Concentration of solutions

Every solution answers one question in several different accents: how much solute is packed into how much solvent, or how much solute is packed into how much solution? Chemists switch between mass, volume, and mole-based scales depending on what is easiest to measure on the bench — a balance for mass percentage, a volumetric flask for molarity, a thermometer-friendly mass of solvent for molality. This article builds the full toolkit ISC Class 12 expects at the start of the Solutions unit: mass and volume percentage, mole fraction, molarity, molality, normality, and ppm, plus the one relation — linking molarity to mass percentage through density — that turns a bench measurement into a laboratory concentration, and the reasoning for why molality, not molarity, survives a change in temperature.

The core insight

A solution's concentration can be expressed on several equivalent scales — mass %, volume %, mole fraction, molarity, molality, normality, ppm — and converting between them, especially molarity and molality via the solution's density, is the core numerical skill of this topic.

The core idea

A solution has a solute (the component present in smaller amount) dissolved in a solvent (the component present in larger amount). Every concentration scale is a ratio of "how much solute" to "how much solution or solvent," and the scales differ only in what units go into the numerator and denominator.

Mass- and volume-based scales. Mass percentage and volume percentage compare solute to the whole solution:

% ww=mass of solutemass of solution×100,% vv=volume of solutevolume of solution×100\%\,\frac{w}{w} = \frac{\text{mass of solute}}{\text{mass of solution}} \times 100, \qquad \%\,\frac{v}{v} = \frac{\text{volume of solute}}{\text{volume of solution}} \times 100

where: both are dimensionless percentages, useful whenever no density is known and masses (or volumes) are measured directly on a balance or in a measuring cylinder. Parts per million follows the same pattern for trace amounts: ppm=mass of solutemass of solution×106\text{ppm} = \dfrac{\text{mass of solute}}{\text{mass of solution}} \times 10^6.

Mole-based scale. For a solvent-solute pair with n1n_1 mol solvent and n2n_2 mol solute, the mole fraction is

x1=n1n1+n2,x2=n2n1+n2,x1+x2=1x_1 = \frac{n_1}{n_1+n_2}, \qquad x_2 = \frac{n_2}{n_1+n_2}, \qquad x_1+x_2 = 1

where: x1,x2x_1, x_2 are dimensionless fractions that must always sum to 1 for a two-component solution. Mole fraction is the natural scale for vapour-pressure work (Raoult's and Henry's laws), since vapour pressure depends on the fraction of molecules of each kind at the surface, not on their mass or volume.

Volume-of-solution scale. Molarity (MM) is moles of solute per litre of solution:

M=nsoluteVsolution (L)M = \frac{n_{\text{solute}}}{V_{\text{solution}}\,(\text{L})}

where: nsoluten_{\text{solute}} is in mol and VsolutionV_{\text{solution}} is the total solution volume in litres, read off a volumetric flask. Because volume expands slightly on heating, molarity is temperature-dependent — the same 1 mol of solute in a slightly larger volume on a hot day reads a slightly lower molarity.

Mass-of-solvent scale. Molality (mm) is moles of solute per kilogram of solvent:

m=nsolutewsolvent (kg)m = \frac{n_{\text{solute}}}{w_{\text{solvent}}\,(\text{kg})}

where: wsolventw_{\text{solvent}} is the mass of solvent alone (not the solution) in kilograms. Mass does not change with temperature, so molality is temperature-independent — this is exactly why molality, not molarity, is used later in this chapter for freezing-point depression and boiling-point elevation. Finally, normality (NN) counts gram-equivalents of solute per litre of solution, N=M×n-factorN = M \times n\text{-factor}, where the nn-factor is the number of replaceable H+H^+ for an acid, replaceable OH−OH^- for a base, or total charge transferred for a salt (1 for HCl, 2 for H2SO4H_2SO_4). An error in the nn-factor is the single most common source of wrong answers in normality problems, since it scales the whole result.

Figure
Two beakers compared, molarity measured against the volume of the whole solution and molality measured against the mass of solvent only
Molarity vs molality — same solute, two different denominators Molarity M volume of solution M = mol solute / L solution Molality m mass of solvent only m = mol solute / kg solvent Heating expands the solution volume but not its solvent mass, so only molarity drifts with temperature.

Deriving the density bridging formula

Explain, from first principles and unit tracking alone, how the molarity of a solution can be computed directly from its mass percentage and density without ever measuring a volume of solute — a bridge used constantly when a bottle label gives density and mass percentage but a titration calculation needs molarity.

Step 1. Fix a convenient basis. Since molarity is defined per litre of solution, take exactly V=1000 mL=1 LV = 1000\ \text{mL} = 1\ \text{L} of the solution as the working sample; any consistent basis works, but 1 L makes the final division by volume trivial.

Step 2. Convert that volume to mass using the given density dd (in g mL−1^{-1}). Mass of the 1 L sample is masssolution=1000×d\text{mass}_{\text{solution}} = 1000 \times d grams — density is exactly the conversion factor between the volume basis molarity wants and the mass basis percentage gives.

Step 3. Extract the solute's mass using the mass percentage % ww\%\,\frac{w}{w}. By definition % ww=mass of solutemass of solution×100\%\,\frac{w}{w} = \dfrac{\text{mass of solute}}{\text{mass of solution}} \times 100, so rearranging, masssolute=% ww100×(1000 d)=1000 d % ww100\text{mass}_{\text{solute}} = \dfrac{\%\,\frac{w}{w}}{100} \times (1000\,d) = \dfrac{1000\,d\,\%\,\frac{w}{w}}{100}.

Step 4. Convert that mass to moles using the solute's molar mass M2M_2, then divide by the 1 L basis to read off molarity directly:

M=masssolute/M21 L=1000 d % ww100 M2=10 d % wwM2M = \frac{\text{mass}_{\text{solute}}/M_2}{1\ \text{L}} = \frac{1000\, d\, \%\,\tfrac{w}{w}}{100\, M_2} = \frac{10\, d\, \%\,\tfrac{w}{w}}{M_2}

where: dd is in g mL−1^{-1}, % ww\%\,\frac{w}{w} is the mass percentage of solute, and M2M_2 is the solute's molar mass in g mol−1^{-1}; MM comes out in mol L−1^{-1}. (Some texts fold the factor of 100 differently and write M=1000 d %(w/w)M2M = \tfrac{1000\,d\,\%(w/w)}{M_2} with %(w/w)\%(w/w) already meaning the fraction ×100\times 100 divided again by 100 inside — the version above, 10 d %(w/w)/M210\,d\,\%(w/w)/M_2, is the same formula with the arithmetic pre-simplified.) The reasoning chain is simply volume-to-mass (via density), mass-to-solute-mass (via percentage), solute-mass-to-moles (via molar mass) — three unit conversions stacked into one formula.

Worked example

Reconsider the aqueous H2SO4H_2SO_4 sample from before: density 1.198 g mL−11.198\ \text{g mL}^{-1}, 27%27\% H2SO4H_2SO_4 by mass, M2=98 g mol−1M_2 = 98\ \text{g mol}^{-1}. Use the bridging formula to find its molarity directly, then find the normality, and finally find the volume to which 250 mL of this stock must be diluted to make it exactly 1.5 N1.5\ N.

Step 1. Apply the derived formula: M=10×1.198×2798=323.4698=3.30 mol L−1M = \dfrac{10 \times 1.198 \times 27}{98} = \dfrac{323.46}{98} = 3.30\ \text{mol L}^{-1}. This matches the value obtained earlier by working through 1 L from scratch — the shortcut formula is exactly that same working, compressed into one line.

Step 2. Convert to normality using the nn-factor of H2SO4H_2SO_4, which is 2 (two replaceable H+H^+ per molecule): N=M×n=3.30×2=6.60 eq L−1N = M \times n = 3.30 \times 2 = 6.60\ \text{eq L}^{-1}.

Step 3. Apply the dilution law. Diluting with solvent changes the volume but not the total gram-equivalents of solute, so N1V1=N2V2N_1V_1 = N_2V_2. Taking V1=250 mLV_1 = 250\ \text{mL} of the 6.60 N6.60\ N stock and the target N2=1.5 NN_2 = 1.5\ N: V2=N1V1N2=6.60×2501.5=1100 mLV_2 = \dfrac{N_1V_1}{N_2} = \dfrac{6.60 \times 250}{1.5} = 1100\ \text{mL}.

Step 4. Interpret: 250 mL of the concentrated stock, made up to a total volume of 1100 mL with water (adding 1100−250=850 mL1100 - 250 = 850\ \text{mL} of water), gives the required 1.5 N1.5\ N solution. Molarity =3.30 mol L−1= 3.30\ \text{mol L}^{-1}, normality =6.60 eq L−1= 6.60\ \text{eq L}^{-1}, final volume =1100 mL= 1100\ \text{mL}.

Common traps

  • Confusing molarity's denominator (volume of the whole solution) with molality's denominator (mass of the solvent alone) — swapping them is the single most frequent numerical slip.
  • Forgetting that a computed x1+x2≠1x_1 + x_2 \ne 1 signals an arithmetic error in a mole-fraction problem.
  • Plugging percentage as a plain fraction (0.27) instead of the percentage number (27) into the density bridging formula, which throws the answer off by a factor of 100.
  • Using the wrong nn-factor when converting molarity to normality — always check the number of replaceable ions per formula unit before multiplying.

Ask the tutor: stuck on converting between molarity, molality, and normality using density, or want another dilution problem worked through step by step? Ask the AI tutor.

Why do we need so many different concentration scales instead of just one

Each scale is convenient for a different job. Mass percentage and ppm need only a balance, so they suit trace or industrial samples where no density is known. Mole fraction is the natural variable in vapour-pressure laws because vapour pressure tracks the fraction of molecules at the surface, not their mass. Molarity matches volumetric glassware used every day in titrations. Molality is chosen specifically because it does not drift with temperature, which matters for freezing-point and boiling-point calculations later in this unit. Knowing which scale a formula expects, and being able to convert into it, is the actual skill being tested.

Why is molarity temperature-dependent but molality is not

Molarity's denominator is the volume of the solution, and volumes expand when a liquid is heated because the molecules spread further apart, even though no matter is added or removed. So the same fixed amount of solute divided by a slightly larger volume gives a slightly smaller molarity on a hot day. Molality's denominator is the mass of solvent, and mass does not change with temperature (no atoms are created or destroyed by heating). This is exactly why colligative-property equations, which must hold across a range of experimental temperatures, are written in terms of molality rather than molarity.

How do I know when to use the density bridging formula instead of working through 1 L directly

They give the identical answer — the formula is just the 1 L working pre-solved algebraically. Use the formula when you need speed and are confident with the units (d in g per mL, percentage as the plain number like 27 not 0.27, and molar mass in g per mol). If you are unsure of the formula or worried about a units slip, fall back to the explicit 1 L method: find the mass of 1 L of solution from density, find the solute's mass from the percentage, divide by molar mass for moles, and that is the molarity. Both routes are worth showing on an exam, since the explicit method demonstrates understanding even if you mis-remember the compressed formula.

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