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A-level Chemistry/WJEC/Module 1/Calculations

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Balanced Equations and Associated Calculations

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Central to chemical calculations is the balanced chemical equation. Here is an example:

2 C2H6 + 7 O2 → 4 CO2 + 6 H2O

Two molecules of ethane (C2H6) react with 7 molecules of oxygen (O2) to form 4 molecules of carbon dioxide (CO2) and 6 molecules of water (H2O).

A balanced chemical equation is required to convert information about one chemical into information about a second chemical.

Examples:

How many molecules of oxygen would react with 200 molecules of ethane?

A very useful idea is the extent (ξ) of the reaction. This is the amount of a chemical divided by the number of molecules for that chemical which react.
For ethane, 200 molecules is an extent of 200 / 2 = 100 molecules.
For oxygen, if ξ = 100 molecules then it means that 100 x 7 = 700 molecules of oxygen can react.

How many molecules of carbon dioxide form if 300 molecules of ethane react with 350 molecules of oxygen?

For ethane, 300 molecules is an extent of 300 / 2 = 150 molecules.
For oxygen, 350 molecules is an extent of 350 / 7 = 50 molecules.
ξ for oxygen is lower, which means that during the reaction, oxygen will run out first and the reaction will stop. We call oxygen the limiting reagent and ethane is said to be in excess.
For carbon dioxide, if the reaction is limited to ξ = 50 molecules then it means that 50 x 4 = 200 molecules of carbon dioxide will form.
For ethane, if the reaction is limited to ξ = 50 molecules then it means that 50 x 2 = 100 molecules of ethane can react. The reaction began with 300 molecules of ethane, so 200 molecules of ethane will be left unreacted.

How many molecules of water form if 500 molecules of ethane react with 2100 molecules of oxygen?

For ethane, 500 molecules is an extent of 500 / 2 = 250 molecules.
For oxygen, 2100 molecules is an extent of 2100 / 7 = 300 molecules.
This time, ξ for ethane is lower, which means that during the reaction, ethane will run out first and the reaction will stop. In this scenario, ethane is the limiting reagent and oxygen is said to be in excess.
For water, if the reaction is limited to ξ = 250 molecules then it means that 250 x 6 = 1500 molecules of water will form.
For oxygen, if the reaction is limited to ξ = 250 molecules then it means that 250 x 7 = 1750 molecules of oxygen can react. The reaction began with 2100 molecules of oxygen, so 350 molecules of oxygen will be left unreacted.

For practical chemistry, we need to work with much larger numbers of molecules. Chemists originally defined a "much larger number" to be the number of atoms in 1 g of hydrogen, the lightest element. This number is called a mole and is now defined as 6.02 x 1023.

The Mole

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One "mole" is a number of particles. The number chosen for 1 mole is a very large, so that the mass of 1 mole of atoms, or molecules, is a convenient mass for laboratory use. e.g. 1 mole of 12C atoms have a mass of 12.0 g. Until 2019, the value of the mole was defined using 12C atoms as the standard.

The number of particles in 1 mole is the Avogadro Constant, which is given the symbol NA (or sometimes L). NA = 6.02 x 1023 mol-1 - this figure is in your Data Booklet. Since 2019 the value of NA has simply been defined as 6.022 140 76 x 1023 mol-1. The first 3 significant figures are adequate for A-level calculations.

So, a mole of particles is NA particles which is 6.02 x 1023 particles.

If a mole of 12C atoms have a mass of 12.0 g then a single 12C atom has a mass of 12.0 g ÷ 6.02 x 1023 = 1.99 x 10-23 g.

What is left if 0.500 moles of ethane react with 2.800 moles of oxygen?

2 C2H6 + 7 O2 → 4 CO2 + 6 H2O

For ethane, 0.500 moles is an extent of 0.500 / 2 = 0.250 moles.
For oxygen, 2.800 moles is an extent of 2.800 / 7 = 0.400 moles.
ξ for ethane is lower, which means that during the reaction, ethane will run out first and the reaction will stop. In this scenario, ethane is the limiting reagent and oxygen is said to be in excess.
For carbon dioxide, if the reaction is limited to ξ = 0.250 moles then it means that 0.250 x 4 = 1.000 moles of carbon dioxide will form.
For water, if the reaction is limited to ξ = 0.250 moles then it means that 0.250 x 6 = 1.500 moles of water will form.
For oxygen, if the reaction is limited to ξ = 0.250 moles then it means that 0.250 x 7 = 1.750 moles of oxygen can react. The reaction began with 2.800 moles of oxygen, so 1.050 moles of oxygen will be left unreacted.

How do we figure out the number of moles of a chemical? There are three main methods:

  1. comparing the mass of a chemical sample to the mass of 1 mole of that chemical
  2. comparing the volume of a pure gas to the volume of 1 mole of gas, and
  3. measuring volumes of solutions where the number of moles dissolved in a standard volume is known.

Relative Masses and Molar Masses

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1 mole of the isotope 35Cl is 35.0 g. We say that the relative isotopic mass (Ir) of 35Cl is 35.0.

Chlorine naturally occurs as a mixture of two isotopes, 35Cl and 37Cl. 76 % of chlorine atoms are 35Cl. The average mass of chlorine atom is 76 % of 35 + 24 % of 37 = 26.60 + 8.88 = 35.48. This is chlorine's relative atomic mass (Ar), which we round up to 35.5.

No single chlorine atom has a mass of 35.5, the atoms have an Ir of either 35.0 or 37.0. This is similar to the average UK family having 1.5 children - some families have 1 child, some have 2 or more. On average, there are 1.5 children per family but obviously there is no such thing as 0.5 of a child.

Chlorine atoms do not usually exist on their own. Chlorine atoms usually form diatomic molecules, Cl2 which have a relative molecular mass (Mr) of 71.0. In the same way, chloroform (CHCl3) has an Mr of 119.5 (12.0 + 1.01 + 3 x 35.5).

1 mole of sodium chloride, NaCl, has a mass of 58.5 g. We can say that its relative formula mass (Mr) is 58.5. Because NaCl is not made of molecules, we refer to its relative formula mass but the symbol (Mr) is the same as for relative molecular mass.

A useful alternative term is molar mass (M). This has units of g mol-1 ("grams per mole") or kg mol-1 on the Physics specification. Molar mass can refer to isotopes, atoms, molecules or formulae, so you do need to be specific:

  • The molar mass of the chlorine-35 isotope is 35.0 g mol-1
  • The molar mass of chlorine atoms is 35.5 g mol-1
  • The molar mass of chlorine molecules is 71.0 g mol-1

In Biology, masses of molecules are often measured in daltons (Da) or kilodaltons (kDa). For all practical purposes, 1 Da = 1 g mol-1. (It is actually 0.999 999 999 65 g mol-1). Glucose, for example, has a relative molecular mass of 180.156, a molar mass of 180.156 g mol-1 and a mean mass of 180.156 Da (2.99171 x 10-22 g).

Empirical and Molecular Formulae

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Definitions:

  • Empirical formula: The simplest whole number ratio of atom types present in a molecule of a compound.
  • Molecular formula: The actual number of atoms of each element present in a molecule of a compound.

To determine a molecular formula you need the given mass of the substance and the empirical formula mass. Divide the given mass by the empirical formula mass.

Multiply the given answer by the ratios in the empirical formula and you will have the molecular formula.

A typical question might ask about a compound with 39.97 % carbon, 6.73 % hydrogen and 53.30 % oxygen and Mr = 180.12

There are two ways to find the empirical and molecular formulae:

If we assume a 100 g sample, we would have:

  • 39.97 g carbon ÷ 12.0 = 3.331 mol ÷ 3.331 mol = 1
  • 6.73 g hydrogen ÷ 1.01 = 6.663 mol ÷ 3.331 mol = 2
  • 53.30 g oxygen ÷ 16.0 = 3.3310 mol ÷ 3.331 mol = 1

Divide each mass by the Ar for that element, and then divide the amounts by the smallest amount to find the ratio.

Empirical formula: CH2O

If CH2O were the molecular formula, then Mr would be 30.02

Mr is actually 180.12.

180.12 / 30.02 = 6, so the molecular formula is C6H12O6

Alternatively:

If we assume a 180.12 g sample (1 mole), we would have:

  • 39.97 % carbon x 180.12 g = 71.99 g ÷ 12.0 = 6.000 mol
  • 6.73 % hydrogen x 180.12 g = 12.12 g ÷ 1.01 = 12.000 mol
  • 53.30 % oxygen x 180.12 g = 96.00 g ÷ 16.0 = 6.000 mol

Find the mass of each element in 1 mole, then divide each mass by the Ar for that element.

Molecular formula: C6H12O6

The ratios in the molecular formula will simplify to CH2O, the empirical formula.

Anhydrous and Hydrated Salts

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Solid salts consist of a lattice of positive and negative ions, sometimes water molecules are incorporated into the lattice. The water in a lattice is called the water of crystallisation. When a salt contains water the salt is hydrated, if a salt does not contain water of crystallisation the salt is anhydrous.

A mole of a particular hydrated salt usually has the same number of moles of water of crystallisation, its formula shows how many water molecules are present for every molecule of salt e.g. copper sulfate, CuSO4, has 5 moles of water for every mole of salt, therefore its hydrated formula is CuSO4⋅5H2O, (a dot ⋅ separates the salt's formula from the water of crystallisation).

Examples:

  • CuSO4⋅5H2O
  • Na2CO3⋅10H2O
  • MgSO4⋅7H2O

Dehydration

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Many hydrated salts lose their water of crystallisation when heated. For example:

CuSO4⋅5H2O(s) → CuSO4(s) + 5 H2O(g)

Mr of CuSO4 is 159.6 and Mr of H2O is 18.0

An experiment might start with 12.48 g of CuSO4⋅5H2O(s) and find that after heating, only 7.98 g of solid are left.

7.98 g of CuSO4 is 7.98 / 159.6 = 0.0500 mol

The 4.50 g of mass that is "lost" is the H2O(g). 4.50 g of H2O is 4.50 / 18.0 = 0.250 mol

The ratio of CuSO4 to H2O is 0.0500 mol to 0.250 mol which is 1 to 5.

Practically, these experiments are prone to errors if not all the water is evaporated or if extra mass is lost. Extra mass can be lost if the solid "spits" during heating and some solid jumps out, or if the anhydrous salt itself can decompose if it is heated for too long:

2 CuSO4 → 2 CuO(s) + 2 SO2(g) + O2(g)

Concentrations of Solutions

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Water of crystallisation is confusing when working out concentrations of salt solutions. If we want to make 250 cm3 of a 0.100 mol dm-3 solution of sodium carbonate, then how much sodium carbonate do we need?

The easy bit is (or should be) n = c x V = 0.250 dm3 x 0.100 mol dm-3 = 0.0250 mol.

What is the mass of 0.0250 mol of sodium carbonate? If we are using the decahydrate (Na2CO3⋅10H2O) then its Mr is 286.2 and the mass is m = n x Mr = 7.16 g

If we are using the anhydrous salt (Na2CO3) then its Mr is 106.0 and the mass is m = n x Mr = 2.65 g

So 7.16 g of Na2CO3⋅10H2O dissolved in 250 cm3 is an Na2CO3 solution (notice the water is no longer mentioned) with a concentration of 0.100 mol dm-3.


Standard Solutions

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A standard solution of a chemical has a known concentration.

concentration = quantity of solute / volume of solution

Various sizes of volumetric flask. In each case, the liquid level is made up so that the bottom of the meniscus is on the calibration line. The flasks are marked in "ml" (millilitres) which are identical to cm3. 5000 ml = 5000 cm3 = 5 dm3.

Usually, the solute is measured in moles, the volume is measured in dm3 and concentration is measured in mol dm-3 ("moles per decimetre cubed").

c = n / V

It is important to be able to convert between dm3 (litres, L or l) and the common units used in the laboratory, cm3 (centimetres cubed, c.c., millilitres, mL or ml).

1 dm3 = 1000 cm3 1 cm3 = 1/1000 dm3 (0.001 dm3 or 1 x 10-3 dm3

Notice that concentration is based on the volume of the solution. Dissolving 1 mole (58.5 g) of sodium chloride in 1 dm3 of water does not make a 1 mol dm-3 solution. This mixture would have a volume of 1.021 dm3 (1021 cm3) and a density of 1.037 g cm-3. The concentration would actually be 0.979 mol dm-3.

1 mol dm-3 NaCl solution can be made by taking 58.5 g of NaCl and making the total volume of solution up to 1 dm3 by adding water. The volume is typically measured with a volumetric flask. This actually requires 0.980 dm3 (980 cm3) of water and the solution has a density of 1.036 g cm-3. However, we do not need to know the volume of water, or the density, if we use a volumetric flask to measure the total volume of solution.

Most importantly, if we measure 25 cm3 (for example) of this solution, we know that this 25 cm3 sample contains 1.00 mol dm-3 x 0.025 dm3 = 0.025 mol of NaCl.

A burette filled with a coloured solution showing the meniscus at the top of the the liquid. In this case the burette reading is 20.05 cm3. Remember to read the bottom of the meniscus and notice that the burette scale is from top to bottom. Burette readings are expected to be recorded to the nearest 0.05 cm3 (even if the reading is 0.00 cm3, write "0.00" not "0").

The Ideal Gas Equation

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pV=nRT

p is the pressure of the gas in Pa (Nm−2)

V is the volume of the gas in m3

Shortcut: p is often given in kPa and V is often given in dm3.
22.4 dm3 at 101 kPa can be written as 0.0224 m3 at 101 000 Pa, but notice that 22.4 x 101 = 0.0224 x 101 000.
So if p is given in kPa and V is given in dm3 then you need not convert p to Pa and V to m3 - just multiply the values you're given.

n is the amount (number of moles)

R is the gas constant (8.31 J mol−1 K−1)

T is the temperature in kelvin (equivalent to 273 + θ, the temperature in degrees Celsius)

Example: How many moles of gas occupy 250 cm3 at 15 °C and 200 kPa?

Using pV = nRT, n = pV / RT

n = 200 000 Pa x 2.5 x 10-4 m3 / (8.31 J mol-1 K-1 x 288 K)
n = 2.089 x 10-2 mol

(Using the Vm method (see below) the value comes out as 2.095 x 10-2 mol. Using unrounded values for R, p and T, the answer should be 2.087 x 10-2 mol i.e. the pV = nRT method is more precise if p is given in kPa or Pa.)

Molar Gas Volumes, Vm

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The Data Booklet gives two values for Vm, 22.4 dm3 mol−1 at 273 K and 1 atm, and 24.5 dm3 mol−1 at 298 K and 1 atm.

These are the volumes of 1 mole of gas under these conditions.

To find the actual number of moles, divide the volume of gas by the appropriate value of Vm. For example, 49.0 dm3 of gas at 298 K and 1 atm is 49.0 / 24.5 = 2.00 mol.

Vm can be corrected for different temperatures and pressures. It is best to start with the 22.4 dm3 mol−1 figure at 273 K and 1 atm. The 24.5 dm3 mol−1 figure at 298 K and 1 atm is good only for those exact conditions because it has a larger rounding error (-0.01 % for 22.4 dm3 mol−1 vs +0.19 % for 24.5 dm3 mol−1).

At temperature T and pressure p, Vm = 22.4 dm3 mol−1 x T / (273 x p)

T and p must be in kelvin and atmospheres respectively.

For example, at 100 °C and 2 atm, Vm = 22.4 dm3 mol−1 x 373 K / (273 x 2 atm) = 15.3 dm3 mol−1

Use this approach if the pressure is given in atm, or is stated to be 101 kPa (i.e. 1 atm). For pressure given in kPa, or Pa, the pV = nRT approach is more precise.

n = pV / RT (p is in Pa, V in m3, T in K, R = 8.31 J mol−1 K−1)
n = V / Vm = 273 K x pV / (22.4 dm3 mol−1 x T) (p is in atm, V in dm3, T in K)

Example: How many moles of gas occupy 250 cm3 at 45 °C and 1.2 atm?

n = 273 K x pV / (22.4 dm3 mol−1 x T)
T = 45 + 273 = 318 K
V = 0.250 dm3
n = 273 K x 1.2 atm x 0.250 dm3 / (22.4 dm3 mol−1 x 318 K)
n = 0.01150 mol = 1.150 x 10-2 mol

Using pV = nRT, n = pV / RT

n = 121 200 Pa x 2.5 x 10-4 m3 / (8.31 J mol-1 K-1 x 318 K)
n = 1.147 x 10-2 mol

(Using unrounded values for R, p and T, the answer should be 1.149 x 10-2 mol i.e. the Vm method is more precise if p is given in atm.)

Errors

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It is important to know how certain a measurement is; What is the potential error in the measurement?

A 25 cm3 volumetric pipette is marked ± 0.06 cm3. This is the absolute uncertainty, u.

If the uncertainty is not recorded, we can assume that the absolute uncertainty is:

  • one-half of the divisions drawn on a scale
  • one-half of the last decimal place shown on a digital display

For a ruler which has a 1 mm scale, the absolute uncertainty is ± 0.5 mm. For a digital thermometer showing 24.2 ᐤC, the absolute uncertainty is ± 0.05 ᐤC.

Ruler with 1 mm scales, marked every 1 cm
Digital thermometer

Be careful, many measurements are actually the difference between two measurements. If we used the rule to measure 297 mm, we rely on the 0 mm and the 297 mm marks being accurate. If we add the two absolute uncertainties we find that we have measured 297 mm ± 1 mm†. This is true of burettes and balances.

† To be exact, we shouldn't add the uncertainties, but square the uncertainties, add the squares, and then take the square root: √(0.52 + 0.52) = 0.71 mm. There's no time for this at A-level: Just add the uncertainties!

Examples:

  • Initial burette reading: 0.4 cm3. The scale is marked every 0.1 cm3 so this initial reading is 0.4 ± 0.05 cm3.
  • Final burette reading: 24.7 cm3 ± 0.05 cm3.
  • Titre: 24.7 - 0.4 = 24.3 ± 0.1 cm3
  • Initial burette reading: 0.0 ± 0.05 cm3.
  • Final burette reading: 24.3 cm3 ± 0.05 cm3.
  • Titre: 24.3 - 0.0 = 24.3 ± 0.1 cm3

This is why it is often a waste of time to "zero" a burette. Just record the initial and final values.

  • Mass of weighing boat: 1.210 g. The digital scale gives three decimal places so this reading is 1.210 ± 0.0005 g.
  • Mass of weighing boat with sample: 2.210 ± 0.0005 g.
  • Mass of weighing boat after sample transferred to beaker: 1.211 ± 0.0005 g.
  • Mass of sample transferred to beaker: 2.210 - 1.211 = 0.999 ± 0.001 g

Notice how it is important to record the final zero if you have measured it. 0.0 cm3 is more precise than 0 cm3. 1.210 g is more precise than 1.21 g.

What if you use the 0.999 g of sample to make a 250 cm3 solution, and measure 24.3 cm3 from this solution using the burette? How many grams of sample are in the 24.3 cm3?

Well, 0.999 g x 24.3 cm3 ÷ 250 cm3 = 0.0971 g but how certain is this value?

We have three uncertainties to consider:

  • Balance: 0.999 ± 0.001 g
  • Volumetric flask: 250 ± 0.3 cm3
  • Burette: 24.3 ± 0.1 cm3

The uncertainties add up, but how?

We can calculate the relative (percentage) uncertainty, ur from the equation ur = 100 % x absolute error ÷ the value measured.

  • Balance: 100 % x 0.001 g ÷ 0.999 g = 0.100 %
  • Volumetric flask: 100 % x 0.3 cm3 ÷ 250 cm3 = 0.120 %
  • Burette: 100 % x 0.1 cm3 ÷ 24.3 cm3 = 0.411 %

Adding the percentage errors gives us ± 0.631 % (or 0.440 % using the square-root-of-the-sum-of-the-squares method you really don't need to know).

The 24.3 cm3 of solution contains 0.0971 g ± 0.631 %.

Significant figures

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As a rule, give your answers to 3 significant figures unless told otherwise. This implies a percentage error between 0.5 % and 0.05 %.

0.999 g could be between 0.9995 and 0.9985 g so ± 0.0005 g or ± 0.05 %
0.100 g could be between 0.1005 and 0.0995 g so ± 0.0005 g or ± 0.5 %
  • 2 significant figures implies a percentage error between 5 % and 0.5 %.
  • 3 significant figures implies a percentage error between 0.5 % and 0.05 %.
  • 4 significant figures implies a percentage error between 0.05 % and 0.005 %.

If you use several values in a calculation, the value with the lowest number of significant figures dictates the number of significant figures in the answer.

Example: 0.998 g ÷ 2.0 dm3 = 0.50 g dm-3

Exception: When adding or subtracting numbers, the value with the lowest number of decimal places dictates the number of decimal places in the answer.

Example: 2.0 g - 0.998 g = 1.0 g