Sandstone Reservoirs Research Paper Example | Topics and Well Written Essays - 1250 words

Sandstone Reservoirs - Research Paper ExampleExamples of sandstone reservoirs are found in Western Canada Sedimentary Basin, coastal basins of Equatorial Africa, United States Gulf Coast, Rocky Mountains and Southern North ocean (Stoneley 39). 2. Carbonate Rock Reservoirs Carbonate reservoirs comprise of geologic formation that are naturally fractured which are characterized by heterogeneous permeability and porosity distributions. These are the predominant types of reservoirs all over the world accounting for nigh 50% of all reservoirs. The distinctive picture of carbonate reservoirs is their intrabasinal origin. Their mode of formation was primarily dependent on organic activities. They were formed through biochemical processes in special environments. Organisms involved in their formation besides contributed in determination of their qualities. Carbonate reservoirs are highly susceptible to processes of modification as a payoff of post-depositional mechanisms. The variations o bserved among various carbonate reservoirs result from processes such as lithification and compaction (Ahr 50). A notable have got of these reservoirs is their high sensitivity to environmental changes. Changes in temperatures scratch biogenic activities thus affecting sediment production. This aspect is what makes carbonate reservoir development depth dependent. Favorable conditions enhance organic productivity while in unfavorable conditions productivity ceases. Carbonate reservoirs are considered autochthonous since they develop close to their final depositional sites. Water brawniness and basin configuration influences deposition which leads to formation of carbonate reservoirs. Examples of carbonate reservoirs are found in great Horn Basin in Wyoming and south Caspian basin which encompasses... They develop better vugs and fractures that are relatively classical for flow and storage of fluids. Carbonate reservoirs are also harder and tighter than sandstone reservoirs (Ren pu 9). Primary porosity of sandstone reservoirs is exclusively interparticle while that of carbonate reservoirs dissolve either be intraparticle, interparticle, intercrystalline, vuggy, fenestral or cavernous. Porosity-permeability relationships of sandstones are relatively consistent and dependent on particle texture while that of carbonate reservoirs are highly varied and independent of particle size of it (Ahr 53). Shale reservoirs differ from sandstone reservoirs in that shale reservoirs can contain organic mudstones which are not present in sandstone reservoirs. They can also have open fractures which are not common in sandstone reservoirs. Conglomerate reservoirs differ from sandstone reservoirs in that conglomerate reservoirs exhibit an extra-high heterogeneity as a result of a complex pore structure. They also display rapid changes in permeability and porosity between their layers which is not the case with sandstone reservoirs (Zou 298).Advantages of Sandstone ReservoirsP orosity of sandstone reservoirs is consistent over time since it does not diminish with increasing saturation of the reservoir. Chemical processes do not affect the permeability and porosity of sandstone reservoirs. Effects and of micro and macro organisms do not impede fluid dislodge through sandstone reservoirs as can be the case with carbonate reservoirs (Renpu 11).