Carbon
Carbon was known in prehistory in the form of soot; while charcoal was made in Roman times (by heating wood while exclude air) and diamonds were known as early as 2500 BC in China. In 1772, Antoine Lavoisier (Figure 1) showed that diamonds were a form of carbon, when he burned samples of carbon and diamond and showed that both formed the same amount of carbon dioxide per gram of material. Carl Scheele (Figure 2) showed that graphite was a form of carbon rather a form of lead.
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A new allotrope of carbon, fullerene, was discovered in 1985 by Robert Curl, Harry Kroto, and Richard Smalley (Figure 3) who subsequently shared the Nobel Prize in Chemistry in 1996. Fullerenes have been reveled to include nanostructured forms such as buckyballs and nanotubes. The renewed interest in new forms lead to the discovery of further exotic allotropes, including glassy carbon, and the realization that amorphous carbon is not amorphous.
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Silicon
Silicon was first identified by Antoine Lavoisier (Figure 1) in 1787 as a component of flints, and was later mistaken by Humphry Davy (Figure 4) for a compound rather than an element. In 1824, Berzelius (Figure 5) prepared amorphous silicon by the reaction of potassium with silicon tetrafluoride, Equation 1
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Germanium
In 1869 Dmitri Mendeleev (Figure 6) predicted the existence of several unknown elements, including ekasilicon (Es) between silicon and tin.
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In 1885 a new mineral (named argyrodite because of its high silver content) was found in a mine near Freiberg, Saxony. Clemens Winkler (Figure 7) isolated Mendeleev’s missing element. He originally was going to name neptunium because like this element, because like ekasilicon, the planet Neptune had been preceded by mathematical prediction of its existence. However, the name neptunium had already been given to an element and so Winkler named the new metal germanium in honor of his fatherland.
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Winkler was able to isolate sufficient germanium from 500 kg of ore to determine a number properties, including an atomic weight of 72.32 g/mol by analyzing pure germanium tetrachloride (GeCl4). Winkler prepared several new compounds of germanium, including the fluorides, chlorides, sulfides, germanium dioxide, and tetraethylgermane (Ge(C2H5)4). The physical data from these compounds, corresponded with Mendeleev's predictions (Table 2).
| Property | Ekasilicon | Germanium |
| Atomic mass | 72 | 72.59 |
| Density (g/cm3) | 5.5 | 5.35 |
| Melting point (°C) | High | 947 |
| Color | Gray | Gray |
| Oxide type | Refractory dioxide | Refractory dioxide |
| Oxide density (g/cm3) | 4.7 | 4.7 |
| Oxide activity | Feebly basic | Feebly basic |
| Chloride boiling point (°C) | Under 100 | 86 (GeCl4) |
| Chloride density (g/cm3) | 1.9 | 1.9 |
Tin
Tin is one of the earliest metals known. When the addition of about 5% tim to molten copper produced an alloy (bronze) that was easier to work and much harder than copper, it revolutionized civilization. The widespread use of bronze to make tools and weapons became part of what archaeologists call the Bronze Age. The Bronze Age arrived in Egypt, Mesopotamia and the Indus Valley culture by around 3000 BC.
Lead
Lead has been commonly used for thousands of years because of its ease of extraction, and its ease of smelting. Lead beads dating back to 6400 BC have been found in Çatalhöyük in modern-day Turkey, while lead was used during the Bronze Age.


























