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In focus: Sulphur |
| Chemical Composition: S | |
| Group: Native element | |
| Colour: Yellow, Orange, White | |
| Streak: none | |
| Hardness: 1.5-2.5 | |
| Density: 2-2.1 | |
| Luster: Resinous | |
| Cleavage: Imperfect |
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Sulphur (S) is a soft, bright yellow element which is solid at room temperature and which occurs naturally. Sulphur (from Latin sulfur or sulpur) was known in ancient times but the name itself is probably from the Arabic sufra, meaning 'yellow'. Until the late 18th century sulphur was thought to be a compound. It was only in the late 1770s that the scientist Antoine Lavoisier managed to convince the chemists of his day that it was in fact an element. |
Although not a compound, Sulphur could certainly deserve to be put in this section simply because its many interesting properties and economic importance are as great as any conmpound. One of these properties is its complex crystal structure. Depending on the specific conditions and the sulphur allotropes (different forms of the same element in the same physical state) sulphur can form several different structures. Rombic and monoclinic are the most common crystal structures of allotrope S8. But sulphur has many allotropes besides S8. For example, it can exist as S7 (where it loses the characteristic yellow colour), S12 or S18. At high temperature sulphur produces long polymer chains which are responsible for its high viscosity.
In its natural form, sulphur can be found near hot springs and in volcanic regions. Large sulphur deposits are found along the Pacific's 'Ring of Fire'. There are currently sulphur mines in Indonesia, Chile and Japan. Sicily (Italy) is also a large producer of naturally occuring sulphur. Large deposits of natural sulphur also exist in other parts of Europe and Asia. These are predominantly in the form of evaporates (material precipitated by evaporation). Evaporates are believed to come from either sulphate minerals, particularly from gypsum or precipitated by the action of anaerobic bacteria. Fossil-based sulphur deposits are the basis of commercially produced sulphur in number of countries including Poland, Russia and the United States.
Sulphur combines with many minerals to create a large number of naturally occurring sulphur compounds. These include the above-mentioned gypsum (calcium sulphate), pyrite (iron sulphate), galena (lead sulphate), barite (barium sulphate) just to mention a few. Sulphur also readily associates with gasses. When burned, sulphur combines with oxygen to give rise to sulphur dioxide. Further oxidation will lead to the production of sulphur trioxide which when combined with water produces sulphuric acid (H2SO4). The latter compound is largely responsible for sulphur being one of the most important raw materials in industry.
The use of sulphur and sulphur compounds is so widespread in the modern world that it is impossible to list all the uses in that section.
At room temperature, sulphur is a soft, bright yellow material. It has only a faint odour similar to that of matches. Sulphur is insoluble in water but soluble in carbon disulphide and to a lesser extent in other organic solvents such as benzene and toluene. It burns with a blue flame that emits sulphur dioxide, notable for its peculiar suffocating odour. A noteworthy property of sulphur is its viscosity in its molten state. Unlike most other liquids, temperature increases to above 200oC lead to the formation of polymer chains. The molten sulphur also becomes dark red above this temperature. However, after a specific temperature is reached, the viscosity is reduced because there is enough energy to break the chains.
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