A diamondoid, in the context of building materials for nanotechnology components, most generally refers to structures that resemble diamond in a broad sense: namely, strong, stiff structures containing dense, 3-D networks of covalent bonds, formed chiefly from first and second row atoms with a valence of three or more. Examples of diamondoid structures would include crystalline diamond, sapphire, and other stiff structures similar to diamond but with various atom substitutions which might include N, O, Si, S, and so forth. Sp²-hybridized carbon structures that – in contrast to sp³-hybridized carbon in diamond – arrange in planar sheets ("graphene" sheets) are sometimes also included in the class of diamondoid materials for nanotechnology, e.g., graphite, carbon nanotubes consisting of sheets of carbon atoms rolled into tubes, spherical buckminsterfullerenes and other graphene structures.
In the context of classical chemistry, "diamondoid" refers to variants of the carbon cage molecule known as adamantane (C10H16), the smallest unit cage structure of the diamond crystal lattice. Diamondoids also known as nanodiamonds or condensed adamantanes may include one or more cages (adamantane, diamantane, triamantane, and higher polymantanes) as well as numerous isomeric and structural variants of adamantanes and polymantanes. These diamondoids occur naturally in petroleum deposits and have been extracted and purified into large pure crystals of polymantane molecules having more than a dozen adamantane cages per molecule. These species are of interest as molecular approximations of the cubic diamond framework, terminated with C-H bonds. Cyclohexamantane may be thought of as a nanometer-sized diamond of approximately 5.6 * 10−22 grams.
- Adamantane (C10H16)
- Iceane (C12H18)
- BC-8 (C14H20)
- Diamantane (C14H20) also diadamantane, two face-fused cages
- Triamantane (C18H24), also triadamantane. Diamantane has 4 identical faces available for anchoring a new C4H4 unit.
- Isotetramantane (C22H28). Triamantane has 8 faces on to which a new C4H4 unit can be added resulting in 4 isomers. One of these isomers displays a helical twist and is therefore prochiral. The P and M enantiomers have been separated.
- Pentamantane has 9 isomers with chemical formula C26H32 and one more pentamantane exists with chemical formula C25H30
- Cyclohexamantane (C26H30)
- Super-adamantane (C30H36)
- Basic beryllium acetate Be4O(O2CCH3)6
One tetramantane isomer is the largest ever diamondoid prepared by organic synthesis using a keto-carbenoid reaction to attach cyclopentane rings. Longer diamondoids have been formed from diamantane dicarboxylic acid. The first ever isolation of a wide range of diamondoids from petroleum took place in the following steps: a vacuum distillation above 345 °C, the equivalent atmospheric boiling point, then pyrolysis at 400 to 450 °C in order to remove all non-diamondoid compounds and then a series of HPLC separation techniques.
In one study a tetramantane compound is fitted with thiol groups at the bridgehead positions. This allows their anchorage to a gold surface and formation of self-assembled monolayers (diamond-on-gold).
Organic chemistry of diamondoids even extends to pentamantane. The medial position (base) in this molecule (the isomer [1(2,3)4]pentamantane) is calculated to yield a more favorable carbocation than the apical position (top) and simple bromination of pentamane 1 with bromine exclusively gives the medial bromo derivative 2 which on hydrolysis in water / DMF forms the alcohol 3.
In contrast nitroxylation of 1 with nitric acid gives the apical nitrate 4 as an intermediate which is hydrolyzed to the apical alcohol 5 due to the higher steric demand of the active electrophilic NO2 - HNO3+ species. This alcohol can react with thionyl bromide to the bromide 6 and in a series of steps (not shown) to the corresponding thiol. Pentamantane can also react with tetrabromomethane and tetra-n-butylammonium Bromide (TBABr) in a free radical reaction to the bromide but without selectivity.
Origin and occurrence of diamondoids
Diamondoids are found in mature high-temperature petroleum fluids (volatile oils, condensates and wet gases). These fluids can have up to a spoonful of diamondoids per gallon (about 3.78 liters). A review by Mello and Moldowan in 2005 showed that although the carbon in diamonds is not biological in origin, the diamondoids found in petroleum are composed of carbon from biological sources. This was determined by comparing the ratios of carbon isotopes present.
Optical and electronic properties
The optical absorption for all diamondoids lies deep in the UV spectral region with optical band gaps around 6 eV and higher. The spectrum of each diamondoid is found to reflect its individual size, shape and symmetry. Due to their well defined size and structure diamondoids also serve as a model system for electronic structure calculations. Many of the optoelectronic properties of diamondoids are determined by the difference in the nature of the highest occupied and lowest unoccupied molecular orbitals: the former is a bulk state, whereas the latter is a surface state. As a result, the energy of the lowest unoccupied molecular orbital is roughly independent of the size of the diamondoid. 
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