1 0 4 Pa .
Why this step? Straight from the definition of pressure — the same push over a smaller patch means more pressure.
Units: m 2 N = m 2 kg m s − 2 = kg m − 1 s − 2 .
Why this step? Substituting the newton's base-unit spelling (N = kg m s − 2 ) and simplifying m / m 2 = m − 1 reads the pascal off the formula — no memorisation.
Verify: 5.0 × 1 0 4 Pa = 0.5 bar ✓ (divide by 1 0 5 ). Had we forgotten the cm² conversion we'd get 150/30 = 5 Pa — off by 1 0 4 , the area-scaling factor.
Worked example E7 — Cell G: everything at once (word problem, ideal gas in pure SI)
A weather balloon holds 12.0 L of helium at 27 ∘ C and a pressure of 95 kPa . How many moles of helium are inside? (R = 8.314 J mol − 1 K − 1 .) This is the meeting point of all four units — see Ideal Gas Law .
Forecast: Roughly room conditions, about half a mole of gas per 11 L is typical, and 12 L is near a half-mole scale. Guess: around 0.4–0.5 mol.
Convert every quantity to SI before touching the formula:
Volume: V = 12.0 L = 12.0 × 1 0 − 3 m 3 .
Temperature: T = 27 + 273.15 = 300.15 K .
Pressure: p = 95 kPa = 95 × 1 0 3 Pa = 9.5 × 1 0 4 Pa .
Why this step? R is written in joules, and a joule is Pa ⋅ m 3 . If any of p , V , T is in the "wrong" unit (L, °C, kPa), the joules won't cancel and the answer is garbage.
Rearrange p V = n R T for the unknown: n = R T p V .
Why this step? We want n alone, so divide both sides by R T .
n = ( 8.314 ) ( 300.15 ) ( 9.5 × 1 0 4 ) ( 12.0 × 1 0 − 3 ) = 2495.4 1140 = 0.457 mol .
Why this step? Numerator = p V = 1140 Pa⋅m 3 = 1140 J ; denominator = R T = 2495.4 J/mol ; joules cancel, leaving mol.
Verify: 0.457 mol lands inside the forecast 0.4–0.5 ✓. Units: J/mol J = mol ✓.
Worked example E8 — Cell H: degenerate and limiting inputs
Read each edge case and predict what the formula says.
(a) m = 0 g of any substance — how many moles and particles?
(b) A rigid 2.0 L sealed box at 0 K — what pressure does p V = n R T predict?
(c) If you had N = 6.022 × 1 0 25 atoms of neon (M = 20 g/mol ), what mass is that?
Forecast: Zero mass → zero of everything. Zero kelvin → the formula gives zero pressure (a limit, not a real gas). 1 0 25 is 100× N A , so expect ~100 mol = ~2 kg.
(a) n = M 0 = 0 mol , so N = 0 × N A = 0 particles.
Why this step? No matter of substance means no moles and no particles — the formulas degrade gracefully to zero, never divide-by-zero (we divide by M , not by m ).
(b) p = V n R T with T = 0 K gives p = 0 Pa .
Why this step? At absolute zero the model has no thermal motion, so no molecular impacts on the walls — pressure vanishes. (Real gases liquefy long before this; the ideal-gas limit is what's shown.)
(c) n = 6.022 × 1 0 23 6.022 × 1 0 25 = 100 mol , so m = 100 × 20 = 2000 g = 2 kg .
Why this step? N is exactly 100 × N A , so it's 100 mol; multiply by molar mass for grams.
Verify: (a) 0 and 0 ✓; (b) 0 Pa ✓; (c) 2000 g = 2 kg ✓, matching the ~2 kg forecast.
Recall Which formula, which direction?
Going mass → count you multiply by N A ; going count → mass you divide by N A ::: divide when going from a big raw count to moles; multiply when going from moles to a count
Before plugging into p V = n R T , what three conversions must you always check? ::: L → m³, °C → K, kPa/bar → Pa
Why did E3's two routes agree? ::: moles is a count; it cannot depend on whether mass was written in g or kg, as long as m and M share a unit
What does p V = n R T predict at T = 0 K ? ::: p = 0 — zero thermal motion, zero wall impacts
Mnemonic The pre-flight checklist for any gas problem
"Liters, Lids, Loads" → L itres to m³, temperature L id (kelvin), pressure L oad to pascals — do all three before the formula.