Audited ·Last updated 27 Jul 2026·5 citations·Tier 1·0 uses

Dilution Calculator (C1V1 = C2V2)

Free dilution calculator (C1V1=C2V2). Solve for initial or final concentration, or initial or final volume — any consistent unit, lab or industrial.

Dilution Calculator

Solve for
Concentration of the stock/starting solution. Any consistent unit works — mol/L, %, mg/mL, ppm, CFU/mL — as long as you use the same unit for C2. Required unless you are solving for this field.
Volume of stock solution taken for the dilution, in litres. Convert mL to L by dividing by 1000. Required unless you are solving for this field.
L
Desired concentration after dilution, in the same unit as C1. Required unless you are solving for this field.
Total volume after dilution (stock plus added diluent), in litres. Required unless you are solving for this field.
L
Solved value
0.05
The quantity you chose in 'Solve for' — computed from the other three via the dilution law C1V1 = C2V2.
Initial concentration (C1)
10
Initial (stock) volume (V1)
0.05 L
Final concentration (C2)
0.5
Final (total) volume (V2)
1 L
Diluent to add
0.95 L
Dilution factor
20

Background.

A dilution calculator solves the single most-used equation in wet-lab chemistry — the dilution law, C1 × V1 = C2 × V2 — for whichever of the four quantities you do not already know: the concentration of your stock solution (C1), the volume of stock you take (V1), the concentration you want after dilution (C2), or the total final volume you need (V2). Pick a 'solve for' mode, type in the other three values, and the calculator returns the missing one along with two practical extras: the volume of diluent (water, buffer, saline, solvent) you need to add, and the dilution factor, the single number lab technicians write on tube labels as a shorthand for how many times a stock was diluted.

The dilution law itself is nothing more than a statement of conservation. When you take V1 litres from a stock solution at concentration C1, you remove a fixed amount of solute — n = C1 × V1 units of it, whether those units are moles, milligrams, or colony-forming units. Adding solvent to bring the total volume up to V2 does not create or destroy any of that solute; it only spreads the same amount through a larger volume. The new concentration is therefore C2 = n / V2 = (C1 × V1) / V2, which rearranges into the familiar symmetric form C1V1 = C2V2. Because the law is a statement about a conserved quantity divided by a volume, it holds for any consistent pair of concentration and volume units — molarity in mol/L, percent solutions in % w/v, drug concentrations in mg/mL, environmental contaminant levels in parts per million, and bacterial or viral titres in colony-forming units or plaque-forming units per millilitre. This calculator is deliberately built to be unit-agnostic for exactly that reason: it is as useful to a microbiology student running a ten-fold serial dilution series as it is to an analytical chemist preparing a 0.01 M working standard from a 1 M stock.

Dilution calculations show up constantly outside the research bench, too. A pharmacist compounding a paediatric liquid dose from a concentrated adult formulation is solving a dilution problem. A pool-maintenance technician diluting concentrated chlorine stock to a target parts-per-million reading is solving a dilution problem. A cleaning-products manufacturer specifying '1 part concentrate to 40 parts water' on a bottle label has already solved the dilution problem for the end user and expressed the answer as a dilution factor. Home brewers diluting a hop extract, hydroponics growers diluting a nutrient concentrate to a target electrical-conductivity reading, and photography darkroom technicians diluting stock developer to a working strength are all running the identical C1V1 = C2V2 calculation, just with different instruments measuring the concentration axis.

Most general-purpose molarity calculators — including the molarity calculator elsewhere on this site — bundle a single dilution submode into a broader tool that also solves M = n/V, and that submode typically only answers one direction of the question: given a stock concentration, a stock volume, and a target concentration, what is the final volume? That is a common question, but it is not the only one. Equally common in practice is the inverse: given a stock concentration, a target concentration, and a target final volume, how much stock do you actually need to pipette? This calculator treats all four directions as equally first-class, because in a real protocol you often know the target concentration and target volume (dictated by the assay or recipe) and need to solve backward for how much stock to measure out — precisely the calculation a fixed single-direction tool cannot do without manual algebra.

Below the calculator you will find the full derivation of the dilution law from conservation of solute, a worked example preparing a 0.500 mol/L sodium hydroxide working solution from a 10.00 mol/L stock, guidance on choosing which of the four modes matches the data you actually have, an explanation of dilution factor and how serial dilutions chain multiple dilution factors multiplicatively, and safety notes for diluting concentrated acids and bases. The solver itself runs on Decimal.js arbitrary-precision arithmetic and is registered at dilution.calculate in the Quanta engine, with every mode validated against division-by-zero and non-positive concentration or volume inputs.

What is dilution calculator?

Dilution is the process of reducing the concentration of a solute in a solution, almost always by adding more solvent while holding the amount of solute fixed. The dilution law, C1V1 = C2V2, is the mathematical expression of that process: C1 and V1 are the concentration and volume of the solution before dilution (the 'stock' or 'initial' state), and C2 and V2 are the concentration and total volume after dilution (the 'working' or 'final' state). The law follows directly from the definition of concentration as amount of solute per unit volume: amount of solute n = C × V is fixed by the act of taking an aliquot from the stock, and diluting changes only the volume it occupies, not the amount itself, so C1V1 (the amount taken from stock) must equal C2V2 (the same amount now expressed at the new, larger volume). Two closely related quantities appear throughout dilution work. The volume of diluent to add is simply V2 − V1 — the amount of solvent you pour in after measuring out your V1 aliquot of stock. The dilution factor, commonly written DF, is V2 / V1 (equivalently C1 / C2): a dilution factor of 10 means the final volume is ten times the aliquot volume, so the concentration has dropped to one-tenth of the stock value. Dilution factors are typically reported as a ratio, '1:10' or '1-in-10', meaning one part stock combined with enough diluent to reach ten total parts — not one part stock to ten parts diluent, a common point of confusion. Serial dilutions chain this idea: taking a 1-in-10 dilution and diluting it 1-in-10 again produces an overall 1-in-100 dilution, because dilution factors multiply along the chain (10 × 10 = 100), which is exactly how microbiologists prepare the wide concentration range needed to get a countable number of colonies on an agar plate from an unknown, highly concentrated bacterial culture.

How to use this calculator.

  1. Pick the one quantity you don't know from the 'Solve for' menu: initial (stock) volume, final volume, final concentration, or initial (stock) concentration.
  2. Fill in the other three fields. The calculator ignores whichever field you are solving for — you can leave it at its default.
  3. Use any consistent unit for the two concentration fields (mol/L, %, mg/mL, ppm, CFU/mL) and any consistent unit for the two volume fields — the calculator's math is unit-agnostic, but C1 and C2 must share a unit, and V1 and V2 must share a unit (litres, by default, on this page; convert mL to L by dividing by 1000).
  4. Read the primary result (the value you solved for) plus the full echoed quartet of C1, V1, C2, V2 underneath it.
  5. Check 'Diluent to add' (V2 − V1) for the practical answer to 'how much water do I pour in?' and 'Dilution factor' (V2 / V1) for the lab-notebook shorthand.
  6. For serial dilutions, chain the calculator: use the final volume of one dilution step as the starting point for planning the next, and multiply the individual dilution factors to get the overall dilution across the whole series.
  7. Safety: when diluting concentrated acids or bases, always add the concentrated reagent to the larger volume of water, never the reverse — the dissolution/mixing is exothermic and can spatter if water is added to a concentrated acid.

The formula.

C₁V₁ = C₂V₂

The dilution law is a direct consequence of two definitions: concentration is amount of solute per unit volume, and diluting a solution does not add or remove solute. Start from C = n / V, so the amount of solute in a stock aliquot is n = C1 × V1. When that aliquot is diluted to a total volume V2, the amount of solute is unchanged — it is still n — but it is now expressed in a larger volume, so the new concentration is C2 = n / V2. Substituting n = C1V1 into C2 = n/V2 gives C2 = C1V1/V2, which rearranges into the symmetric form C1V1 = C2V2. Every one of the calculator's four modes is this single identity solved for a different unknown: V1 = C2V2/C1, V2 = C1V1/C2, C2 = C1V1/V2, and C1 = C2V2/V1.

Two secondary quantities follow immediately. The volume of diluent to add is V2 − V1, because the total final volume is made up of the original stock aliquot plus whatever solvent you pour in afterward. The dilution factor is V2 / V1 — equivalently, by the dilution law, C1 / C2 — a single dimensionless number describing how many times more dilute the final solution is relative to the stock. Because the dilution law is homogeneous in the concentration units (C1 and C2 always appear as a ratio or together in a product with matching volumes), the equation is exactly as valid for mass-percent concentrations, ppm, or colony-forming-unit titres as it is for molarity — nothing in the derivation assumes moles or litres specifically, only that whatever unit you choose for concentration is used consistently on both sides and whatever unit you choose for volume is used consistently on both sides.

Serial dilutions extend the same logic across multiple steps. If a first dilution has factor DF1 = V2,1/V1,1 and the resulting solution is itself diluted again with factor DF2 = V2,2/V1,2, the overall dilution factor relative to the original stock is DF1 × DF2, because each step divides the concentration by its own factor in sequence: C_final = C_original / (DF1 × DF2). This multiplicative chaining is why microbiologists can span nine or ten orders of magnitude in concentration with only nine or ten pipetting steps, each an easy-to-execute 1-in-10 dilution.

A worked example.

Example

A lab technician needs 1.000 L of a 0.500 mol/L sodium hydroxide (NaOH) working solution and has a 10.00 mol/L NaOH stock on the shelf. Selecting 'Solve for: Initial (stock) volume' and entering C1 = 10.00, C2 = 0.500, and V2 = 1.000, the calculator applies V1 = C2 × V2 / C1 = 0.500 × 1.000 / 10.00 = 0.05000 L — that is, 50.00 mL of the 10 M stock. It also reports the diluent to add, V2 − V1 = 1.000 − 0.050 = 0.950 L (950 mL of water), and the dilution factor, V2 / V1 = 1.000 / 0.050 = 20, meaning this is a 1-in-20 dilution of the stock. In practice, the technician measures exactly 50.00 mL of the 10 M stock into a 1 L volumetric flask, then tops up carefully to the 1.000 L mark with water — not by adding 950 mL of water directly, since the total volume of a mixture is not always precisely additive at the milliliter level, and a volumetric flask's calibration mark is what defines the true final volume. As a check on the other three modes: given C1 = 10.00, V1 = 0.05000, C2 = 0.500 the calculator's 'solve for finalVolume' mode returns V2 = 1.000 L; given V1 = 0.05000, C2 = 0.500, V2 = 1.000 the 'solve for initialConcentration' mode returns C1 = 10.00 mol/L — all three alternate modes reproduce the same self-consistent dilution exactly, which is the internal cross-check the calculator's own test suite relies on.

final Concentration0.5
final Volume1
initial Concentration10
solve ForinitialVolume

Frequently asked questions.

What is the dilution equation C1V1 = C2V2?
It is the mathematical statement that the amount of solute in a solution does not change when you dilute it — only the volume it occupies changes. C1 and V1 are the concentration and volume before dilution (the stock), and C2 and V2 are the concentration and volume after dilution (the working solution). Because amount of solute equals concentration times volume, and that amount is conserved through dilution, C1 times V1 must equal C2 times V2. The equation works for any consistent unit of concentration (molarity, percent, mg/mL, ppm) as long as C1 and C2 share the same unit, and any consistent unit of volume as long as V1 and V2 share the same unit.
How do I know which variable to solve for?
Solve for whichever quantity your protocol or problem does not already specify. If you know your stock concentration, how much of it you're taking, and want to know the final volume needed to hit a target concentration, solve for final volume (V2). If you know your stock concentration and want a specific final volume at a specific target concentration, solve for initial (stock) volume (V1) — this is the most common real-lab question, 'how much stock do I pipette?' If you diluted a fixed stock aliquot to a known final volume and want to know what concentration resulted, solve for final concentration (C2). If you're back-calculating an unknown stock concentration from a dilution you already performed and measured, solve for initial concentration (C1).
Why does this calculator work for percent solutions and ppm, not just molarity?
Because the dilution law is derived purely from conservation of the amount of solute divided by volume — nothing in the derivation is specific to moles. If C1 and C2 are both expressed as percent w/v, the same C1V1 = C2V2 equation gives the correct dilution. If both are expressed in parts per million, milligrams per millilitre, or colony-forming units per millilitre, it still holds. The only requirement is internal consistency: C1 and C2 must be in the same unit as each other, and V1 and V2 must be in the same unit as each other. Mixing units — entering C1 in mol/L and C2 in mg/mL without converting — will silently produce a meaningless answer, because the calculator has no way to know the units you intended.
What is a dilution factor, and how is it written?
The dilution factor (DF) is the final volume divided by the volume of stock used, DF = V2 / V1, which by the dilution law also equals C1 / C2. A dilution factor of 20 means the final solution is 20 times more dilute than the stock. Dilution factors are conventionally written as a ratio, '1:20' or '1-in-20', meaning one part of stock is combined with enough diluent to reach a total of 20 parts — this is a common point of confusion, because it is NOT one part stock to 20 parts diluent (that would be a 1:21 dilution, DF = 21). This calculator always reports the correct V2/V1 definition.
How do serial dilutions work, and how do the dilution factors combine?
A serial dilution is a chain of individual dilutions, each one performed on the product of the previous step rather than on the original stock. If step one has dilution factor DF1 and step two (applied to the output of step one) has dilution factor DF2, the overall dilution factor relative to the very first stock is the product DF1 × DF2. Ten successive 1-in-10 dilutions therefore produce an overall 1-in-10,000,000,000 (10^10) dilution — this is exactly how microbiologists count colony-forming units in a highly concentrated bacterial culture: dilute in a series of easy 10× steps until a plate yields a countable number of colonies, then multiply back through the chain of dilution factors to recover the original concentration.
What happens if I enter a target concentration higher than my stock concentration?
The calculator will still return a mathematically valid answer, but it describes a concentrating step, not a dilution — physically, you cannot increase a solution's concentration just by adding more solvent. If you solve for final volume (V2) with C2 > C1, the calculator returns a V2 smaller than V1, and 'Diluent to add' will be negative, which is the calculator's signal that your inputs describe concentrating rather than diluting. In real lab work, concentrating a solution requires removing solvent (evaporation, lyophilization) or adding more solute, not the dilution workflow this calculator models.
How is this different from the dilution mode built into the molarity calculator?
The molarity calculator's dilution submode is scoped to molar concentration (mol/L) and answers only one direction: given a stock concentration, a stock volume, and a target concentration, what final volume results? This dilution calculator solves the same underlying law but in all four directions — including the common inverse question, 'given a target concentration and target final volume, how much stock do I need?' — and is deliberately unit-agnostic so it works equally well for percent solutions, ppm, and microbiological titres, not only molarity. Use the molarity calculator when you also need the mass-to-moles conversion via molar mass in the same workflow; use this calculator for a standalone, any-unit, any-direction dilution.
Why should I add acid to water rather than water to acid when diluting?
Dissolving a concentrated acid (or base) in water releases heat, and the amount of heat released per unit volume of water is what matters for safety. If you add a small amount of water to a large amount of concentrated acid, that small amount of water heats up rapidly and can boil almost instantly, turning to steam violently enough to eject droplets of concentrated acid — this is the classic laboratory 'acid splash' accident. Adding the concentrated acid slowly to a larger volume of water instead means the heat is dissipated into a much larger thermal mass, keeping the temperature rise gradual and controlled. The mnemonic taught in every introductory chemistry lab is 'add acid to water, never water to acid,' and it applies to any exothermic dilution, not only mineral acids.
Can I use this calculator for mass-based dilutions instead of volume-based ones?
The equation itself, C1V1 = C2V2, is written for volumes because it comes from the definition of concentration as amount per unit volume, but an analogous conservation equation holds for mass-based dilutions of a solid or a viscous liquid: C1m1 = C2m2, where m1 and m2 are masses instead of volumes. If your dilution is genuinely mass-based (diluting a concentrated mass fraction of an ointment or a powder with an inert diluent by mass, for example), you can still use this calculator by entering your masses into the volume fields — the arithmetic is identical, only the physical interpretation of V1 and V2 changes from 'volume' to 'mass'. Just make sure both mass values use the same unit.

References& sources.

  1. [1]IUPAC Gold Book, 'amount-of-substance concentration, c' — the formal IUPAC definition of concentration, c = n/V, underlying the dilution law's conservation-of-solute derivation. International Union of Pure and Applied Chemistry.
  2. [2]Harvey, D.T. Analytical Chemistry 2.1, §2.5 'Preparing Solutions' — derives the dilution law C_o × V_o = C_d × V_d from conservation of the amount of solute and gives worked dilution examples. LibreTexts / DePauw University.
  3. [3]NIST Chemistry WebBook — searchable reference database of molar masses, concentrations, and physical property data used to cross-check dilution calculations for real compounds. National Institute of Standards and Technology, Standard Reference Database 69.
  4. [4]Skoog, D.A., West, D.M., Holler, F.J. & Crouch, S.R. (2013). Fundamentals of Analytical Chemistry, 9th ed. Cengage. Chapter 4 covers concentration units, dilution calculations, and standard laboratory dilution practice. ISBN 978-0495558286.
  5. [5]Atkins, P.W. & de Paula, J. (2014). Atkins' Physical Chemistry, 10th ed. Oxford University Press. Foundations section on amount of substance and molar concentration, the basis for the conservation argument behind C1V1 = C2V2.

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