1.3.2 · D2Materials & Atomic Structure

Visual walkthrough — Valence electrons and bonding

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Prerequisites we lean on (build them if rusty): Atomic structure and electron shells, and where we head next: Silicon crystal lattice, Energy bands and band gap.


Step 1 — Draw the atom and find its outermost ring

WHAT. We picture a silicon atom as a nucleus (the heavy centre, charge ) surrounded by electrons living on nested rings called shells. A shell is just "an allowed distance-band where electrons are permitted to orbit." The innermost ring is lowest energy; each ring out is higher.

WHY. Bonding is decided by the outermost occupied ring only. Inner electrons sit deep in the nucleus's pull and never leave — they are spectators. So before anything else we must isolate that outer ring and count who lives there.

PICTURE. Silicon's 14 electrons fill: 2 in ring 1, 8 in ring 2, and 4 in ring 3 (the outer ring). Those 4 are the valence electrons — coloured pale yellow below.


Step 2 — State the goal every atom chases: 8

WHAT. We give the atom a target: outer shells "want" to hold 8 electrons. We call this the octet rule. Silicon has 4, so it is 4 short.

WHY. A full outer shell (8 electrons) is a low-energy, stable, symmetric arrangement — nature always rolls downhill toward low energy, so atoms rearrange electrons to reach 8. This "distance from 8" is the driving force of all bonding.

PICTURE. A gauge: silicon's needle sits at 4 out of 8 — exactly halfway. Not eager to dump electrons (like a metal with 1), not eager to grab (like chlorine with 7). Dead centre.


Step 3 — Share instead of transfer: build one covalent bond

WHAT. Two silicon atoms each contribute one electron to a common pair that both atoms count. That shared pair is a covalent bond.

WHY. Neither atom can afford to lose 4 electrons or gain 4 (too much energy cost). Sharing lets both atoms count the same pair toward their octet — a bargain that lowers energy for both.

PICTURE. Two nuclei, one electron from each, meeting in the middle as a chalk-blue shared pair. The left atom now "sees" its own 3 remaining plus the shared pair… we finish the count in Step 4.


Step 4 — Four neighbours, octet complete: the lattice logic

WHAT. One bond gives silicon a share of 2 electrons but it needs 4 more total. So it forms 4 bonds, one to each of 4 neighbours.

WHY. Each bond supplies a share of 1 "extra" electron. Silicon is 4 short → it needs 4 bonds. This is not a choice; it is forced by the arithmetic .

PICTURE. Central silicon with 4 chalk-blue bonds radiating to 4 neighbour atoms. Count around the centre: its own 4 electrons plus the 4 it shares in from neighbours . Octet satisfied. This repeating pattern is the Silicon crystal lattice.


Step 5 — Why the bond has a length: attraction vs repulsion

WHAT. Two atoms don't collapse into each other, nor drift apart. They settle at a fixed separation. To see why, we track their combined potential energy as a function of separation (the distance between two nuclei).

WHY this tool — energy vs distance? Force is hard to eyeball, but energy has a shape: systems roll to the lowest point of an energy curve like a ball rolling into a valley. Plotting turns "where do atoms settle?" into "where is the bottom of the valley?" — a question we can answer by eye and, in Step 6, by calculus.

PICTURE. Two competing effects:

  • Attraction (electrons pulled to both nuclei) dominates at long range → pulls atoms together → lowers energy.
  • Repulsion (nuclei pushing apart, electron clouds resisting overlap) dominates at short range → shoots energy up sharply.

Their sum is a valley: energy falls as atoms approach, hits a minimum, then rockets up if pushed closer.


Step 6 — Find the bottom of the valley with a derivative

WHAT. We locate the exact separation where the valley bottoms out. That is the equilibrium bond length — the distance atoms actually sit at.

WHY the derivative? The derivative measures the slope of the energy curve — how steeply energy rises or falls as changes. At the very bottom of a valley the ground is momentarily flat: slope . So "find the minimum" becomes the clean equation . No other tool pinpoints a curve's bottom so directly.

PICTURE. Zoom on the valley floor: to the left the slope tilts down-hill, to the right it tilts up-hill, and exactly at the tangent line is horizontal (slope ).


Step 7 — The valley DEPTH is the bond energy (and the band gap)

WHAT. The vertical distance from the valley floor up to the line is — the bond energy: how much energy you must pump in to yank the atoms apart.

WHY. A deeper valley means a stronger bond, meaning it takes more energy to break. For a whole crystal this "energy to free an electron from its bond" is exactly the band gap . Silicon's valley is moderate — about .

PICTURE. Same valley, now with a chalk-pink arrow measuring its depth, labelled "bond energy ." A shallow valley (weak bond) and a deep valley (strong bond) shown for contrast.


Step 8 — The degenerate cases (never leave the reader stranded)

WHAT. We check the boundary scenarios the formula and the physics must survive.

WHY. A good derivation predicts its own limits. If any input breaks the picture, the reader deserves to see it.

PICTURE. Four small panels, one per edge case.

  • (atoms shoved together): repulsion blows up → . The steep left wall. Atoms cannot occupy the same point — this is what gives matter its solidity.
  • (atoms far apart): both terms , so from below. No interaction — free atoms, no bond.
  • K: no thermal energy to lift an electron out of the valley → every valence electron stays bonded → silicon behaves like an insulator at absolute zero.
  • (attraction and repulsion equally sharp): exponent divides by zero → no equilibrium length → no stable bond. This confirms why repulsion must be sharper () for bonds to exist at all.

The one-picture summary

Everything on one board: atom → count 4 → share into 4 bonds → the energy valley whose bottom () sets the bond length and whose depth sets the band gap that makes silicon a semiconductor.

Recall Feynman retelling — the whole walkthrough in plain words

Picture a silicon atom as a tiny sun with rings of electrons. Only the outermost ring matters, and it holds 4 electrons. Every atom secretly wants 8 in that ring to feel stable, so silicon is 4 short. It's too "middle-of-the-road" to steal or give away 4 electrons, so it does the neighbourly thing: it shares one electron with each of 4 buddies, and each buddy shares one back — now everyone counts to 8 and is happy. That handshake between two atoms is a bond, and it has a comfortable arm's-length distance: too close and the atoms shove apart (repulsion), too far and the pull weakens (attraction). Draw energy against distance and you get a valley; the bottom of the valley is that comfy distance, and we find it by asking "where is the ground flat?" — that's the derivative set to zero. How deep the valley is tells you how hard the bond is to break — and for silicon it's a moderate depth (about 1.1 eV). Too deep and no electron ever escapes (insulator); no valley and they all wander (metal); moderate, and a little warmth frees the odd electron to carry current. That's a semiconductor — and it all fell out of the number 4.

Recall Quick self-check

Why does silicon form exactly 4 bonds? ::: It has 4 valence electrons and needs 4 more to reach an octet of 8, sharing one with each of 4 neighbours. What condition locates the equilibrium bond length? ::: The slope of the energy curve is zero, (bottom of the valley). For , what is ? ::: . What must be true of and for a stable bond to exist? ::: (repulsion sharper than attraction); otherwise the exponent is undefined. What does the valley DEPTH correspond to physically? ::: The bond energy — and for a crystal, the band gap ( eV for silicon).