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---
title: The Periodic Table
subtitle: 118 elements, one organising principle
author: md2any examples
date: auto
theme: light
aspect: 16:9
layout: clean
toc: true
---

# Why the table looks the way it does

## Mendeleev's gamble

Dmitri Mendeleev published the first recognisable periodic table in 1869. He had 63 known elements, ordered by **atomic mass**, arranged so that elements with similar chemistry sat in the same column.

His move was the gaps. Mendeleev left empty slots and **predicted** the properties of the missing elements — including atomic mass, density, and reactivity. Eka-aluminium (gallium, discovered 1875), eka-boron (scandium, 1879) and eka-silicon (germanium, 1886) all turned up with properties within a few percent of his predictions.

The table got refined twice afterwards:

- 1913: Henry Moseley showed the right ordering is **atomic number** ($Z$), not atomic mass. Fixed a handful of out-of-order pairs (Ar/K, Co/Ni, Te/I).
- 1944: Glenn Seaborg moved the actinides into their own row below the lanthanides, giving the table its modern shape.

## What "periodic" means

Properties repeat at regular intervals along the rows because electrons fill orbitals in a predictable order. The "period" is how long each row is — and the row lengths reflect the size of each new electron shell:

| Period | Length | Why                                  |
|-------:|-------:|--------------------------------------|
| 1      | 2      | 1s only                              |
| 2      | 8      | 2s + 2p (2 + 6)                      |
| 3      | 8      | 3s + 3p                              |
| 4      | 18     | 4s + 3d + 4p (2 + 10 + 6)            |
| 5      | 18     | 5s + 4d + 5p                         |
| 6      | 32     | 6s + 4f + 5d + 6p (2 + 14 + 10 + 6)  |
| 7      | 32     | 7s + 5f + 6d + 7p                    |

The "f-block" elements (lanthanides + actinides) get pulled out below the main table to keep the layout printable. They're really part of periods 6 and 7.

# The 18 groups

## Reading the columns

Elements in the same column share their **outermost electron configuration** and therefore most of their chemistry.

| Group | Name                | Outer shell | Examples           |
|-------|---------------------|-------------|--------------------|
| 1     | Alkali metals       || Li, Na, K, Rb, Cs  |
| 2     | Alkaline earth      || Be, Mg, Ca, Sr, Ba |
| 3-12  | Transition metals   | (n−1)d, ns  | Fe, Cu, Ag, Au, Pt |
| 13    | Boron group         || B, Al, Ga          |
| 14    | Carbon group        || C, Si, Ge, Sn      |
| 15    | Pnictogens          || N, P, As, Sb       |
| 16    | Chalcogens          | p⁴          | O, S, Se, Te       |
| 17    | Halogens            | p⁵          | F, Cl, Br, I       |
| 18    | Noble gases         | p⁶ (full)   | He, Ne, Ar, Kr     |

The noble gases have full outer shells — chemically inert under most conditions. The alkali metals are one electron *over* a full shell — desperate to give it away — which makes them the most reactive metals. Halogens are one electron *short* — equally desperate to take one — which makes them the most reactive non-metals.

# Period 1 and 2 (the small ones)

## Hydrogen and helium

| Z | Symbol | Name      | Atomic mass | Notable                                |
|---|--------|-----------|-------------|----------------------------------------|
| 1 | H      | Hydrogen  | 1.008       | Most abundant element in the universe (≈75% by mass) |
| 2 | He     | Helium    | 4.003       | Second most abundant; second highest ionisation energy |

Hydrogen sits on the table awkwardly — it has 1 electron like the alkali metals (group 1), but its chemistry is more like the halogens (group 17). Different tables put it in different places.

## Period 2: the building blocks of life

| Z  | Sym | Name      | Mass    | Found in                              |
|----|-----|-----------|---------|---------------------------------------|
| 3  | Li  | Lithium   | 6.94    | Mood stabilisers, EV batteries        |
| 4  | Be  | Beryllium | 9.012   | Aerospace alloys; toxic dust          |
| 5  | B   | Boron     | 10.81   | Borosilicate glass, neutron absorbers |
| 6  | C   | Carbon    | 12.011  | Every organic molecule                |
| 7  | N   | Nitrogen  | 14.007  | 78% of Earth's atmosphere             |
| 8  | O   | Oxygen    | 15.999  | 21% of atmosphere; most abundant in Earth's crust |
| 9  | F   | Fluorine  | 18.998  | Toothpaste; the most reactive non-metal |
| 10 | Ne  | Neon      | 20.180  | Signs that say OPEN                   |

Carbon, hydrogen, nitrogen and oxygen account for ~96% of human body mass. The chemistry of life is mostly the chemistry of the second row.

# Period 3 and 4 (the workhorses)

## Period 3

| Z  | Sym | Name       | Mass    | Notable                                |
|----|-----|------------|---------|----------------------------------------|
| 11 | Na  | Sodium     | 22.990  | Half of table salt                     |
| 12 | Mg  | Magnesium  | 24.305  | Chlorophyll's central atom             |
| 13 | Al  | Aluminium  | 26.982  | Most abundant metal in Earth's crust   |
| 14 | Si  | Silicon    | 28.085  | Second most abundant in crust; semiconductors |
| 15 | P   | Phosphorus | 30.974  | DNA backbone; matches                  |
| 16 | S   | Sulfur     | 32.06   | Vulcanised rubber; smell of struck matches |
| 17 | Cl  | Chlorine   | 35.45   | The other half of table salt; pool sanitiser |
| 18 | Ar  | Argon      | 39.948  | 1% of atmosphere; welding shield gas   |

## Period 4 (highlights)

The first row with transition metals. 18 elements; here are the famous ones:

| Z  | Sym | Name      | Mass    | Notable                                  |
|----|-----|-----------|---------|------------------------------------------|
| 19 | K   | Potassium | 39.098  | Bananas; nerve impulse pumps             |
| 20 | Ca  | Calcium   | 40.078  | Bones, teeth, intracellular signalling   |
| 22 | Ti  | Titanium  | 47.867  | Aerospace; medical implants              |
| 24 | Cr  | Chromium  | 51.996  | Stainless steel; emerald colour          |
| 26 | Fe  | Iron      | 55.845  | Haemoglobin; structural alloys           |
| 27 | Co  | Cobalt    | 58.933  | Battery cathodes; vitamin B₁₂           |
| 28 | Ni  | Nickel    | 58.693  | Stainless steel; coinage                 |
| 29 | Cu  | Copper    | 63.546  | Electrical wiring; brass and bronze      |
| 30 | Zn  | Zinc      | 65.38   | Brass; immune function                   |
| 33 | As  | Arsenic   | 74.922  | Semiconductors; historically a poison    |
| 35 | Br  | Bromine   | 79.904  | Flame retardants; one of two liquid elements at room temp |
| 36 | Kr  | Krypton   | 83.798  | Defined the metre, 1960-1983             |

# The transition-metal jewels

## Where we get our coinage and catalysts

The 10-element-wide transition-metal block contains most metals familiar from everyday objects, currency, and chemistry catalysts.

| Z  | Sym | Name       | Mass    | Notable                                 |
|----|-----|------------|---------|-----------------------------------------|
| 42 | Mo  | Molybdenum | 95.95   | Steel alloying; nitrogen fixation enzymes |
| 44 | Ru  | Ruthenium  | 101.07  | Pen nibs; catalysis                     |
| 45 | Rh  | Rhodium    | 102.906 | Catalytic converters; most expensive precious metal as of 2023 |
| 46 | Pd  | Palladium  | 106.42  | Catalytic converters; hydrogen storage  |
| 47 | Ag  | Silver     | 107.868 | Coinage; antimicrobial; best electrical conductor |
| 74 | W   | Tungsten   | 183.84  | Highest melting point of any element (3422°C); incandescent filaments |
| 76 | Os  | Osmium     | 190.23  | Densest naturally occurring element (22.59 g/cm³) |
| 77 | Ir  | Iridium    | 192.217 | Second-densest; Cretaceous-Paleogene boundary layer marker for the asteroid impact |
| 78 | Pt  | Platinum   | 195.084 | Catalysis; jewellery; defined the kilogram 1889-2019 |
| 79 | Au  | Gold       | 196.967 | Jewellery; reserve currency; electronics contacts |
| 80 | Hg  | Mercury    | 200.59  | Only metal liquid at room temperature; thermometers; toxic |

# Lanthanides and actinides

## The "f-block"

These 30 elements (atomic numbers 57-71 and 89-103) get displayed below the main table so the layout fits on a page. Chemically they're remarkable: the lanthanides ("rare earths") are essential to almost every modern electronic device.

| Z  | Sym | Name        | Modern use                                        |
|----|-----|-------------|---------------------------------------------------|
| 57 | La  | Lanthanum   | Camera lenses; battery electrodes                 |
| 58 | Ce  | Cerium      | Catalytic converters; glass polishing             |
| 59 | Pr  | Praseodymium| Magnets; aircraft engine alloys                   |
| 60 | Nd  | Neodymium   | The strongest permanent magnets ever made         |
| 62 | Sm  | Samarium    | High-temperature magnets                          |
| 63 | Eu  | Europium    | Red and blue phosphors in OLED displays           |
| 64 | Gd  | Gadolinium  | MRI contrast agents                               |
| 66 | Dy  | Dysprosium  | EV motor magnets                                  |
| 67 | Ho  | Holmium     | Strongest magnetic moment of any element          |
| 68 | Er  | Erbium      | Fibre-optic amplifiers                            |
| 70 | Yb  | Ytterbium   | Atomic clocks                                     |

Despite the name, rare-earth elements aren't actually rare in the crust — they're just rarely concentrated in mineable deposits, and their chemistries are so similar that separation is the expensive step.

## The actinides

Atomic numbers 89-103. Only thorium (90) and uranium (92) occur in nature in meaningful quantities; everything else is synthesised in reactors or accelerators.

| Z  | Sym | Name        | Half-life of most stable isotope |
|----|-----|-------------|----------------------------------|
| 90 | Th  | Thorium     | 14 billion years (Th-232)        |
| 92 | U   | Uranium     | 4.5 billion years (U-238)        |
| 93 | Np  | Neptunium   | 2.1 million years (Np-237)       |
| 94 | Pu  | Plutonium   | 80 million years (Pu-244)        |
| 95 | Am  | Americium   | 7,370 years (Am-243); in smoke detectors |
| 96 | Cm  | Curium      | 16 million years (Cm-247)        |
| 98 | Cf  | Californium | 898 years (Cf-251)               |
| 99 | Es  | Einsteinium | 472 days (Es-252)                |
| 102| No  | Nobelium    | 58 minutes (No-259)              |
| 103| Lr  | Lawrencium  | 11 hours (Lr-266)                |

# Synthesised elements

## Beyond uranium

Every element with $Z > 92$ has been made in a particle accelerator. The first transuranium element was neptunium in 1940 (Berkeley). The most recent additions completed period 7 in 2016:

| Z   | Sym | Name          | Synthesised | Half-life of best isotope |
|-----|-----|---------------|-------------|---------------------------|
| 113 | Nh  | Nihonium      | 2003 (RIKEN)| ~10 seconds (Nh-286)      |
| 114 | Fl  | Flerovium     | 1999 (JINR/LLNL)| ~2.6 seconds (Fl-289)  |
| 115 | Mc  | Moscovium     | 2003 (JINR/LLNL)| ~0.65 seconds          |
| 116 | Lv  | Livermorium   | 2000 (JINR/LLNL)| ~60 milliseconds       |
| 117 | Ts  | Tennessine    | 2010 (JINR/ORNL)| ~80 milliseconds       |
| 118 | Og  | Oganesson     | 2002 (JINR/LLNL)| ~0.7 milliseconds      |

Oganesson is the heaviest element produced to date and the only synthetic element named after a living person (Yuri Oganessian) at the time of its naming.

The hunt for the **island of stability** — a predicted region around $Z = 114-126$ where superheavy nuclei should be unusually long-lived — continues.

# Trends across the table

## Atomic radius

Atoms get **smaller** moving left-to-right across a period (more protons pulling the same shell closer) and **larger** moving top-to-bottom down a group (each new period adds a shell).

$$r_{\text{Cs}} \approx 260\ \text{pm} \quad \gg \quad r_{\text{He}} \approx 31\ \text{pm}$$

Caesium is roughly 8× the diameter of helium. The largest stable atom vs. the smallest.

## Ionisation energy

Energy needed to remove the outermost electron. **Opposite trend**: smaller, tighter atoms hold their electrons more strongly.

| Element  | First ionisation energy (kJ/mol) |
|----------|---------------------------------:|
| Cs       | 376                              |
| K        | 419                              |
| Na       | 496                              |
| Mg       | 738                              |
| H        | 1312                             |
| F        | 1681                             |
| He       | 2372                             |

Helium is the hardest atom to ionise. The alkali metals are the easiest — which is why they react explosively with water (the water happily takes the loose electron).

## Electronegativity (Pauling scale)

How strongly an atom pulls electrons toward itself in a bond. Linus Pauling's 1932 scale runs from 0.7 (caesium) to 3.98 (fluorine).

| F   | O   | N   | Cl  | C   | H   | Na  | Cs  |
|-----|-----|-----|-----|-----|-----|-----|-----|
| 3.98| 3.44| 3.04| 3.16| 2.55| 2.20| 0.93| 0.79|

The electronegativity *difference* between two bonded atoms predicts bond type:

- $\Delta\chi < 0.5$ → non-polar covalent (C-H, C-C)
- $0.5 \leq \Delta\chi < 1.7$ → polar covalent (H-O, H-N)
- $\Delta\chi \geq 1.7$ → ionic (Na-Cl is 2.23)

# Isotopes and abundance

## Same element, different mass

Atoms of one element can have different numbers of neutrons. The element is fixed by proton count; the isotope by total nucleon count.

| Element  | Isotopes (stable + notable radio) | Notable                          |
|----------|------------------------------------|----------------------------------|
| Hydrogen | ¹H (99.98%), ²H deuterium, ³H tritium | Deuterium in heavy water       |
| Carbon   | ¹²C (98.9%), ¹³C, ¹⁴C            | ¹⁴C dating (half-life 5730 y)    |
| Oxygen   | ¹⁶O, ¹⁷O, ¹⁸O                    | ¹⁸O/¹⁶O ratio reconstructs paleoclimate |
| Uranium  | ²³⁸U (99.27%), ²³⁵U (0.72%)       | ²³⁵U is the fissile one          |

The "atomic mass" on a periodic table is the weighted average of natural isotope abundances. That's why hydrogen reads 1.008 (mostly ¹H but with some ²H) rather than exactly 1.

## Elements in the universe

The Big Bang made hydrogen, helium, and trace lithium. Stars made everything up to iron via fusion. Supernovae and neutron-star mergers made everything heavier.

| Element  | Solar-system abundance (atoms, log scale) |
|----------|-------------------------------------------|
| H        | 10¹²                                      |
| He       | 10¹¹                                      |
| C        | 8.4 × 10⁸                                |
| O        | 6.8 × 10⁸                                |
| Fe       | 3.2 × 10⁷                                |
| Au       | 1.0                                       |

Carl Sagan: "The nitrogen in our DNA, the calcium in our teeth, the iron in our blood — were all made in the interiors of collapsing stars. We are made of star-stuff."

# What md2any showed off in this deck

## Feature index

- **Tables, tables, tables** — 14 of them, ranging from 3 columns to 6, with right-aligned numerics, mixed text + scientific notation, and back-to-back layouts
- **Unicode coverage** — element symbols (Th, U), Greek symbols ($\Delta\chi$), superscripts (¹²C, ²³⁸U), subscripts (B₁₂), degree sign (°C)
- **Math** — inline ($r_{\text{Cs}} \approx 260$ pm) and display ($\Delta\chi$ thresholds)
- **Block quotes** with attribution (Sagan)
- **Comparison rows** with $\gg$ relations
- **Front-matter TOC** auto-generates the contents slide

All facts are textbook periodic-table data. Sources: Royal Society of Chemistry periodic table; NIST atomic weights; IUPAC element discovery summaries.