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 (ss, pp, dd, ff). 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.

The core insight

An element's period equals the highest principal quantum number nn 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; n=1n=1). Periods 2 and 3 hold 8 each (n=2,3n=2,3, only ss and pp subshells filling). Periods 4 and 5 hold 18 each, because the dd-block now joins in. Periods 6 and 7 hold 32 each, because the ff-block joins too. So the period number is simply the largest nn 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 ns1ns^1; Group 17 (halogens) is always ns2np5ns^2np^5; Group 18 (noble gases) is always ns2np6ns^2np^6 (except He, 1s21s^2). 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:

  • ss-block — Groups 1–2, valence ns1 or 2ns^{1\text{ or }2}, reactive metals.
  • pp-block — Groups 13–18, valence ns2np1–6ns^2np^{1\text{–}6}, spans metals, metalloids, non-metals, and the noble gases.
  • dd-block (transition elements) — Groups 3–12, general valence (n−1)d1–10ns0–2(n-1)d^{1\text{–}10}ns^{0\text{–}2}; the differentiating electron enters an inner (n−1)d(n-1)d subshell while the outer shell is already nn.
  • ff-block (inner-transition elements) — lanthanides and actinides, shown as a separate strip below the main table; general valence (n−2)f1–14(n−1)d0–1ns2(n-2)f^{1\text{–}14}(n-1)d^{0\text{–}1}ns^2.

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 pp-block element with valence configuration ns2npxns^2np^x (x=1x = 1 to 66),

Group=12+x.(1)\text{Group} = 12 + x. \qquad (1)

where: xx is the number of electrons in the outermost pp subshell (from 1 to 6), and the constant 1212 accounts for the two nsns electrons plus the ten already-filled dd-electrons counted into the numbering convention for that period. For a dd-block element with configuration (n−1)dansb(n-1)d^{a}ns^{b}, the rule is simpler still: Group=a+b\text{Group} = a + b, the total count of dd- and ss-electrons beyond the preceding noble-gas core.

Figure
The long form periodic table split into four colour blocks s p d and f with period numbers on the left and group numbers eighteen columns across the top
Blocks of the periodic table, by differentiating electron s-block Groups 1-2 d-block Groups 3-12, Periods 4-7 p-block Groups 13-18 f-block — lanthanides and actinides, shown below the table P1 P2 P3 P4-5 P6-7

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 1s,2s,2p,3s,3p,4s,3d,4p,…1s,2s,2p,3s,3p,4s,3d,4p,\dots — note that 4s4s fills before 3d3d, even though 3d3d belongs to a lower shell number. This is exactly why the dd-block "lags behind" by one period: a dd-block element's outermost occupied shell is nsns (giving its period), but its last-added electron sits in the inner (n−1)d(n-1)d subshell (giving its block). The same logic pushes the ff-block two shells inward, (n−2)f(n-2)f, 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.

Derivation ADeriving the group number formula for a p-block element from its valence configuration

The goal is to show, purely by counting electrons against the eighteen-group IUPAC numbering convention, why a pp-block element with valence configuration ns2npxns^2np^x sits in group 12+x12+x, so that a student can assign any pp-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 ss-block (ns1ns^1, ns2ns^2). Groups 3 to 12 are the ten columns of the dd-block, one column per possible (n−1)d(n-1)d electron count from 1 to 10. Groups 13 to 18 are the six columns of the pp-block.

Step 2. Fix the starting point of the pp-block. Since Groups 1–2 use two columns and Groups 3–12 use ten columns, the pp-block's first column, corresponding to np1np^1 (one pp-electron, valence ns2np1ns^2np^1), must be column number 2+10+1=132 + 10 + 1 = 13. This matches Group 13, the boron family.

Step 3. Generalise to any pxp^x. Each additional pp-electron simply moves one column to the right, so npxnp^x sits at column 13+(x−1)=12+x13 + (x-1) = 12 + x. Check the boundary: for x=6x=6 (a full ns2np6ns^2np^6 shell), the formula gives 12+6=1812+6=18, the noble-gas column — consistent with Group 18.

Step 4. Confirm with a known case. Oxygen has valence configuration 2s22p42s^22p^4, so x=4x=4, giving group 12+4=1612+4=16. Oxygen is indeed in Group 16 (the chalcogens), the same group as sulphur worked below. Verified: x=1⇒x=1\Rightarrow Group 13 (boron family); x=4⇒x=4\Rightarrow Group 16 (chalcogens, matches sulphur and oxygen); x=6⇒x=6\Rightarrow Group 18 (noble gases) — all consistent with the standard eighteen-column table.

Worked example

Question: An element has ground-state configuration 1s2 2s2 2p6 3s2 3p41s^2\,2s^2\,2p^6\,3s^2\,3p^4. Identify its period, group, and block, and name the element.

Step 1. Count total electrons: 2+2+6+2+4=162+2+6+2+4 = 16, so Z=16Z=16. This is sulphur.

Step 2. The highest principal shell occupied is n=3n=3 (the 3s3s and 3p3p electrons), so the element is in Period 3.

Step 3. The valence configuration is 3s23p43s^23p^4, matching the pattern ns2npxns^2np^x with x=4x=4. The last electron enters a 3p3p orbital, so the element is in the pp-block. Applying formula (1): Group=12+4=16\text{Group} = 12+4 = 16.

Step 4. Answer: sulphur sits in Period 3, Group 16, pp-block — a chalcogen, consistent with its known chemistry (it forms SO2\text{SO}_2, H2S\text{H}_2\text{S}, and sits directly below oxygen).

Competitive stretch

Question: Chromium (Z=24Z=24) has the "anomalous" ground-state configuration [Ar] 3d5 4s1[\text{Ar}]\,3d^5\,4s^1 rather than the Aufbau-predicted [Ar] 3d4 4s2[\text{Ar}]\,3d^4\,4s^2. Find its period, group, and block.

Step 1. [Ar][\text{Ar}] accounts for Z=18Z=18; adding 3d54s13d^54s^1 reaches Z=24Z=24.

Step 2. The outermost occupied shell is n=4n=4 (the 4s14s^1 electron), so chromium is in Period 4. The differentiating electron enters the inner 3d3d subshell, so it is a dd-block element.

Step 3. Using the dd-block rule Group=a+b\text{Group} = a+b with a=5a=5 (3d53d^5) and b=1b=1 (4s14s^1): Group=5+1=6\text{Group} = 5+1 = 6.

Step 4. Answer: chromium is Period 4, Group 6, dd-block, unchanged by the Hund's-rule anomaly — the half-filled 3d53d^5 stability shifts one electron between subshells but the differentiating subshell is still 3d3d, so the block assignment is unaffected.

Common traps

  • Placing helium in the pp-block because it is drawn above the noble gases — its configuration is 1s21s^2, so it is genuinely ss-block; it is only positioned with Group 18 for family resemblance.
  • Assuming every period has 8 elements — Periods 4–5 have 18 (the dd-block joins) and Periods 6–7 have 32 (the ff-block joins too).
  • Swapping "period" (row, set by the highest nn) with "group" (column, set by the valence pattern) — they answer different questions from the same configuration.
  • Applying the simple Aufbau order blindly to dd- and ff-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.

Before this

Where this leads