From Atomic Weight to Atomic Number
When Dmitri Mendeleev published the Periodic Law in 1869, chemists knew nothing about the internal structure of the atom. His law was framed in the only quantitative property then available: the properties of the elements are a periodic function of their atomic weights. Arranging elements by increasing atomic weight worked remarkably well, and Mendeleev's boldness in leaving gaps for undiscovered elements such as eka-aluminium (gallium) and eka-silicon (germanium) made the table famous.
Yet the atomic-weight basis carried a quiet flaw. A handful of element pairs refused to behave. Mendeleev himself had to place iodine after tellurium, even though iodine has the lower atomic weight, simply because its properties matched the halogens fluorine, chlorine and bromine. He rationalised this by assuming the atomic-weight measurements were in error. The deeper truth — that some property other than mass governs chemical behaviour — had to wait for the structure of the atom to be uncovered in the early twentieth century.
That property turned out to be the atomic number, the nuclear charge, equal to the number of protons or to the number of electrons in a neutral atom. The historical anomalies dissolve the moment elements are ordered by atomic number rather than atomic weight.
| Pair | Atomic weight | Atomic number (Z) | Correct order by |
|---|---|---|---|
| Tellurium (Te) | 127.6 | 52 | Atomic number — Te before I |
| Iodine (I) | 126.9 | 53 | |
| Argon (Ar) | 39.9 | 18 | Atomic number — Ar before K |
| Potassium (K) | 39.1 | 19 |
By weight, tellurium would sit after iodine and argon after potassium — both wrong chemically. By atomic number the order is correct, with tellurium ($Z = 52$) preceding iodine ($Z = 53$) and argon ($Z = 18$) preceding potassium ($Z = 19$). The anomaly was not a measurement error at all; it was a signal that atomic number, not atomic weight, is the fundamental organising quantity.
Moseley's X-ray Experiment
The decisive evidence came in 1913 from the English physicist Henry Moseley. He bombarded different metallic targets with high-energy electrons and recorded the characteristic X-rays each element emitted. Moseley found a strikingly simple regularity: a plot of the square root of the X-ray frequency against the atomic number gave a straight line, whereas the corresponding plot against atomic mass did not.
Expressed as a relation, Moseley's observation reads
$\sqrt{\nu} = a\,(Z - b)$
where $\nu$ is the frequency of the emitted X-rays, $Z$ is the atomic number, and $a$ and $b$ are constants for a given X-ray series. Because the relationship is linear in $Z$ — and not in atomic mass — Moseley concluded that the atomic number is a more fundamental property of an element than its atomic mass. Mendeleev's Periodic Law was modified accordingly.
Why the √ν–vs–Z line is straight while √ν–vs–mass is not.
The teal line is the ordered, monotonic dependence on $Z$; the coral points show how the same data scatter when plotted against atomic mass. The straight line is what told Moseley that $Z$ is fundamental.
The new law revealed important analogies among the 94 naturally occurring elements and stimulated renewed interest in inorganic chemistry, an interest that has carried into the present with the creation of artificially produced, short-lived elements.
Statement of the Modern Periodic Law
With atomic number established as the fundamental property, Mendeleev's law is restated in its modern form:
The physical and chemical properties of the elements are periodic functions of their atomic numbers.
The single change from Mendeleev's wording — "atomic weights" replaced by "atomic numbers" — is small in text but profound in consequence. It anchors classification to the count of protons and electrons rather than to a mass that varies with isotopic abundance. The table below sets the two laws side by side.
| Feature | Mendeleev's Periodic Law (1869) | Modern Periodic Law (post-1913) |
|---|---|---|
| Basis of ordering | Atomic weight | Atomic number (Z) |
| Statement | Properties are a periodic function of atomic weights | Properties are periodic functions of atomic numbers |
| Anomalous pairs (Te/I, Ar/K) | Required ad hoc reordering | Resolved automatically |
| Physical meaning | None known (atomic structure unknown) | Reflects nuclear charge and electronic configuration |
| Decisive evidence | Predicted properties of gallium, germanium | Moseley's X-ray spectra (1913) |
"Atomic weight" is Mendeleev — not Modern
A recurring distractor swaps the two laws. Any option that ends the periodic-function statement with "atomic weights" or "atomic masses" is Mendeleev's law, not the Modern Periodic Law. The Modern Periodic Law uses atomic number only.
Modern Periodic Law → periodic function of atomic number (Z); Mendeleev → atomic weight.
Structure of the Long Form
Many forms of the periodic table have been devised. The modern "long form" is the most convenient and widely used. Its horizontal rows — which Mendeleev called series — are the periods, and its vertical columns are the groups. Elements with similar outer electronic configurations occupy the same group, which is why groups are also called families.
Following the IUPAC recommendation, the groups are numbered 1 to 18, replacing the older notation of IA…VIIA, VIII, IB…VIIB and 0. There are altogether seven periods. To preserve the table's compact rectangular shape and keep chemically similar elements together, the fourteen 4f elements (lanthanoids) and fourteen 5f elements (actinoids) of the sixth and seventh periods are placed in two separate panels at the bottom.
Schematic block structure of the long-form periodic table.
The s-block (groups 1–2) sits at the left, the p-block (groups 13–18) at the right, the d-block bridge (groups 3–12) between them, and the f-block strip is detached below. The position of the last orbital filled fixes each block.
Each cell of the long form carries an element's atomic number and ground-state outer electronic configuration. The same arrangement also sorts elements physically: a diagonal line from boron ($Z = 5$) to tellurium ($Z = 52$) separates the metals on the lower-left from the non-metals on the upper-right, with the metalloids straddling the line.
The blocks here are the foundation for classifying every element. See s, p, d and f Blocks for the orbital-filling rules that define each region.
Periods and the Principal Quantum Number
The period number is not an arbitrary label. It corresponds to the highest principal quantum number (n) of the elements in that period — equivalently, $n$ for the outermost or valence shell. Successive periods are associated with the filling of the next higher principal energy level: $n = 1$ for period 1, $n = 2$ for period 2, and so on.
From this single rule the length of each period follows. The number of elements in a period equals twice the number of atomic orbitals available in the energy level being filled, because each orbital holds two electrons. Period 1 fills only the $1s$ orbital and so contains two elements; periods 2 and 3 fill $ns$ and $np$ (four orbitals, eight elements); periods 4 and 5 also fill the $(n-1)d$ set (nine orbitals total, eighteen elements); and period 6 additionally fills the $(n-2)f$ set (sixteen orbitals total, thirty-two elements).
| Period | Highest n | Orbitals filled | No. of elements | Begins / ends |
|---|---|---|---|---|
| 1 | 1 | 1s | 2 | H → He |
| 2 | 2 | 2s, 2p | 8 | Li → Ne |
| 3 | 3 | 3s, 3p | 8 | Na → Ar |
| 4 | 4 | 4s, 3d, 4p | 18 | K → Kr |
| 5 | 5 | 5s, 4d, 5p | 18 | Rb → Xe |
| 6 | 6 | 6s, 4f, 5d, 6p | 32 | Cs → Rn |
| 7 | 7 | 7s, 5f, 6d, 7p | 32 (incomplete*) | Fr → Og |
*The seventh period was incomplete in earlier accounts; like the sixth, it has a theoretical maximum of 32 elements, and elements up to atomic number 118 (oganesson) are now known. The signature sequence to memorise is therefore 2, 8, 8, 18, 18, 32.
Justify the presence of 18 elements in the fifth period.
When $n = 5$, the orbitals that fill in increasing energy order are $5s$, then $4d$, then $5p$ (the $4f$ level fills only in period 6). That gives one $5s$ orbital, five $4d$ orbitals and three $5p$ orbitals — nine orbitals in all. Nine orbitals accommodate $9 \times 2 = 18$ electrons, hence $18$ elements: rubidium ($Z = 37$) through xenon ($Z = 54$), with the 4d transition series beginning at yttrium ($Z = 39$).
Why the Law Follows from Electronic Configuration
The Modern Periodic Law is more than an empirical ordering rule; it is a logical consequence of the way electrons fill orbitals. Since the atomic number equals the number of electrons in a neutral atom, fixing $Z$ fixes the electronic configuration. As $Z$ increases one unit at a time, electrons enter orbitals in a regular pattern, so the outer (valence) configuration recurs at definite intervals.
Chemical bonding occurs almost entirely through the outermost shell: an atom loses, gains or shares its valence electrons during reactions. Elements with identical outer electronic configurations therefore display similar physical and chemical properties and are placed in the same group. It is in this sense that the Periodic Law is, in NCERT's words, "essentially the consequence of the periodic variation in electronic configurations."
How the same valence configuration reappears down a group.
Lithium, sodium, potassium and rubidium all end in $ns^1$. Their atomic numbers differ widely, yet the periodic recurrence of the valence configuration is exactly why they share the chemistry of the alkali metals — the visible face of the Modern Periodic Law.
This is also why the law and the long-form table are inseparable. The table is not merely a chart; it is the geometric expression of orbital filling. Reading an element's position tells you the quantum numbers of its last filled orbital, and conversely, the electronic configuration predicts where an element must sit.
The same logic explains the most useful consequence of the law for problem-solving: elements with similar outer configurations behave alike, regardless of how heavy they are. Group 17 (the halogens) all end in $ns^2 np^5$ and are one electron short of a noble-gas octet, so each is a strong oxidising non-metal that forms a singly-charged anion. Group 18 ends in $ns^2 np^6$ (helium in $1s^2$), the stable closed-shell arrangement that accounts for the near-inertness of the noble gases. When a NEET stem asks for the family of an unfamiliar or super-heavy element, the route is always the same: write the configuration, read off the valence shell, and map it to a group.
It is worth noting one boundary of the law's reach. Periodicity is governed by the valence configuration, not by total electron count, which is why widely separated atomic numbers can share a column. The recurrence is also why the lengths of the repeating blocks change — short for the s/p periods, longer once the d and f orbitals join — exactly the lengthening pattern Lothar Meyer first glimpsed in his atomic-volume curves before the atom's structure was known.
Period number = highest n, not number of shells in the core
Students sometimes count occupied shells or confuse the period number with the group number. The period number equals the highest principal quantum number reached by the valence electrons. For example, scandium ($3d^1 4s^2$) is in period 4 because its highest $n$ is 4, even though its last electron enters a $3d$ orbital.
Period number = highest $n$ of the valence shell; group reflects the outer configuration.
Modern Periodic Law in one screen
- Statement: the physical and chemical properties of the elements are periodic functions of their atomic numbers.
- Moseley (1913): $\sqrt{\nu}$ versus $Z$ is a straight line → atomic number is more fundamental than atomic mass.
- Why Z: atomic number = nuclear charge = number of protons = number of electrons in a neutral atom.
- Long form: 7 periods (rows), 18 groups (columns, IUPAC 1–18); lanthanoids and actinoids in two bottom panels.
- Period = highest n; elements per period follow 2, 8, 8, 18, 18, 32 because count = 2 × (orbitals being filled).
- Root cause: the law is a consequence of the periodic variation in outer electronic configurations.