Intuition What this page is
The parent note gave you the formula M 1 V 1 = M 2 V 2 and three examples. Here we hunt down every kind of question this one formula can throw at you — solve for each unknown, handle "add water" vs "boil water away", mix two solutions, hit the sneaky "concentration is a ratio not a sum" case, and the trap where a reaction happens so the formula must NOT be used. If you can do all of these, no exam version can surprise you.
Before line one: recall the only fact we ever use. Molarity M means "moles of solute divided by litres of solution", written M = V n , so n = M ⋅ V . The single unbreakable idea is: ==adding or removing pure solvent (water) never changes the number of solute particles n ==. Everything below is that sentence, rearranged.
Every dilution question is one cell of this grid. The columns are which unknown you solve for ; the rows are what physical situation creates the two states.
Situation ↓ \ Unknown →
Solve for M 2 (final conc.)
Solve for V 1 (start vol.)
Solve for volume of water
Add water (dilute)
Ex 1
Ex 4
Ex 2
Remove water (concentrate ↑)
Ex 3
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Ex 3
Mix two solutions
Ex 5 (weighted avg)
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Degenerate / limiting
Ex 6 (add nothing; add ∞ water)
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Trap: reaction consumes solute
Ex 7 (formula FAILS)
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—
Non-molarity unit (ppm)
Ex 8 (same logic, different unit)
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—
We hit every cell (the two dashes are combinations that are just Ex 4 / Ex 2 re-labelled). Each example says which cell it fills.
You take 25 mL of 4 M sulfuric acid and add water until the total is 200 mL . What is the final molarity?
Forecast: The volume grew from 25 to 200 mL — that is an 8 × jump. So guess the concentration falls by 8 × : about 4/8 = 0.5 M . Let's confirm.
Step 1. List what we know: M 1 = 4 , V 1 = 25 mL , V 2 = 200 mL , unknown M 2 .
Why this step? Three of the four slots in M 1 V 1 = M 2 V 2 are known, so the fourth is forced.
Step 2. Rearrange the formula for the unknown: divide both sides by V 2 .
M 2 = V 2 M 1 V 1 = 200 4 × 25
Why this step? We want M 2 alone; dividing by V 2 peels it off the right side.
Step 3. Compute: M 2 = 200 100 = 0.5 M .
Why this step? Just arithmetic on the numbers from Step 2.
Verify: Volume ratio V 1 V 2 = 25 200 = 8 , and concentration ratio M 2 M 1 = 0.5 4 = 8 . They match — concentration dropped by exactly the factor the volume rose. Units: mL cancelled mL, leaving M. ✔
How many millilitres of water must be added to 120 mL of 2.5 M KCl to bring it down to 0.75 M ?
Forecast: Concentration must fall by 2.5/0.75 ≈ 3.33 × , so the final volume is about 120 × 3.33 ≈ 400 mL , meaning roughly 280 mL of water. Careful — the formula gives the total , not the water.
Step 1. Find the final total volume V 2 : V 2 = M 2 M 1 V 1 = 0.75 2.5 × 120 .
Why this step? The formula relates the two total volumes. Water added is a separate, later subtraction.
Step 2. Compute: V 2 = 0.75 300 = 400 mL .
Why this step? Arithmetic; this is the whole solution after topping up.
Step 3. Water added = V 2 − V 1 = 400 − 120 = 280 mL .
Why this step? You already had 120 mL of liquid; only the extra 280 mL is new water.
Verify: Check the diluted solution really is 0.75 M: M 2 = 400 2.5 × 120 = 400 300 = 0.75 M. ✔ And 280 mL sits between "some water" and "less than the full 400 ", as expected.
Common mistake The classic slip here
Do not report 400 mL as "water added". V 2 is the total final volume ; the water is V 2 − V 1 . This is the single most missed step in dilution problems.
500 mL of 0.20 M glucose is left in an open dish and 300 mL of water evaporates. What is the new concentration, and did we add or remove solvent?
Forecast: We removed water, so volume shrinks 500 → 200 mL and concentration should rise . Volume fell by 2.5 × , so guess ≈ 0.20 × 2.5 = 0.5 M .
Step 1. New total volume V 2 = 500 − 300 = 200 mL .
Why this step? Evaporation removes solvent, so the total volume goes down by the amount lost — but the glucose molecules stay in the dish.
Step 2. Apply M 1 V 1 = M 2 V 2 (still valid — glucose was neither made nor destroyed, just less water):
M 2 = V 2 M 1 V 1 = 200 0.20 × 500
Why this step? Conservation of moles works for removing solvent exactly as for adding it — the moles are frozen either way.
Step 3. Compute: M 2 = 200 100 = 0.5 M .
Why this step? Arithmetic; concentration rose, as forecast.
Verify: Moles before = 0.20 × 0.500 L = 0.10 mol . Moles after = 0.50 × 0.200 L = 0.10 mol . Identical — the same 0.10 mol of glucose, now crowded into less water. ✔
You need 250 mL of 0.05 M HNO₃. Your stock bottle is 15.8 M . What volume of stock do you measure out (then top up to 250 mL )?
Forecast: Stock is enormously stronger (15.8 vs 0.05 ) — a ratio of about 316 × . So we need a tiny sip of stock: about 250/316 ≈ 0.8 mL .
Step 1. Identify the unknown as V 1 : here state 1 is the stock , state 2 is the final dilute solution . Known: M 1 = 15.8 , M 2 = 0.05 , V 2 = 250 mL .
Why this step? "Before" always means the more concentrated stock; "after" the diluted target.
Step 2. Rearrange for V 1 : V 1 = M 1 M 2 V 2 = 15.8 0.05 × 250 .
Why this step? Divide both sides by M 1 to isolate the stock volume.
Step 3. Compute: V 1 = 15.8 12.5 ≈ 0.79 mL of stock, then add water up to 250 mL.
Why this step? Arithmetic; the answer is tiny, matching the forecast.
Verify: Plug back: M 2 = 250 15.8 × 0.79 = 250 12.48 ≈ 0.05 M . ✔ Sanity: a very strong acid needs only a droplet to make a weak one — never trust an answer of "hundreds of mL of stock" here.
You pour together 200 mL of 3 M NaCl and 300 mL of 1 M NaCl. What is the concentration of the mixture? (Assume volumes just add.)
Forecast: The answer must land between 1 and 3 M — never below, never above. Since there is more of the weak solution, expect it closer to 1 than to 3 : maybe about 1.8 M .
Step 1. This is NOT a single M 1 V 1 = M 2 V 2 . Instead, conserve total moles by adding each solution's moles:
n total = M a V a + M b V b = ( 3 ) ( 200 ) + ( 1 ) ( 300 )
Why this step? Each solution carries its own moles; mixing pools them. You add moles, never molarities.
Step 2. Compute total "moles" (using mL, we'll divide by mL too so units are consistent): n total = 600 + 300 = 900 (mmol).
Why this step? Arithmetic; keeping mL throughout means the answer still comes out in mol/L.
Step 3. Total volume V total = 200 + 300 = 500 mL .
Why this step? Volumes are additive; that is the "spread into" step.
Step 4. Final concentration M mix = V total n total = 500 900 = 1.8 M .
Why this step? Molarity is total moles ÷ total volume — the definition, applied to the pooled system.
Verify: 1.8 lies between 1 and 3 , and closer to 1 (there was more of it). ✔ If you had wrongly added the molarities you'd get 4 M — impossible, since no part was stronger than 3 M. That is the trap the parent note's mistake box warns about.
Two edge cases on 100 mL of 2 M solution:
(a) Add zero water. (b) Add enormously much water — say dilute to 100 L . What are the concentrations, and what do these limits tell us?
Forecast: (a) Adding nothing changes nothing → still 2 M . (b) A huge volume should crush the concentration toward almost zero.
Step 1 (case a). V 2 = V 1 = 100 mL , so M 2 = V 2 M 1 V 1 = 100 2 × 100 = 2 M .
Why this step? When V 2 = V 1 the ratio V 1 / V 2 = 1 , so M 2 = M 1 . The formula correctly does nothing when you do nothing — a good self-check that it isn't magic.
Step 2 (case b). Convert: 100 L = 100000 mL . Then M 2 = 100000 2 × 100 = 100000 200 = 0.002 M .
Why this step? We must keep the same unit on both sides, so express both volumes in mL before dividing.
Step 3 (the limit). As V 2 → ∞ , M 2 = V 2 M 1 V 1 → 0 .
Why this step? The numerator M 1 V 1 (the fixed moles) is constant while the denominator explodes — a constant over a growing number heads to zero. Physically: the same solute smeared through an ocean is essentially undetectable, but never exactly zero (the solute never disappears).
Verify: Case (a): moles before = 2 × 0.1 = 0.2 mol, after = 2 × 0.1 = 0.2 mol — unchanged. ✔ Case (b): moles = 0.002 × 100 = 0.2 mol still. ✔ The conserved 0.2 mol survives every scenario — that is the whole point.
You mix 100 mL of 1 M HCl with 100 mL of 1 M NaOH. A student writes M 1 V 1 = M 2 V 2 and claims the HCl is now "0.5 M". Is this right?
Forecast: Something smells wrong — HCl and NaOH react : HCl + NaOH → NaCl + H 2 O . Solute is being consumed , not merely spread out.
Step 1. Count moles: HCl = 1 × 0.100 = 0.10 mol ; NaOH = 1 × 0.100 = 0.10 mol .
Why this step? We must check whether the "solute" still exists after mixing before any dilution formula can apply.
Step 2. They react 1 : 1 and are equal , so all 0.10 mol of HCl is neutralised. Remaining HCl = 0.10 − 0.10 = 0 mol .
Why this step? M 1 V 1 = M 2 V 2 assumes the moles of that species are conserved. Here they drop to zero — the assumption is broken.
Step 3. So the true HCl concentration afterward is 0 M , not 0.5 M. The correct tool for "who used up whom" is Titration and neutralisation / Normality and N1V1 = N2V2 at the equivalence point.
Why this step? When solute is destroyed by reaction, you switch from conservation-of-moles-of-one-species to stoichiometry.
Verify: Equivalence check via N 1 V 1 = N 2 V 2 (both are 1 N here): 1 × 100 = 1 × 100 — they exactly cancel, confirming zero excess of either. ✔ The naive 0.5 M answer would have been the dilution result if nothing reacted — it's the wrong model.
Common mistake When you may NOT use
M 1 V 1 = M 2 V 2
Only when solute is diluted or concentrated , never consumed . If two species react, use stoichiometry or N 1 V 1 = N 2 V 2 at equivalence.
A tank of pool water tests at 6 ppm chlorine. You pump in fresh water, changing the volume from 30 000 L to 50 000 L (no chlorine added). New ppm?
Forecast: More water, same chlorine → ppm falls. Volume rose by 50/30 ≈ 1.67 × , so guess 6/1.67 ≈ 3.6 ppm .
Step 1. Recognise ppm is also an "amount ÷ volume" measure (see ppm and parts-per notation ), so the dilution formula works with ppm in place of M :
C 1 V 1 = C 2 V 2
Why this step? The derivation only ever needed "amount is conserved". Any concentration-per-volume unit obeys it.
Step 2. Solve for C 2 : C 2 = V 2 C 1 V 1 = 50000 6 × 30000 .
Why this step? Isolate the unknown final concentration.
Step 3. Compute: C 2 = 50000 180000 = 3.6 ppm .
Why this step? Arithmetic; matches the forecast.
Verify: Chlorine "amount" before ∝ 6 × 30000 = 180000 ; after ∝ 3.6 × 50000 = 180000 . Equal — no chlorine created or lost. ✔
In a "how much water to add" problem, what do you compute first , before subtracting?
When you mix two solutions, do you add the molarities or the moles?
Why does removing water (evaporation) still obey M 1 V 1 = M 2 V 2 ?
When must you refuse to use the dilution formula?
Which volume is the total, not the water added? V 2 , the final total volume; water added = V 2 − V 1 .
Mixing 200 mL of 3 M with 300 mL of 1 M gives what concentration? 500 600 + 300 = 1.8 M.
Does evaporation break M 1 V 1 = M 2 V 2 ? No — removing solvent still conserves solute moles, so the formula holds.
When does the dilution formula fail? When the solute is chemically consumed (e.g. HCl + NaOH neutralisation) — use stoichiometry instead.
As V 2 → ∞ , what happens to M 2 ? It tends to 0 but never reaches it (fixed moles over growing volume).
Can you use the formula with ppm? Yes — any amount-per-volume unit obeys C 1 V 1 = C 2 V 2 .
Parent: Dilution formula — the derivation these examples exercise.
Molarity and concentration units — the M = n / V definition behind every step.
The Mole concept — moles n are the conserved quantity across all cases.
Normality and N1V1 = N2V2 — the tool for Example 7's reacting case.
Titration and neutralisation — where solute is consumed, not diluted.
ppm and parts-per notation — Example 8's alternative unit.