By Vivek Patel
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R. (1979) Preliminary organic geochemical studies of samples from the Niger Delta (Nigeria). Analyses of crude oils for triterpanes. , Huizinga, B. , (1994) The molecular fossil re‐ cord of oleanane and its relation to angiosperms. Science 265, 768-771. , Dessort, T. D. and Albrecht, P. (1986) The microbial input in carbonate anhydrite facies of sabkha environment from Guatemala; A molecular approach In : Leythaeuser, D. and Rullkotter, J. ) Advances in Organic Geo‐ chemistry, 1985. Oxford-Pergamon, 20-50.
Tetracyano-metallates and hexacyano-metallates (Prussian blue analogues) are part of the materials with cyanide bridge group. Anion cyano (CN-) is a functional group with the ability to be simultaneously coordinated by both atoms at different cations. This makes it an excellent molecular block to generate different lattices structural at 1, 2, and 3 dimensions. The chemical bond in the cyanometallate in networks is the linear bridge M-CN-M; M = metal, with a distance M–M approximately 5 to 6 Å.
76%. According to Schoell  the natural_gas may be classified as wet if it exhibits a wetness index greater than 5%. The natural gas samples examined from the western Nile Delta can therefore be classified as wet gas, while the major number of gas samples from the eastern Nile Delta is classified as dry gas except the samples produced from the two wells PSE-1and DEN-1. Wet gas is thermogenic in origin but associated with condensate in most cases while the dry gas may have either a microbial or late mature thermal origin  or may be related to that microbial alteration occurring within the reservoirs through the preferential removal of the C3+ components .
Advances in Petrochemicals by Vivek Patel