Hydrocarbons Essay

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Two properties are required for fluid movement of Reservoir rocks and Source rocks: permeability and porosity. It consist voids or pores, ability to contain fluid (known as porosity) and the pores are interconnected (permeability) in order to allow flow to occur. Hydrocarbons can be termed as reservoir fluid. The volume of hydrocarbons stored in a reservoir depends upon the porosity of the reservoir rock. The rate and volume at which hydrocarbons are withdrawn depends upon the permeability of the reservoir rock. Almost complete pore space of the superior several kilometres of earth’s crust contains water. Therefore in this water environment hydrocarbons exist with amalgamation of oil, gas and water occurring in different proportions.
The two dominant physical properties of oil and gas that enhance their movement through subsurface substance are their relative immiscibility in water and their lower density than water which causes their buoyancy. Buoyancy of the hydrocarbons occurs because of differences in densities of respective fluids while transcend via the oil and gas reservoir is a stimuli which creates differential pressures that exist in a reservoir bed.
The basic properties of rocks can be classified as the following:
Skeletal
The "skeleton" structures of the rocks of reservoir are affected by the depositional surrounding and numerous earth processes after deposition.
Dynamic
This is related to the blending of the fluids and rocks of the reservoir. Skeletal properties of interest to reservoir engineers include porosity, pore size distribution, compressibility, and absolute permeability of the rod. Interaction or dynamic properties of reservoir rocks are affected by the nature and by its interaction with present fluids, as...

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...a producing well is significantly lower than at other areas where no well is drilled. The driving force could be either natural or created by engineering design involving fluid injection through certain wells placed optimally to achieve the best results. Experimental data suggests that reservoir rocks are abundantly permeable in both vertical and horizontal directions. Among a myriad of factors related to geological and geochemical processes, the permeability of a rock is influenced by the slit, shape, configuration, and connectivity or a porous network.

Darcy Equation and its Application
Darcy’s law provides an accurate description of the flow of ground water in almost all hydrogeological environments. Henri Darcy established empirically that the flux of water through a permeable formation is proportional to the distance between top and bottom of the soil column.

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