3.2 Construct IPR of a vertical well in a saturated oilreservoir using Vogel's equation. The following dataare given:Porosity, = 0.2Effective horizontal permeability, k 80 mdPay zone thickness, h 55 ftReservoir pressure, p = 4,500 psiaBubble point pressure, p, = 4,500 psiaFluid formation volume factor, B, = 1.1Fluid viscosity, H. = 1.8 cpTotal compressibility, c, = 0.000013 psi-Drainage area, A = 640 acres (re = 2,980 ft)Wellbore radius, rw 0.328 ftSkin factor, S = 2%3D

Answered: Image /qna-images/answer/3e5d3dc3-7ae9-45e0-a5c7-e3da62c86919.jpg

iven: -sity, = 0.2 tive horizontal permeability, k = 80 1 zone thickness, h = 55 ft rvoir pressure, p 4,500 psia ple point pressure, ph = 4,500 psia d formation volume factor, B, = 1.1 d viscosity, , = 1.8 cp 1 compressibility c.= 0 000013 nsi-!

iven: -sity, = 0.2 tive horizontal permeability, k = 80 1 zone thickness, h = 55 ft rvoir pressure, p 4,500 psia ple point pressure, ph = 4,500 psia d formation volume factor, B, = 1.1 d viscosity, , = 1.8 cp 1 compressibility c.= 0 000013 nsi-!

Principles of Geotechnical Engineering (MindTap Course List)

9th Edition

ISBN:9781305970939

Author:Braja M. Das, Khaled Sobhan

Publisher:Braja M. Das, Khaled Sobhan

Chapter7: Permeability

Section: Chapter Questions

Problem 7.23P

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Concept explainers

Sediment transport

Sediment transport or Soil transport is the movement of solid particles, usually due to the combination of gravitational forces acting on the sediment, and the movement of the liquid at which the sediment enters. Soil erosion occurs in natural systems where the particles are sandstones (sand, rocks), mud, or clay; the liquid is air, water, or ice; and the gravitational force that works to move particles to the landing surface. Sediment transportation or soil migration due to the movement of liquids occurs in rivers, lakes, lakes, oceans, and other bodies of water as a result of currents and waves. Transportation is also caused by glaciers as they flow, and to places on earth under the influence of wind. Soil erosion due to gravity alone is possible in most sloping areas, including hills, scarves, cliffs, and the continental shelf — the continental boundary of the slope.

Question

3.2 Construct IPR of a vertical well in a saturated oil
reservoir using Vogel's equation. The following data
are given:
Porosity, = 0.2
Effective horizontal permeability, k 80 md
Pay zone thickness, h 55 ft
Reservoir pressure, p = 4,500 psia
Bubble point pressure, p, = 4,500 psia
Fluid formation volume factor, B, = 1.1
Fluid viscosity, H. = 1.8 cp
Total compressibility, c, = 0.000013 psi-
Drainage area, A = 640 acres (re = 2,980 ft)
Wellbore radius, rw 0.328 ft
Skin factor, S = 2
%3D

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