Modern periodic law

Mendeleev's periodic table was a triumph, but it had cracks. Elements such as tellurium and iodine sat "out of order" when arranged strictly by atomic mass, and no one could say why the table repeated its pattern every eight or eighteen elements. The crack was sealed not by a chemist but by a physicist studying X-rays. In 1913, Henry Moseley found a hidden whole number buried in every element's X-ray spectrum — a number that climbed by exactly one, element to element, with no exceptions. That number, the atomic number, became the true basis of the periodic table. This article explains the Modern Periodic Law, shows why atomic number succeeds where atomic mass failed, and walks through how the 18 groups and 7 periods of today's table follow directly from electron arrangement.

The core insight

The Modern Periodic Law states that the physical and chemical properties of elements are a periodic function of their atomic number, and this single change from atomic mass to atomic number removes the ordering anomalies (such as tellurium before iodine) that troubled Mendeleev's table.

The core idea

Moseley's discovery. In 1913, Henry Moseley bombarded a series of elements with fast electrons and studied the characteristic X-rays each element emitted. He found that the frequency of these X-rays was tied to a whole number that increased by exactly one from element to element, with no gaps and no exceptions. This number is the atomic number (ZZ), equal to the number of protons in the nucleus. Atomic mass, by contrast, does not increase in such a clean, unbroken sequence — it can even step backwards for neighbouring elements.

Statement of the law. The Modern Periodic Law says: the physical and chemical properties of elements are a periodic function of their atomic numbers. This replaced Mendeleev's law, which used atomic mass, and it is the single idea that underlies the entire layout of the table used today.

Why the switch matters — the tellurium-iodine anomaly. Tellurium has atomic mass about 127.6 and iodine about 126.9, so mass-ordering places iodine before tellurium. But tellurium's atomic number is 52 and iodine's is 53, so atomic-number-ordering places tellurium first — and this matches their chemistry. Tellurium behaves like oxygen and sulphur (Group 16), while iodine behaves like fluorine, chlorine and bromine (Group 17). Atomic number, not atomic mass, is the true ordering variable.

Layout of the modern periodic table. The table has 18 vertical groups and 7 horizontal periods. Elements in the same group share the same number of valence (outermost-shell) electrons and therefore similar chemical behaviour; elements in the same period share the same number of occupied electron shells. Group 3 to Group 12, spanning Periods 4 to 7, hold the transition elements; two extra rows placed below the main table hold the inner-transition elements (lanthanides and actinides). At this level you only need to know that these blocks exist and roughly where they sit — their detailed chemistry is a later topic. The electron capacity of each shell is fixed by a simple rule, and this rule is the tool that turns a bare atomic number into a period and a group.

nmax⁡=2n2n_{\max} = 2n^2

where: nn is the shell number counted outward from the nucleus (1, 2, 3, ...), and nmax⁡n_{\max} is the maximum number of electrons that shell can hold before the next shell must start filling. This gives capacities of 2, 8, 18, 32 for shells 1, 2, 3, 4.

Figure
A periodic table grid showing 18 groups across and 7 periods down with the transition block in the middle and Moseleys atomic number ordering arrow
Modern periodic table — ordered by atomic number Z, not atomic mass 18 groups (columns) x 7 periods (rows) transition elements (Groups 3-12) P1 P2 P3 P4 P5 P6 P7 Z increases by 1 across a period, then continues into the next row

Why it works

Since the Modern Periodic Law is a statement about periodicity, not a computed quantity, the natural "derivation" here is the reasoning that connects electron-shell filling to the table's shape — this is the tool used to place any element once its atomic number is known. Placing an element in the correct period and group from nothing but its atomic number is a two-step act of reasoning that only needs the shell-capacity rule above and a subtraction, and getting it right is the single most testable skill this topic produces.

Step 1. Convert the atomic number into a shell-by-shell electron distribution. Fill shell 1 first, up to its capacity of 2×12=22\times1^2 = 2; then shell 2, up to 2×22=82\times2^2 = 8; then shell 3, up to 2×32=182\times3^2 = 18 — but note that for the elements on this syllabus (up to around Z=20Z = 20), shell 3 in practice stops filling at 8 once shell 4 begins, so the working capacities to use are 2, 8, 8, 2 in sequence rather than the full 2n22n^2 ceiling. Subtract each shell's electrons from the running total until none remain.

Step 2. Count how many shells received at least one electron — this count is the period number, because a period is defined as a row sharing the same number of occupied shells.

Step 3. Read off the number of electrons in the outermost (last-filled) shell — this is the valence electron count, and for the main-group elements on this syllabus it fixes the group number directly (1 valence electron places an element in Group 1, 2 in Group 2, and so on up to Group 18 for a full outer shell of 8).

Step 4. Cross-check the result against known chemical behaviour where possible — elements in the same group should show family resemblance (for example, all Group 1 elements form compounds of the pattern XClXCl, all Group 2 elements form XCl2XCl_2), which confirms the shell-counting method is consistent with the Modern Periodic Law's promise that properties repeat periodically with atomic number.

Worked example

Problem. An element X has atomic number 12. State which period and which group it belongs to, using the shell-filling rule, and name a chemical property that confirms the placement.

Step 1. Distribute the 12 electrons into shells. Shell 1 takes 2 (capacity 2×12=22\times1^2=2), leaving 12−2=1012-2=10. Shell 2 takes 8 (capacity 2×22=82\times2^2=8), leaving 10−8=210-8=2. Shell 3 takes the remaining 2. Distribution: 2, 8, 2.

Step 2. Count occupied shells: shells 1, 2 and 3 all hold electrons, so X is in Period 3.

Step 3. Read the outermost shell: shell 3 holds 2 valence electrons, so X is in Group 2.

Step 4. Confirm with chemistry: Group 2 elements form chlorides of formula XCl2XCl_2 (for example MgCl2MgCl_2), consistent with X being magnesium — atomic number 12 is indeed magnesium, and it is a known alkaline-earth metal in Period 3, Group 2.

Answer: element X (Z = 12, magnesium) is in Period 3, Group 2.

Competitive stretch

Try the same method on atomic number 17. Shell 1 takes 2 (remaining 15), shell 2 takes 8 (remaining 7), shell 3 takes the remaining 7. Three occupied shells give Period 3; 7 valence electrons give Group 17. This is chlorine, a halogen — and Group 17 elements are known to form compounds such as HClHCl, matching the family pattern for that group.

Common traps

  • Saying the Modern Periodic Law is based on atomic mass — it is based on atomic number, Moseley's discovery, not Mendeleev's original ordering variable.
  • Confusing period with group — a period is a row (same number of occupied shells); a group is a column (same number of valence electrons).
  • Using the full 2n22n^2 ceiling for shell 3 when placing syllabus-level elements — in practice shell 3 fills to 8 before shell 4 begins for the elements studied here, not to its theoretical maximum of 18.
  • Assuming transition-metal or inner-transition-metal chemistry is examinable — the syllabus asks only that you know these blocks exist and roughly where they sit in the table.

Ask the tutor: want to practise finding the period and group for a few more atomic numbers, or see how Moseley's X-ray data actually looked?

Why did Moseley's X-ray work succeed where Mendeleev's atomic-mass table failed?

Atomic mass depends on the number of protons plus neutrons, and different isotopes of the same element can shift this value unpredictably, occasionally making a heavier element sit before a lighter one in the wrong chemical family — tellurium and iodine are the classic case. Moseley's X-ray spectra instead revealed atomic number, the proton count, which increases by exactly one from element to element with no exceptions. Because chemical behaviour is governed by electrons (and hence indirectly by proton count, since atoms are neutral), atomic number turned out to be the true periodic variable, and switching to it removed every mass-based anomaly.

Do I need to memorise the detailed chemistry of transition elements for this chapter?

No. At this stage you only need to know that the modern periodic table contains a transition block (Groups 3 to 12, across Periods 4 to 7) and an inner-transition block (the lanthanides and actinides, usually shown as two separate rows below the main table), and roughly where each sits. Their detailed electron configurations and chemical reactions are studied in later, more advanced chemistry courses, so exam questions at this level will not ask you to go beyond recognising their existence and position.

How is the group number related to valence electrons for every element, not just the ones in worked examples?

For the main-group elements covered at this level (Groups 1, 2, and 13 to 18), the group number is read directly from the number of valence electrons: 1 valence electron means Group 1, up to 8 valence electrons meaning Group 18 (a full, stable outer shell, as in noble gases). This clean rule works because elements in the same group share the same valence-electron count by definition, which is exactly why they show similar chemical behaviour. It does not extend simply to the transition metals in Groups 3 to 12, whose group-numbering follows different rules you are not required to know yet.

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