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In the modern Periodic Table, elements are arranged in order of increasing atomic (proton) number. Each horizontal row is called a period and each vertical column is called a group.
The key physical idea: because the elements are arranged in order of atomic number, elements within a group have the same pattern of outer-shell electrons. It is the outer-shell electron configuration that controls the chemistry, which is why group members behave similarly.
Periodicity is the repeating trend in physical and chemical properties across periods of the Periodic Table. When we move across Period 3 (Na → Ar) and then into Period 4 (K → Ca and beyond), we see the pattern of properties repeating. Examples of periodic properties include:
We will meet each of these in later lessons.
The Periodic Table can be split into blocks according to which sub-shell the highest-energy electron occupies:
graph LR
A[Periodic Table] --> B[s-block: Groups 1 and 2]
A --> C[p-block: Groups 13-18 Groups 3-0]
A --> D[d-block: transition metals]
A --> E[f-block: lanthanides and actinides]
B --> B1[highest e- in s sub-shell]
C --> C1[highest e- in p sub-shell]
D --> D1[highest e- in d sub-shell]
E --> E1[highest e- in f sub-shell]
| Block | Groups | Outer configuration | Examples |
|---|---|---|---|
| s | 1, 2 (and He) | ns1 or ns2 | Na [Ne] 3s1, Mg [Ne] 3s2 |
| p | 13 - 18 | ns2 npx | Cl [Ne] 3s2 3p5, Ar [Ne] 3s2 3p6 |
| d | Transition metals | (n-1)dx ns2 | Fe [Ar] 3d6 4s2, Cu [Ar] 3d10 4s1 |
| f | Lanthanides + actinides | (n-2)fx | U [Rn] 5f3 6d1 7s2 |
Helium is a special case: its electron configuration is 1s2 (s-block), but chemically it is grouped with the noble gases (Group 0/18) because of its full outer shell. OCR expects you to know this anomaly.
Consider Group 2:
| Element | Electron configuration | Outer electrons |
|---|---|---|
| Be | [He] 2s2 | 2 (in s) |
| Mg | [Ne] 3s2 | 2 (in s) |
| Ca | [Ar] 4s2 | 2 (in s) |
| Sr | [Kr] 5s2 | 2 (in s) |
| Ba | [Xe] 6s2 | 2 (in s) |
All Group 2 elements have two electrons in their outer s sub-shell. They therefore all tend to lose these two electrons to form 2+ ions, and they show similar chemistry (reaction with water, formation of oxides and hydroxides). The same principle applies across every group.
Dmitri Mendeleev (1869) arranged the then-known 63 elements by atomic mass, but crucially left gaps where he believed undiscovered elements should go and predicted their properties. His prediction of "eka-silicon" (later discovered as germanium, 1886) was accurate to within a few percent for atomic mass, density and oxide formula. This success entrenched the Periodic Table as a predictive tool.
The modern table differs from Mendeleev's in two major respects:
Q: Classify each of the following elements by block and state the outer electron configuration: (a) Sulfur (Z = 16) (b) Vanadium (Z = 23) (c) Strontium (Z = 38)
Answer:
(a) S: 1s2 2s2 2p6 3s2 3p4 → outer sub-shell is 3p → p-block; outer config 3s2 3p4 (b) V: [Ar] 3d3 4s2 → highest occupied sub-shell is 3d → d-block (transition metal); outer config 3d3 4s2 (c) Sr: [Kr] 5s2 → outer sub-shell is 5s → s-block (Group 2); outer config 5s2
The modern Periodic Table arranges elements in order of increasing atomic number into periods (rows) and groups (columns). Elements in the same group share outer-shell electron arrangements and therefore show similar chemistry. Elements can be further classified into s-, p-, d- and f-blocks based on the sub-shell of their highest-energy electron. This framework underpins all of OCR spec 3.1, from periodic trends and Group 2 chemistry to the halogens and beyond.