The Elements In Each Column Have

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The periodic table isn't just a chart. It's a map Most people skip this — try not to..

Every column tells a story. The elements in each column have the same number of valence electrons — and that single fact dictates almost everything about how they behave. Reactivity. Now, bonding. Whether they're metals, nonmetals, or something weird in between.

Most people memorize the groups for a test and forget them. But if you actually understand why the columns work the way they do, chemistry stops being a list of exceptions and starts making sense.

Let's walk through it.

What the Columns Actually Represent

The periodic table is arranged by atomic number — protons, basically. But the shape of the table, the rows and columns, comes from electron configuration.

Each column is a group. In real terms, the elements in each column have the same number of electrons in their outermost shell. In real terms, there are 18 of them. Even so, that's the valence shell. And valence electrons are the only ones that really participate in chemistry The details matter here..

Easier said than done, but still worth knowing.

Inner electrons? Shielded. Think about it: core. They don't bond. They don't react. They're just along for the ride. They sit there Not complicated — just consistent..

So when you look at Group 1 — lithium, sodium, potassium, rubidium, cesium, francium — they all have one valence electron. And because of that, they all want to lose it. Even so, one. On top of that, that's it. Badly.

Group 17? Practically speaking, fluorine, chlorine, bromine, iodine, astatine, tennessine. Because of that, they're one short of a full shell. But seven valence electrons. So they take electrons. Aggressively.

That's the whole game. The column tells you the valence count. The valence count tells you the personality That's the part that actually makes a difference..

The numbering systems (yes, there are two)

You'll see groups labeled 1–18 (IUPAC, modern) and the old A/B system (1A, 2A, 3B… 8A). Consider this: the new one is cleaner. Group 1 = alkali metals. Group 2 = alkaline earth. Groups 3–12 = transition metals. Group 13 = boron group. 14 = carbon group. Plus, 15 = pnictogens. Here's the thing — 16 = chalcogens. 17 = halogens. 18 = noble gases.

I'll use the 1–18 numbers. Less confusion.

Why the Columns Matter More Than the Rows

Rows (periods) show you how many electron shells an element has. Period 1 = one shell. Period 2 = two. And so on Easy to understand, harder to ignore..

But columns show you chemical behavior. Think about it: elements in the same group react similarly. Form similar compounds. Have similar ratios in their formulas Small thing, real impact..

Sodium chloride. All soluble. All 1:1. Practically speaking, all ionic. Lithium chloride. Potassium chloride. All white crystalline solids The details matter here..

Magnesium oxide. Plus, calcium oxide. Strontium oxide. Now, all 1:1. All basic oxides. All high melting points.

This isn't coincidence. It's the valence electrons Simple, but easy to overlook..

The diagonal relationship — a fun exception

Sometimes an element acts more like its diagonal neighbor than its own group. Worth adding: lithium resembles magnesium. Beryllium resembles aluminum. Boron resembles silicon.

Why? Competing trends. Because of that, going down a group: atoms get bigger, ionization energy drops, metallic character increases. Going across a period: atoms get smaller, ionization energy rises, metallic character decreases Not complicated — just consistent..

Move diagonally? Because of that, the two effects partially cancel. You get similar charge density, similar electronegativity, similar chemistry.

It's a reminder: the table has trends, not laws. Exceptions exist. But the column rule holds remarkably well.

Group by Group: What the Elements in Each Column Have in Common

Group 1: Alkali Metals — One Valence Electron, One Goal

Lithium. Sodium. Potassium. Rubidium. Cesium. Francium.

Soft. In real terms, silvery. Low density — lithium floats on oil. Still, low melting points. One valence electron they desperately want to lose.

They form +1 ions. Which means always. No exceptions in normal chemistry.

React violently with water. The reaction gets more intense down the group:

  • Lithium fizzes
  • Sodium dances and melts
  • Potassium ignites
  • Rubidium and cesium explode

They're never found free in nature. Still, too reactive. Always as salts.

What they have in common: +1 oxidation state, ionic bonding, basic oxides, soluble salts, flame tests (crimson, yellow, lilac, red-violet, blue-violet).

Group 2: Alkaline Earth Metals — Two Valence Electrons

Beryllium. Magnesium. Calcium. Strontium. Barium. Radium Worth keeping that in mind..

Harder than Group 1. Higher melting points. Two valence electrons → +2 ions Easy to understand, harder to ignore..

Still reactive, but less so. In real terms, magnesium burns bright white. Calcium reacts steadily with water. Barium's so reactive it's stored under oil.

What they have in common: +2 oxidation state, basic oxides, mostly soluble salts (except sulfates — solubility decreases down the group, opposite of most trends), flame tests (brick red, crimson, green, pale green) Easy to understand, harder to ignore..

Beryllium is the weirdo. Now, small. Because of that, high charge density. On the flip side, covalent character. Worth adding: amphoteric oxide. It's the diagonal relationship with aluminum showing up.

Groups 3–12: Transition Metals — The d-Block Mess

This is where "same valence electrons" gets complicated.

The elements in each column have similar outer electron counts (usually 2 in the s orbital), but the inner d orbitals are filling. And those d electrons participate in bonding.

So you get multiple oxidation states. Iron: +2, +3, +6. Manganese: +2 through +7. Color. Which means magnetism. Catalysis. Complex ions.

Group 3: Scandium, yttrium, lanthanum, actinium. Mostly +3. Boring-ish Less friction, more output..

Group 4: Titanium, zirconium, hafnium. Which means +4 dominant. Very similar to each other — lanthanide contraction makes Zr and Hf nearly identical in size Easy to understand, harder to ignore. Nothing fancy..

Group 11: Copper, silver, gold. On the flip side, relativistic effects make gold… gold-colored. In real terms, +1 and +2 (Cu), +1 (Ag), +1 and +3 (Au). The coinage metals. And unreactive.

What they have in common (within a group): Similar maximum oxidation states. Similar ionic radii trends. But the chemistry diverges more than main groups. Don't treat them like Group 1 And it works..

Group 13: Boron Group — Three Valence Electrons

Boron. Aluminum. Gallium. Indium. Thallium.

Boron is a metalloid. Electron-deficient. Consider this: forms weird multicenter bonds. Everything else: metals But it adds up..

+3 oxidation state dominates. But down the group, +1 gets more stable. Thallium(I) is more stable than thallium(III) — the inert pair effect. The 6s electrons don't want to ionize. Relativistic stabilization.

What they have in common: Three valence electrons, +3 oxidation state (mostly), amphoteric oxides (except B₂O₃ acidic, Tl₂O basic), form [M(OH)₄]⁻ complexes.

Group 14: Carbon Group — Four Valence Electrons

Carbon. Silicon. Germanium. Tin. Lead.

The most dramatic transition in the table. Nonmetal → metalloid → metal.

Carbon: covalent networks (diamond, graphite), millions of organic compounds. Silicon: covalent networks, semiconductors, silicates. Germanium: semiconductor. Tin: two allotropes (gray = semiconductor, white = metal). Lead: soft metal That's the part that actually makes a difference..

+4 and +2 oxidation states. Inert pair effect hits hard — lead(IV) is a strong oxidizer

, while lead(II) is the stable form. Tin(II) is reducing; tin(IV) is not And that's really what it comes down to..

What they have in common: Four valence electrons, +4 oxidation state (mostly), but +2 becomes more stable down the group. Carbon forms an unparalleled array of compounds due to catenation and strong C-C bonds Small thing, real impact. But it adds up..

Group 15: Nitrogen Group — Five Valence Electrons

Nitrogen. Phosphorus. Arsenic. Antimony. Bismuth.

Another dramatic shift: from diatomic gas to brittle solids Most people skip this — try not to..

Nitrogen: inert N≡N triple bond. Worth adding: phosphorus: highly reactive allotropes (white P₄, red P, black P). Also, antimony: metalloid. Consider this: arsenic: metalloid. Bismuth: post-transition metal It's one of those things that adds up..

+5 and +3 oxidation states. The inert pair effect again — bismuth(III) is more stable than bismuth(V).

What they have in common: Five valence electrons, +5 oxidation state (mostly), but +3 becomes more stable down the group. Form pnictides, nitrides, and various oxyacids Simple as that..

Group 16: Chalcogens — Six Valence Electrons

Oxygen. Sulfur. Selenium. Tellurium. Polonium.

Oxygen: unique due to high electronegativity and small size. Forms strong hydrogen bonds. Diatomic O₂ and reactive O₃ Worth keeping that in mind..

Sulfur: S₈ rings, multiple allotropes, essential in organic chemistry and biochemistry.

Selenium and tellurium: increasingly metallic. Polonium: radioactive metal.

+2, +4, and -2 oxidation states. Oxygen is almost always -2 (except in peroxides and superoxides).

What they have in common: Six valence electrons, -2 oxidation state (mostly), form chalcrides, and various oxyacids. Oxygen's chemistry is exceptional due to its position Worth keeping that in mind..

Group 17: Halogens — Seven Valence Electrons

Fluorine. Chlorine. Bromine. Iodine. Astatine The details matter here..

The most reactive nonmetals. Diatomic molecules (F₂, Cl₂, Br₂, I₂). Physical properties change dramatically: gases → liquid → solid → solid (with increasing atomic number) Not complicated — just consistent..

+1, +3, +5, +7 oxidation states. But -1 is their defining characteristic — they're electron-hungry.

Fluorine: the most electronegative element. Bromine: liquid at room temperature. Still, reacts with almost everything. Chlorine: essential for life (NaCl, disinfection). Iodine: solid, purple vapor.

Astatine: radioactive, rare, and poorly understood.

What they have in common: Seven valence electrons, -1 oxidation state (dominant), form interhalogens, and are strong oxidizing agents. Reactivity decreases down the group.

Group 18: Noble Gases — Full Shells

Helium. Neon. Argon. Krypton. Xenon. Radon. Oganesson.

Inert. In practice, full valence shells. Minimal reactivity — the original "inert gases The details matter here. No workaround needed..

Except xenon and radon, which can form compounds under extreme conditions. Oganesson is predicted to be reactive due to relativistic effects.

What they have in common: Complete valence shells, zero oxidation state (mostly), and extremely low chemical reactivity. Used in lighting, lasers, and as inert atmospheres Worth keeping that in mind..


The Bigger Picture

The periodic table isn't just a chart — it's a predictive machine. Once you understand the patterns of electron configuration, atomic size, ionization energy, and electronegativity, you can anticipate how elements will behave It's one of those things that adds up..

Main group elements follow cleaner trends. Transition metals are messy but rich in complexity. The further down you go, the more the inert pair effect dominates. The smaller the atom, the more covalent character appears And that's really what it comes down to. Turns out it matters..

And beryllium? It will always be the odd one out — small enough to mimic aluminum's behavior, but too different to truly fit anywhere else.

In the end, the periodic table rewards those who look beyond simple electron counting. It's about understanding why those electrons matter, how they interact, and what happens when atoms get too big, too small, or too weird for their own good Practical, not theoretical..

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