The atom
Introduction
We have investigated many types of matter and how materials are classified. To understand why different materials behave differently we must examine their basic building blocks - the atom. Atoms form all structures and organisms in the universe: planets, stars, plants, air and living organisms are composed of different combinations of atoms.
Our modern understanding of the atom developed over a long period of time, through the work of many scientists. The following sections reconstruct the historical development, define the parts of an atom, explain atomic masses and sizes, and present electron arrangement and its importance for chemical behaviour.
Scientific models of the atom evolved as new evidence and experiments became available. A model is a simplified representation of a real system that helps us understand its properties. Atomic models are representations based on experimental observations; they are not literal pictures but tools for understanding and prediction.
The idea that matter is made of indivisible particles was proposed by Greek philosophers such as Leucippus and Democritus in the fifth century BC. The Greek word atomon means "indivisible". Early ideas were qualitative; later scientists developed experimental evidence and quantitative models.
John Dalton proposed that all matter is composed of small indivisible particles called atoms. Dalton's model treated atoms as solid, indivisible spheres and helped explain conservation of mass and definite proportions in chemical reactions. At the time electrons and the nucleus were not known.
After the discovery of the electron by J. J. Thomson (1897), the plum-pudding model (1904) pictured the atom as a diffuse positive "soup" with negatively charged electrons embedded in it, analogous to plums in a pudding. This model accounted for the existence of electrons but did not explain how positive charge was distributed or how electrons were arranged.
Ernest Rutherford (1911) proposed that positive charge and most of the mass are concentrated in a tiny central nucleus, with electrons around it. He compared the atom to a miniature solar system: a small dense nucleus with electrons orbiting at relatively large distances. Rutherford's model followed from scattering experiments (see detailed section on the alpha-particle scattering experiment below).
Niels Bohr (1913) refined the planetary view by introducing quantised electron orbits. Electrons can occupy only certain discrete energy levels; transitions between levels explain why atoms emit or absorb light at particular wavelengths. Bohr's model explained atomic emission spectra of hydrogen but had limitations for multi-electron atoms.
Rutherford predicted a neutral particle in the nucleus to account for mass without extra positive charge. James Chadwick discovered the neutron in 1932 and measured its mass. The nucleus is therefore made of protons (positively charged) and neutrons (neutral), collectively called nucleons.
Further development led to quantum mechanics. Scientists such as Erwin Schrödinger, Werner Heisenberg, Max Born and others developed the quantum-mechanical model where electrons occupy orbitals - regions of space with specific energies and probability distributions. This modern view replaces classical orbits with probability clouds and explains atomic structure and chemical behaviour more accurately.
Because atomic masses are extremely small, special units are used and comparisons are more convenient than absolute SI masses.
The atomic mass unit (u) is defined using the carbon standard: one atom of carbon-12 is assigned a mass of exactly 12.00 u. In SI units, 1 u ≈ 1.6605 × 10-27 kg (≈ 1.6605 × 10-24 g). Using atomic mass units simplifies comparison of masses of atoms.
Example atomic masses (approximate, in u):
| Element | Atomic mass (u) |
|---|---|
| Carbon (C) | 12.00 |
| Nitrogen (N) | 14.00 |
| Bromine (Br) | 79.90 |
| Magnesium (Mg) | 24.30 |
| Potassium (K) | 39.10 |
| Calcium (Ca) | 40.08 |
| Oxygen (O) | 16.00 |
Individual atoms have masses around 10-27 to 10-26 kg. For example, a hydrogen atom has mass ≈ 1.67 × 10-27 kg and a carbon atom ≈ 1.99 × 10-26 kg. Atoms are extremely small; the nucleus occupies only a tiny fraction of the atom's volume. A common analogy: if an atom were the size of a football stadium, the nucleus would be roughly the size of a pea at the centre.
Rutherford investigated how alpha (α) particles (positively charged helium nuclei) scatter when directed at thin metal foils (gold foil experiment). He placed a zinc sulphide screen around the foil to detect where alpha particles struck. Predictions from the plum-pudding model would have most α particles deflected only slightly. The experiment showed that most α particles passed through the foil, a small fraction were deflected at large angles and a very few rebounded. Rutherford concluded that:
An atom consists of a central nucleus (protons and neutrons) and electrons around the nucleus. The protons and neutrons are called nucleons.
| Particle | Mass (kg, approximate) | Charge (in elementary units) | Charge (C) |
|---|---|---|---|
| Proton | 1.6726 × 10-27 | +1 | +1.602 × 10-19 |
| Neutron | 1.6749 × 10-27 | 0 | 0 |
| Electron | 9.11 × 10-31 | -1 | -1.602 × 10-19 |
Electrons are treated as elementary (point-like) particles in atomic models; they cannot be subdivided by current experimental evidence.
Atomic number (Z) is the number of protons in the nucleus and determines the chemical identity of the element. The atomic number appears on the periodic table and is an integer (1 to about 118).
Mass number (A) is the total number of nucleons (protons + neutrons) in the nucleus. The number of neutrons is N = A - Z.
Standard notation for nuclides is written with mass number and atomic number as superscript and subscript, respectively, before the chemical symbol:
<sup>A</sup><sub>Z</sub>X where X is the chemical symbol, A is the mass number and Z is the atomic number. For example, the iron nucleus with 26 protons and 30 neutrons is written as <sup>56</sup><sub>26</sub>Fe (A = 56, Z = 26, N = 30).
For a neutral atom the number of electrons equals the number of protons. If electrons are gained or lost, the resulting charged atom is called an ion. For example, Na+ is a sodium ion that has lost one electron; Cl- is a chlorine ion that has gained one electron.
QUESTION
Use standard notation to represent sodium and give the number of protons, neutrons and electrons in the element.
SOLUTION
Sodium has atomic number Z = 11 and atomic mass number A = 23.
Write sodium in standard notation as <sup>23</sup><sub>11</sub>Na.
The number of protons is Z = 11.
The number of electrons in the neutral atom equals the number of protons, so electrons = 11.
The number of neutrons is N = A - Z = 23 - 11 = 12.
Relative atomic mass of an element is the average mass of all naturally occurring isotopes of that element, weighted by their natural abundances. Units are atomic mass units (u). The value shown on the periodic table is the relative atomic mass (often a decimal) and not necessarily an integer.
Isotopes are nuclides of the same element that have the same number of protons (same Z) but different numbers of neutrons (different N), and therefore different mass numbers A. Chemical properties of isotopes are essentially the same because chemistry depends mainly on the number of electrons/protons, but nuclear stability and some physical properties can differ.
Example: Chlorine has two common isotopes: Cl-35 (35 is the mass number: 17 protons + 18 neutrons) and Cl-37 (17 protons + 20 neutrons). If Cl-35 occurs with 75% natural abundance and Cl-37 with 25%, the average relative atomic mass is calculated by weighting:
Example 2: The relative atomic mass of an isotopic element
QUESTION
The element chlorine has two isotopes, chlorine-35 and chlorine-37. The abundance of these isotopes when they occur naturally is 75% chlorine-35 and 25% chlorine-37. Calculate the average relative atomic mass for chlorine.
SOLUTION
Contribution from Cl-35 = 0.75 × 35 u = 26.25 u.
Contribution from Cl-37 = 0.25 × 37 u = 9.25 u.
Average relative atomic mass = 26.25 u + 9.25 u = 35.50 u.
This agrees with the value ≈ 35.5 u shown on periodic tables.
Electrons in an atom have quantised energies. Electrons with lowest energy are closest to the nucleus; higher-energy electrons are found further away. Electrons occupy energy levels (also called shells) labelled 1, 2, 3, ...
The first main energy level (n = 1) can hold up to 2 electrons. The second (n = 2) can hold up to 8 electrons (2 in an s subshell and 6 in p subshells). The third level starts to fill similarly (it contains s, p and d subshells).
An atomic orbital is a region of space around a nucleus where an electron is likely to be found. Subshells and orbitals have maximum capacities: an s orbital holds 2 electrons, a p subshell (three p orbitals) holds 6 electrons, etc.
The Aufbau principle describes the order in which orbitals are filled as electron number increases (building up). Electron configurations are often written in spectroscopic notation, e.g. lithium: 1s2 2s1. Noble-gas shorthand (condensed notation) uses the nearest preceding noble gas in square brackets followed by the outer electrons, e.g. magnesium: [Ne] 3s2.
Example 3: Aufbau diagrams and spectroscopic electron configuration
QUESTION
Give the electron configuration for nitrogen (N) and draw an Aufbau diagram.
SOLUTION
Nitrogen has seven electrons in a neutral atom.
Place two electrons in 1s: 1s2. Five electrons remain.
Place two electrons in 2s: 2s2. Three electrons remain.
Place three electrons in 2p as single electrons (Hund's rule): 2p3.
Final electron configuration: 1s2 2s2 2p3.
Example 4: Aufbau diagram for an ion
QUESTION
Give the electron configuration for O2- and draw an Aufbau diagram.
SOLUTION
Neutral oxygen has 8 electrons. The O2- ion has gained two electrons, so total electrons = 10.
Fill 1s: 1s2 (2 electrons). Eight electrons remain.
Fill 2s: 2s2 (2 electrons). Six electrons remain.
Fill 2p: 2p6 (6 electrons).
Final electron configuration for O2-: 1s2 2s2 2p6.
Valence electrons are the electrons in the outermost energy level and determine most chemical behaviour. Core electrons are all the electrons that are not valence electrons.
Electron configuration explains periodic trends, bonding and reactivity. Atoms are most stable when their outer energy level is full; noble gases have full outer levels and are chemically inert. Other atoms tend to gain, lose or share electrons to achieve a more stable (often noble-gas-like) configuration. The octet rule (mainly for main-group elements) summarises this tendency: atoms often aim for eight electrons in their valence shell.
Aim: To observe flame colours produced by different metal cations and relate these to electronic transitions.
Apparatus:
Safety: Tie back long hair, secure loose clothing, work in a ventilated space, and keep flammable materials away from the flame.
Method:
Conclusion: Different metal cations produce characteristic flame colours because electrons in the metal ions absorb energy, move to higher energy levels, then fall back emitting light at characteristic wavelengths (line emission).
Match exercise
Match the information in column A with the key discoverer in column B.
Column A
Column B
Further exercises (cleaned and structured):
Explain the meaning of each of the following terms:
Complete the following table (use atomic data from the periodic table):
| Element | Atomic mass units (A) | Atomic number (Z) | Number of protons | Number of electrons | Number of neutrons |
|---|---|---|---|---|---|
| Mg | 24 | 12 | |||
| O | 8 | ||||
| Cl | 17 | ||||
| Ni | 28 | 40 | |||
| Zn | 30 | ||||
| C | 12 | 6 | |||
| Al3+ | 13 | ||||
| O2- | 18 |
Use standard notation to represent the following elements:
For the element 3517Cl, give the number of:
Which of the following atoms has 7 electrons?
Complete isotope and nuclide tables and solve percentage-abundance relative mass problems (examples were given earlier).
Further exercises on isotopes and electron configurations (selected):
In small groups, build a physical model of an atom using craft materials. Before building, discuss:
After building, evaluate accuracy and limitations of the model and suggest improvements. Use models to discuss why they are simplified and what they do and do not show about real atoms.
Write down only the word/term for each of the following descriptions.
For each of the following, say whether the statement is true or false. If it is false, re-write the statement correctly.
The three basic components of an atom are:
The charge of an atom is:
Use the explanations, examples and rules in this chapter to answer the exercises. Where numerical values are needed, use the appropriate data from the periodic table or the sections above.