Blocks, groups and periods
Open the long-form periodic table and three organising ideas run through it at once: seven horizontal periods, eighteen vertical groups, and four colour-coded blocks (, , , ). None of these are arbitrary — each is read directly off an element's ground-state electronic configuration, the same configuration you learned to build with the Aufbau, Pauli, and Hund rules in the Structure of Atom unit. Once you can turn a configuration into a period, group, and block on sight, the table stops being a chart to memorise and becomes a tool that predicts how an element will behave — because elements that share a block or a group share a valence-shell pattern, and valence electrons decide chemistry. This article builds that reading skill from the ground up, with the sulphur and chromium examples worked in full.
An element's period equals the highest principal quantum number in its ground-state configuration, its block is fixed by which subshell holds the last ("differentiating") electron, and its group follows a countable rule built from the valence electrons of that block.
The core idea
Periods are the seven horizontal rows. A new period begins exactly when electrons start occupying a new principal shell. Period 1 holds only 2 elements (H, He; ). Periods 2 and 3 hold 8 each (, only and subshells filling). Periods 4 and 5 hold 18 each, because the -block now joins in. Periods 6 and 7 hold 32 each, because the -block joins too. So the period number is simply the largest appearing in the configuration — no counting of electrons required.
Groups are the eighteen vertical columns. Elements in one group share the same pattern of valence-shell configuration, and it is that shared pattern — not shared atomic number — that gives them family chemistry. Group 1 (alkali metals) is always ; Group 17 (halogens) is always ; Group 18 (noble gases) is always (except He, ). Because the pattern repeats every time a shell fills the same way, the table has vertical families rather than just an unbroken sequence of 118 unrelated elements.
Blocks classify elements by where the differentiating electron lands in the Aufbau order:
- -block — Groups 1–2, valence , reactive metals.
- -block — Groups 13–18, valence , spans metals, metalloids, non-metals, and the noble gases.
- -block (transition elements) — Groups 3–12, general valence ; the differentiating electron enters an inner subshell while the outer shell is already .
- -block (inner-transition elements) — lanthanides and actinides, shown as a separate strip below the main table; general valence .
Because group membership is really a statement about the valence-electron count, it can be written as a formula once you know the block. For a -block element with valence configuration ( to ),
where: is the number of electrons in the outermost subshell (from 1 to 6), and the constant accounts for the two electrons plus the ten already-filled -electrons counted into the numbering convention for that period. For a -block element with configuration , the rule is simpler still: , the total count of - and -electrons beyond the preceding noble-gas core.
Why it works
The differentiating-electron rule is the reason this classification is consistent rather than a memorised list. The Aufbau order fills subshells roughly as — note that fills before , even though belongs to a lower shell number. This is exactly why the -block "lags behind" by one period: a -block element's outermost occupied shell is (giving its period), but its last-added electron sits in the inner subshell (giving its block). The same logic pushes the -block two shells inward, , which is why lanthanides and actinides are drawn as a detached strip rather than widening the main table by fourteen more columns. Reading a configuration therefore separates two different questions cleanly: "which shell is outermost" answers the period, and "which subshell just received an electron" answers the block — group number then follows once the block tells you which valence pattern to count.
The goal is to show, purely by counting electrons against the eighteen-group IUPAC numbering convention, why a -block element with valence configuration sits in group , so that a student can assign any -block group number without consulting a printed table, using nothing beyond the definition of the modern eighteen-column numbering scheme and simple addition.
Step 1. State the numbering convention. The modern IUPAC scheme numbers all eighteen columns 1 to 18 in order across the table, regardless of block. Groups 1 and 2 are the -block (, ). Groups 3 to 12 are the ten columns of the -block, one column per possible electron count from 1 to 10. Groups 13 to 18 are the six columns of the -block.
Step 2. Fix the starting point of the -block. Since Groups 1–2 use two columns and Groups 3–12 use ten columns, the -block's first column, corresponding to (one -electron, valence ), must be column number . This matches Group 13, the boron family.
Step 3. Generalise to any . Each additional -electron simply moves one column to the right, so sits at column . Check the boundary: for (a full shell), the formula gives , the noble-gas column — consistent with Group 18.
Step 4. Confirm with a known case. Oxygen has valence configuration , so , giving group . Oxygen is indeed in Group 16 (the chalcogens), the same group as sulphur worked below. Verified: Group 13 (boron family); Group 16 (chalcogens, matches sulphur and oxygen); Group 18 (noble gases) — all consistent with the standard eighteen-column table.
Worked example
Question: An element has ground-state configuration . Identify its period, group, and block, and name the element.
Step 1. Count total electrons: , so . This is sulphur.
Step 2. The highest principal shell occupied is (the and electrons), so the element is in Period 3.
Step 3. The valence configuration is , matching the pattern with . The last electron enters a orbital, so the element is in the -block. Applying formula (1): .
Step 4. Answer: sulphur sits in Period 3, Group 16, -block — a chalcogen, consistent with its known chemistry (it forms , , and sits directly below oxygen).
Competitive stretch
Question: Chromium () has the "anomalous" ground-state configuration rather than the Aufbau-predicted . Find its period, group, and block.
Step 1. accounts for ; adding reaches .
Step 2. The outermost occupied shell is (the electron), so chromium is in Period 4. The differentiating electron enters the inner subshell, so it is a -block element.
Step 3. Using the -block rule with () and (): .
Step 4. Answer: chromium is Period 4, Group 6, -block, unchanged by the Hund's-rule anomaly — the half-filled stability shifts one electron between subshells but the differentiating subshell is still , so the block assignment is unaffected.
Common traps
- Placing helium in the -block because it is drawn above the noble gases — its configuration is , so it is genuinely -block; it is only positioned with Group 18 for family resemblance.
- Assuming every period has 8 elements — Periods 4–5 have 18 (the -block joins) and Periods 6–7 have 32 (the -block joins too).
- Swapping "period" (row, set by the highest ) with "group" (column, set by the valence pattern) — they answer different questions from the same configuration.
- Applying the simple Aufbau order blindly to - and -block elements — a handful (Cr, Cu, and some lanthanides/actinides) deviate for extra stability of half-filled or fully-filled subshells, but the block is still fixed by where the actual differentiating electron sits, not by the "expected" configuration.
Ask the tutor: if you want practice converting an unfamiliar electronic configuration straight into period, group, and block — or want more anomalous-configuration examples like chromium — ask the AI tutor for extra worked problems.
Why does Group 3 to Group 12 skip straight to 12+x for the p-block instead of continuing 1, 2, 3 ...
The eighteen-column IUPAC scheme numbers every column of the long-form table in one continuous sequence, not block by block from scratch. Groups 1 to 2 are used up by the two s-block columns, and Groups 3 to 12 are used up by the ten d-block columns, so by the time the p-block starts there are already twelve columns behind it — its first column has to be Group 13, not Group 1. This is exactly what the derivation above counts through step by step.
Does the group number formula 12+x work for every element in that column, across all periods?
Yes, for the p-block, because the formula depends only on x, the number of p-electrons in the valence shell, not on which period the element sits in. Carbon (2p2), silicon (3p2), and germanium (4p2) are all in Group 14 by the same reasoning, even though they are in different periods, because they share the same valence pattern ns2np2. That shared pattern, not the period, is what fixes the group.
If chromium and copper break the simple Aufbau order, how do I know which block they belong to without memorising exceptions?
You do not need to memorise the exceptions — you only need the actual ground-state configuration, which your syllabus gives or which you can look up when it matters. Once you have the real configuration, the same rule applies exactly as for any other element: find the subshell that received the last electron, and that subshell fixes the block. For chromium that subshell is 3d, so it is d-block regardless of whether the electron count in 3d is 4 or 5. The anomaly changes how many electrons sit in 3d versus 4s; it never changes which type of subshell is being filled.