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Chemistry notes, chapter 2

Matter and the Atomic Structure

Textbook Chemistry Form 4 KSSM (DLP), pages 22–41

What this chapter covers

  • Describe matter and explain changes in the state of matter using particle arrangement, kinetic energy and attraction force (2.1)
  • Determine the melting point and freezing point of naphthalene from heating and cooling curves (2.1)
  • Compare the relative mass and relative charge of protons, neutrons and electrons, and sequence the atomic models (2.2)
  • Define proton number and nucleon number, write the standard representation and the electron arrangement of an atom (2.3)
  • Define isotopes, calculate relative atomic mass from natural abundance and justify the uses of isotopes (2.4)

2.1Basic concepts of matter

Matter is anything that has mass and occupies space. It is made up of tiny, discrete particles and exists as a solid, a liquid or a gas.

A rainbow has no mass and takes up no space, so it is not matter. Matter is made of atoms, molecules or ions: an element has atoms or molecules (carbon, C; oxygen, O2), a compound has molecules or ions (water, H2O; sodium chloride, NaCl).

Changes in the state of matter

PropertySolidLiquidGas
Arrangement of particlesClosely packed, orderlyClosely packed, not orderlyFar apart
Kinetic energyLowHigher than solidVery high
Attraction forceStrongStrong, but less than solidWeak
ChangeNameHeat energy
Solid to liquidMeltingAbsorbed
Liquid to gasBoiling / evaporationAbsorbed
Solid to gasSublimationAbsorbed
Gas to liquidCondensationReleased
Liquid to solidFreezingReleased
Gas to solidDepositionReleased

Textbook Figure 2.2, p. 25

Melting point is the constant temperature at which a solid changes to a liquid at a given pressure. Freezing point is the constant temperature at which a liquid changes to a solid.

Heating curve of naphthalene (Activity 2.2, pp. 26-28)

Heating curve of naphthalene: temperature rises from A to B, stays at 80 degrees from B to C, then rises from C to D
Heating curve. B to C is flat at the melting point (80 °C).
  • A to B: solid; particles absorb heat and vibrate faster, so temperature rises.
  • B to C: melting; temperature is constant because the heat absorbed is used to overcome the attraction forces between particles, not to raise temperature.
  • C to D: liquid; particles absorb heat and move faster.

On cooling, the curve is flat at the freezing point because heat lost to the surroundings is balanced by the heat released when particles attract each other to form a solid. Naphthalene is heated in a water bath (not directly) because it is flammable and the water bath heats it slowly and evenly; it is stirred continuously during cooling so that it cools evenly; if it is not stirred, some of it may solidify before the rest and the thermometer reading will not be accurate. The boiling tube is placed in a conical flask so that it loses heat slowly.

In every "constant temperature" question, say where the heat goes: it overcomes (melting) or is balanced by (freezing) the attraction forces between particles.
Why does the temperature stay constant while ice melts?
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The heat absorbed is used to overcome the attraction forces between the particles, not to increase their kinetic energy.

2.2The development of the atomic model

Subatomic particleSymbolRelative chargeRelative mass
Protonp+11
Neutronn01
Electrone−11/1840
ScientistContribution
John DaltonMatter is made of atoms: the smallest spherical body that cannot be created, destroyed or divided
J.J. ThomsonDiscovered electrons; the atom is a positively charged sphere with electrons in it
Ernest RutherfordNucleus is the centre of the atom and holds almost all the mass; discovered protons
Niels BohrElectrons move in shells around the nucleus
James ChadwickDiscovered neutrons in the nucleus

Textbook Figure 2.9, pp. 30-31. Memory order: Dalton, Thomson, Rutherford, Bohr, Chadwick.

Mixing up the discoverers. Thomson found the electron, Rutherford the nucleus and proton, Chadwick the neutron. Bohr put electrons in shells.

2.3Atomic structure

Proton number = number of protons in the nucleus.
Nucleon number = number of protons + number of neutrons.

A neutral atom has equal numbers of protons and electrons. So neutrons = nucleon number − proton number. An atom is written as AZX with A the nucleon number and Z the proton number; for example 126C has 6 protons, 6 electrons and 6 neutrons.

Example (textbook p. 33)
A potassium atom has nucleon number 39 and 19 protons.
Electrons = protons = 19. Neutrons = 39 − 19 = 20.

Ions

A chlorine atom (17 p, 18 n, 17 e) gains 1 electron to form Cl− (17 p, 18 n, 18 e). Protons and neutrons never change when an ion forms. Gaining electrons gives an anion; losing electrons gives a cation.

Electron arrangement

Electrons fill the shell nearest the nucleus first. For proton numbers 1 to 20 the maximum is 2, 8, 8. Aluminium (13 electrons) is 2.8.3. Electrons in the outermost (valence) shell are valence electrons; they decide the chemical properties of an element, so elements with the same number of valence electrons behave alike.

ElementProton numberElectron arrangementValence electrons
Oxygen82.66
Sodium112.8.11
Chlorine172.8.77
Calcium202.8.8.22
An atomic structure diagram shows protons and neutrons in the nucleus and the electron shells (for aluminium: 13 p, 14 n in the nucleus, then 2, 8, 3). An electron arrangement diagram shows the nucleus as a single circle (with the element symbol) and the electrons in their shells, without the numbers of protons and neutrons.
Atom Y has 11 protons and 12 neutrons. Write its standard representation and electron arrangement.
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Nucleon number = 11 + 12 = 23, so 2311Y. Electron arrangement 2.8.1.

2.4Isotopes and their uses

Isotopes are atoms of the same element with the same number of protons but a different number of neutrons (different nucleon numbers). Example: chlorine-35 and chlorine-37.

Isotopes have the same chemical properties (same electron arrangement) but different masses. Hydrogen has three isotopes, 11H, 21H and 31H. Chlorine-35 can also be written Cl-35 or 35Cl. Natural abundance is the percentage of each isotope in a natural sample of the element.

Relative atomic mass = Σ(% abundance × mass of isotope) ÷ 100
Example (textbook p. 38)
Chlorine: 75% 35Cl and 25% 37Cl.
RAM = (75 × 35 + 25 × 37) ÷ 100 = 35.5

Uses of isotopes

FieldIsotopeUse
MedicineCobalt-60Radiotherapy to kill cancer cells; sterilising surgical tools
MedicineIodine-131Treating thyroid disorders such as hyperthyroidism and thyroid cancer
AgriculturePhosphorus-32Studying plant metabolism
Nuclear energyUranium-235Generating electricity
ArchaeologyCarbon-14Estimating the age of fossils and artefacts
ArchaeologyLead-210Determining the age of sand and earth layers up to 80 years
IndustryHydrogen-3Tracing sewage and liquid waste
EngineeringSodium-24Detecting leaks in underground pipes

Isotopes bring benefits (treating disease, dating fossils, detecting leaks), but radioactive waste and radiation can harm living things and the environment, so they must be handled and disposed of with care.

Writing "different number of protons" for isotopes. Isotopes of one element always have the same proton number; only the neutrons differ.
Neon has 90% 20Ne and 10% 22Ne. Calculate its relative atomic mass.
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(90 × 20 + 10 × 22) ÷ 100 = 2020 ÷ 100 = 20.2