The periodic table is one of those classic images that you find in many science labs and classrooms. It’s an image almost everyone has seen at some time in their life.
You can also find the periodic table on t-shirts, mugs, beach towels, pillowcases and duvet covers, and plenty of other items. It even inspired a collection of short stories.
Who can forget the periodic table put to music by the American Tom Lehrer, a Harvard mathematics professor who was also a singer/songwriter and satirist. His song, The Elements, includes all the elements that were known at the time of writing in 1959.
Since then, several new elements have been added to the periodic table, including the four that were formally approved last year by the International Union of Pure and Applied Chemistry (IUPAC).
But what exactly does the periodic table show?
In brief, it is an attempt to organise the collection of the elements – all of the known pure compounds made from a single type of atom.
There are two ways to look at how the periodic table is constructed, based on either the observed properties of the elements contained within it, or on the subatomic construction of the atoms that form each element.
The elements
When scientists began collecting elements in the 1700s and 1800s, slowly identifying new ones over decades of research, they began to notice patterns and similarities in their physical properties. Some were gases, some were shiny metals, some reacted violently with water, and so on.
At the time when elements were first being discovered, the structure of atoms was not known. Scientists began to look at ways to arrange them systematically so that similar properties could be grouped together, just as someone collecting seashells might try to organise them by shape or colour.
The task was made more difficult because not all of the elements were known. This left gaps, which made deciphering patterns a bit like trying to assemble a jigsaw puzzle with missing pieces.
Different scientists came up with different types of tables. The first version of the current table is generally attributed to Russian chemistry professor Dmitri Mendeleev in 1869, with an updated version in 1871.
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