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Molality calculator

Compute molality — moles of solute per kilogram of solvent — the concentration unit that, unlike molarity, does not change with temperature. Enter moles directly or a mass with its molar mass, plus the solvent mass, and it returns the molality in mol/kg.

Beer-Lambert law calculatorSolve the Beer-Lambert law A = ε·c·l for any variable — absorbance, molar absorptivity, concentration or path length. Central to spectrophotometry, it links how much light a solution absorbs to how concentrated it is. Pick what to solve for, enter the rest, and read the answer.Normality calculatorCompute the normality of a solution — gram-equivalents of solute per litre. Enter equivalents directly or a mass with its molar mass and n-factor, plus the volume, and it returns the normality (N) and the equivalent molarity (M = N ÷ n-factor).Titration calculatorSolve acid-base titrations with the equivalence relation M₁V₁n₁ = M₂V₂n₂, which accounts for polyprotic acids and bases through their equivalents. Find an unknown analyte molarity from the titrant used, or the volume of titrant needed to reach the equivalence point.Boiling point elevation calculatorCompute how much a dissolved solute raises a solvent's boiling point: ΔTb = i·Kb·m, with i the van't Hoff factor, Kb the ebullioscopic constant and m the molality. It returns the elevation and the new boiling point — why salted pasta water boils a touch hotter.Freezing point depression calculatorCompute how much a dissolved solute lowers a solvent's freezing point: ΔTf = i·Kf·m, where i is the van't Hoff factor, Kf the cryoscopic constant and m the molality. It returns the depression and the new freezing point — the physics behind salting icy roads and antifreeze.Osmotic pressure calculatorCompute osmotic pressure with the van't Hoff equation Π = i·M·R·T — the pressure that drives water across a semipermeable membrane. Enter molarity, temperature and the van't Hoff factor to get the pressure in atmospheres, kilopascals, bar and mmHg. Key to IV fluids, cells and reverse osmosis.Moles calculatorCompute the number of moles of a substance from its mass and molar mass.Boiling point calculator (altitude & pressure)Find the boiling point of water at any altitude or atmospheric pressure. Water boils below 100 °C as you climb because the air pushes down less — this tool converts altitude to pressure with the barometric formula, then to a boiling point via the Clausius-Clapeyron relation. Vital for high-altitude cooking and canning.

The Molality calculator turns Moles of solute (or use mass below), Solute mass (optional), Molar mass (g/mol), Mass of solvent, Solvent unit into Molality, Moles of solute used, instantly and for free. For instance, with Moles of solute (or use mass below) = 0.5, Solute mass (optional) = 0 g, Molar mass (g/mol) = 0, Mass of solvent = 250 and Solvent unit = grams it returns Molality = 2 mol/kg and Moles of solute used = 0.5.

How to use it

  1. Enter your values: Moles of solute (or use mass below), Solute mass (optional), Molar mass (g/mol), Mass of solvent, Solvent unit.
  2. Read the result instantly: Molality, Moles of solute used.

Frequently asked questions

How does the Molality calculator work?

It takes Moles of solute (or use mass below), Solute mass (optional), Molar mass (g/mol), Mass of solvent and Solvent unit and derives Molality and Moles of solute used from them. The calculation is live as you type, so the result updates on every change.

Which values does the calculator ask for?

5 values: Moles of solute (or use mass below), Solute mass (optional) (g), Molar mass (g/mol), Mass of solvent and Solvent unit. Nothing else is required — no account, no file upload.

What does a typical calculation look like?

With Moles of solute (or use mass below) = 0.5, Solute mass (optional) = 0 g, Molar mass (g/mol) = 0, Mass of solvent = 250 and Solvent unit = grams, the calculator returns Molality = 2 mol/kg and Moles of solute used = 0.5. Those figures come from running this exact tool, so you can reproduce them by entering the same values.

How much does the result change with different inputs?

It moves a lot. Using Moles of solute (or use mass below) = 1, Solute mass (optional) = 5 g, Molar mass (g/mol) = 5, Mass of solvent = 500 and Solvent unit = kilograms instead, Molality goes from 2 mol/kg to 0.002 mol/kg — which is why it is worth testing a few scenarios rather than trusting a single figure.

Which “Solvent unit” option should I choose?

You can pick between « grams », « kilograms » and « milligrams ». Each one changes what the calculator works out, so switch and compare — the default is « grams ».

Which units should I enter the values in?

Enter Solute mass (optional) g. Metric and US units are both supported — switch system and the figures convert for you.

What does it give for smaller values?

Scaled down to Moles of solute (or use mass below) = 0.25, Solute mass (optional) = 1 g, Molar mass (g/mol) = 1, Mass of solvent = 125 and Solvent unit = grams, Moles of solute used comes out at 0.25. The relationship is worth checking at both ends before you rely on a single result.

When would I actually use this?

Preparing a solution at a stated concentration, working out how much of a reagent a reaction needs, and converting between mass, moles and volume.

What is the most common mistake?

Confusing molarity with molality. One is per litre of solution and the other per kilogram of solvent; they diverge as concentration rises, and only one of them is temperature-independent.

What is the difference between the Molality calculator and the Beer-Lambert law calculator?

This one returns Molality and Moles of solute used; the Beer-Lambert law calculator returns Result and Unit of result. That is the whole difference — open the one whose figure you need.

Further reading

All guides
How-toHow to Calculate a Dilution with C1V1 = C2V2Solve for the missing term, then convert the answer into a bench instruction. The step almost everyone skips is that the solvent you add is V2 minus V1, not V2.ExplainerThe Ideal Gas Law Explained: PV = nRT, R in Every Unit, and Where It BreaksPV = nRT holds when the gas is dilute and far from condensing. The value of R depends entirely on the units you feed it, and the temperature is never in degrees Celsius.How-toHow to Calculate pH — And When the Weak-Acid Shortcut Stops WorkingFour routes for four kinds of solution, each worked with real numbers. Including the part most pages leave out: the square-root formula for a weak acid is an approximation with a validity limit, and it fails quietly.How-toHow to Calculate Molar Mass, Including Parentheses and HydratesMultiply each atomic weight by its subscript and add. The only three places the arithmetic goes wrong are a subscript after a closing bracket, the hydrate dot, and a capital letter typed as a lowercase one.ExplainerHow Half-Life Works: What Is Left After 1, 3 and 10 Half-LivesOne half-life leaves 50%, three leave 12.5%, ten leave less than a tenth of a percent. The formula is a single line — the part worth understanding is why the answer never reaches zero.How-toHow to Solve Stoichiometry Problems: Grams to Moles to Ratio to GramsEvery problem in the chapter is the same four moves. The mole ratio is the hinge, and it is the step students lose — worked here end to end, limiting reactant and percent yield included.