LESSON 1.3CHEMISTRY I: GENERAL CHEMISTRY

ELEMENTS & THE PERIODIC TABLE

Every atom in the universe belongs to one of 118 known elements — and the periodic table is the map that organises them all.

At this point we have mentioned the concept of an element a few times — but what exactly is one? Think of elements like scents of flowers or flavours of ice cream: each one is distinct, with its own unique characteristics and chemically different behaviour. No two elements are the same, and you cannot reduce one into another by ordinary means.

As we touched on in the last lesson, an element is defined entirely by the number of protons in an atom's nucleus — a value known as its atomic number. Change the proton count and you change the element. Every single atom in the universe with one proton is hydrogen. Every atom with two protons is helium. It is that simple, and that absolute.

The first few elements follow in order:

1HHydrogen
2HeHelium
3LiLithium
4BeBeryllium
5BBoron
6CCarbon
7NNitrogen
8OOxygen
9FFluorine
10NeNeon
and so on, up to element 118

This numbered sequence — one element per proton count, no gaps, no duplicates — is the backbone of the periodic table. There are 118 known elements in total, ranging from hydrogen, the lightest and most abundant in the universe, all the way to oganesson, a synthetic element so unstable it exists for only milliseconds before decaying.

// INTERACTIVE — PERIODIC TABLE OF ELEMENTS

ALKALI METAL
ALKALINE EARTH METAL
TRANSITION METAL
POST-TRANSITION METAL
METALLOID
NONMETAL
HALOGEN
NOBLE GAS
LANTHANIDE
ACTINIDE
1H1.008
2He4.003
3Li6.941
4Be9.012
5B10.811
6C12.011
7N14.007
8O15.999
9F18.998
10Ne20.180
11Na22.990
12Mg24.305
13Al26.982
14Si28.086
15P30.974
16S32.065
17Cl35.453
18Ar39.948
19K39.098
20Ca40.078
21Sc44.956
22Ti47.867
23V50.942
24Cr51.996
25Mn54.938
26Fe55.845
27Co58.933
28Ni58.693
29Cu63.546
30Zn65.380
31Ga69.723
32Ge72.630
33As74.922
34Se78.971
35Br79.904
36Kr83.798
37Rb85.468
38Sr87.620
39Y88.906
40Zr91.224
41Nb92.906
42Mo95.960
43Tc97.000
44Ru101.07
45Rh102.91
46Pd106.42
47Ag107.87
48Cd112.41
49In114.82
50Sn118.71
51Sb121.76
52Te127.60
53I126.90
54Xe131.29
55Cs132.91
56Ba137.33
57La138.91
58Ce140.12
59Pr140.91
60Nd144.24
61Pm145.00
62Sm150.36
63Eu151.96
64Gd157.25
65Tb158.93
66Dy162.50
67Ho164.93
68Er167.26
69Tm168.93
70Yb173.05
71Lu174.97
72Hf178.49
73Ta180.95
74W183.84
75Re186.21
76Os190.23
77Ir192.22
78Pt195.08
79Au196.97
80Hg200.59
81Tl204.38
82Pb207.20
83Bi208.98
84Po209.00
85At210.00
86Rn222.00
87Fr223.00
88Ra226.00
89Ac227.00
90Th232.04
91Pa231.04
92U238.03
93Np237.00
94Pu244.00
95Am243.00
96Cm247.00
97Bk247.00
98Cf251.00
99Es252.00
100Fm257.00
101Md258.00
102No259.00
103Lr266.00
104Rf267.00
105Db268.00
106Sg271.00
107Bh272.00
108Hs270.00
109Mt278.00
110Ds281.00
111Rg282.00
112Cn285.00
113Nh286.00
114Fl289.00
115Mc290.00
116Lv293.00
117Ts294.00
118Og294.00
57–71
89–103
HOVER AN ELEMENT
TO VIEW ITS ATOM

HOW TO READ A CELL

Each cell in the periodic table packs three key pieces of information. The number in the top corner is the atomic number — the count of protons in that element's nucleus, and the value that uniquely identifies it. The large symbol in the centre is the element's chemical abbreviation, used universally in equations, labels, and lab notation. Finally, the number at the bottom is the atomic mass — the average mass of one atom of that element measured in atomic mass units (u), accounting for the natural mix of its isotopes.

// INTERACTIVE — ANATOMY OF A PERIODIC TABLE CELL

3
Li
6.941
← HOVER FOR EXPLAINER

That atomic mass is not arbitrary — it is the weighted average of all naturally occurring isotopes of that element, weighted by how abundant each isotope is in nature. Because different samples of an element always contain isotopes in the same natural ratio, the weighted average is consistent everywhere on Earth — and is the number printed on every periodic table.

Lithium is a clean example. It has two stable isotopes: lithium-6 (3 neutrons) and lithium-7 (4 neutrons). In any natural sample, about 7.6% of lithium atoms are Li-6 and 92.4% are Li-7. To find the weighted average you multiply each isotope's exact mass by its fractional abundance, then add the results:

Li-66.0151 u×0.076=0.4572 u
Li-77.0160 u×0.924=6.4828 u
SUM =6.9400 u ≈ 6.941 u

The result matches what is printed on the periodic table. Notice that 6.941 is close to 7 rather than 6 because the heavier Li-7 isotope makes up the vast majority of natural lithium. This is why atomic masses are almost never whole numbers — they are averages, not counts.

A word of warning: the abbreviations do not always match the English name of the element. Many symbols come from older Latin or Greek names that were established before modern naming conventions existed. A few notable examples:

PbLeadPlumbum
AuGoldAurum
FeIronFerrum
NaSodiumNatrium
KPotassiumKalium
AgSilverArgentum
HgMercuryHydrargyrum
CuCopperCuprum

These mismatches are a quirk of scientific history — names were often standardised in Latin across Europe before English became dominant in science. Once you know the common ones, they become second nature. For now, hover over any cell above to explore the full details of each element.

HOW THE TABLE IS ORGANISED

At first glance the layout of the periodic table can look arbitrary — rows of varying length, a detached block floating beneath the main grid, columns that seem to start and stop at random. In reality every position is deeply intentional.

Each vertical column is called a group, and the elements within a group share remarkably similar chemical behaviour. They react with other substances in the same kinds of ways, form the same types of bonds, and often even look alike as pure materials. This is no coincidence — it is a direct consequence of how many electrons sit in each element's outermost orbital shell. Elements in the same group have the same number of outer electrons, and it is those outer electrons that determine almost everything about how an atom behaves chemically. The horizontal rows, called periods, represent the filling of successive electron shells as the atomic number increases.

A handful of groups are important enough to have their own names that you will encounter constantly in chemistry. Here are the key ones:

GROUPNAMEEXAMPLES
1Alkali MetalsLithium (Li), Sodium (Na), Potassium (K)
Highly reactive metals — they explode in water.
2Alkaline Earth MetalsMagnesium (Mg), Calcium (Ca)
Reactive metals, but less so than Group 1.
17HalogensFluorine (F), Chlorine (Cl), Iodine (I)
Highly reactive nonmetals — one electron away from a full shell.
18Noble GasesHelium (He), Neon (Ne), Argon (Ar)
Completely unreactive — their outermost shell is already full.

Notice that noble gases sit at the far right of every period — they are the endpoint of each row, with completely filled outer shells and no tendency to react. This pattern of shell-filling is what gives the periodic table its shape, and understanding it is the key to predicting how any element will behave. We will explore groups, periods, and electron configuration in much greater depth in future lessons.

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