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Friday 5 April 2013

Elements

The philosophers' elements

The four elements of Western alchemy

The figure (source) shows how the four elements were imagined to combine in various pairs to produce the "qualities" of hot, cold, wetness and dryness.
See this Wikipedia article for a good survey of the classical elements in various cultures.
The concept of the element is an ancient one which developed in many different civilizations in an attempt to rationalize the variety of the world and to understand the nature of change, such as that which occurs when a piece of wood rots, or is burnt to produce charcoal or ash. Most well known to us are the four elements "earth, air, fire and water" that were popularized by Greek philosophers (principally Empedocoles and Aristotle) in the period 500-400 BCE.
To these, Vedic (Hindu) philosophers of India added space, while the ancient Chinese concept of Wu Xing regarded earth, metal, wood, fire and water as fundamental. These basic elements were not generally considered to exist as the actual materials we know as earth, water, etc., but rather to represent the "principles" or essences that the elements conveyed to the various kinds of matter we encounter in the world.

The chemists' elements

Eventually, practical experience (largely connected with the extraction of metals from ores) and the beginnings of scientific experimentation in the 18th Century led to our modern concept of the chemical element.
An element is a substance: the simplest form to which any other chemical substance can be reduced through appropriate thermal or chemical treatment.
"Simplest", in the context of experimentation at the time, was defined in terms of weight; cinnabar (mercuric sulfide) can be broken down into two substances, mercury and sulfur, which themselves cannot be reduced to any lighter forms. The first textbook of Chemistry, Traitè Èlèmentaire de Chemie, published by Antoine Lavoisier ("the father of Chemistry") in 1789, contained the table of elements shown here.
Antoine Lavoisier (1743-1794)
Although old Antoine got many of these right, he did manage to include a few things that don't quite fit into our modern idea of what constitutes a chemical element. There are two such mistakes in the top section of the table that you should be able to identify even if your French is less than tip-top— can you find them?
Lav's other mis-assignment of the elements in the bottom section was not really his fault. Chalk, magnesia, barytes, alumina and silica are highly stable oxygen-containing compounds; the high temperatures required to break them down could not be achieved in Lavoisier's time. (Magnesia, after all, is what fire brick is made of!) The proper classification of these substances was delayed until further experimentation revealed their true nature.
Ten of the chemical elements have been known since ancient times. Five more were discovered through the 17th Century.
Some interesting videos on basic atomic theory

Some frequently-asked questions about elements

How many elements are there?

Ninety-two elements have been found in nature. Around 25 more have been made artificially, but all of these decay into lighter elements, with some of them disappearing in minutes or even seconds.

Where do the elements come from?

The processes by which elements (or more properly, their nuclei) are formed is known as nucleosynthesis. The very first (primordial) nuclei formed shortly after the "big bang".
The present belief is that helium and a few other very light elements were formed within about three minutes of the "big bang", and that the next 23 elements (up through iron) are formed mostly by nuclear fusion processes within stars, in which lighter nuclei combine into successively heavier elements. Elements heavier than iron cannot be formed in this way, and are produced only during the catastrophic collapse of massive stars (supernovae explosions).

How do the elements vary in abundance?

Quite markedly, and very differently in different bodies in the cosmos. Most of the atoms in the universe still consist of hydrogen, with helium being a distant second. On Earth, oxygen, silicon, and aluminum are most abundant. These profiles serve as useful guides for constructing models for the formation of the earth and other planetary bodies.
Elemental abundances in the lithosphere (Earth's crust) and in the universe.
Note that the vertical axis is logarithmic, which has the effect of greatly reducing the visual impression of the differences between the various elements.

How did the elements get their names?

This is too big a subject to cover here in detail, especially since most elements have different names in different languages. Here are some useful links:

How did the element symbols originate?

The system of element symbols we use today was established by the Swedish chemist Jöns Jacob Berzelius in 1814. Prior to that time, graphic alchemical symbols were used, which were later modified and popularized by John Dalton (See here). Fortunately for English speakers, the symbols of most of the elements serve as mnemonics for their names, but this is not true for the seven metals known from antiquity, whose symbols are derived from their Latin names. The other exception is tungsten (a name derived from Swedish), whose symbol W reflects the German name which is more widely used.

How are the elements organized?

Two general organizing principles developed in the 19th Century: one was based on the increasing relative weights (atomic weights) of the elements, yielding a list that begins this way:
H  He  Li  Be  B  C  N  O  F  Ne  Na  Mg  Al  Si  P  S  Cl  Ar  K  Ca...
The other principle took note of the similarities of the properties of the elements, organizing them into groups with similar properties (Döbereiner's "triads", 1829). It was later noted that groups of elements (Chancourtois' "telluric helix", Newlands "octaves", 1864 and Meyer, 1869) having changing properties tended to repeat themselves within the atomic weight sequence, giving rise to the idea of "periodic" sequences of properties. These concepts were finally integrated into the periodic table published by Mendeleev in 1869, which evolved into the various forms of the periodic table in use today.

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