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24-Pet-A3 Fundamental Reservoir Engineering · December 2014

Question 2 of 7: Interwell Flow Direction and Velocity

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

98-Pet-A3 — Fundamental Reservoir Engineering · National Exams, December 2014 · 3 hours, closed book, Casio/Sharp approved calculator only · five (5) questions constitute a complete exam paper (the first five as they appear in the answer book are marked), all questions equal value, all parts of a multipart question equal weight.

Reference texts: Ahmed, T., Reservoir Engineering Handbook, 5th ed. (Darcy's law and fluid potential, transient well testing, p/Z and oil material balance, capillary pressure/relative permeability); Craft, B.C. & Hawkins, M.F., Applied Petroleum Reservoir Engineering, 3rd ed. (reservoir drive mechanisms, material balance fundamentals); Lyons, W.C. (ed.), Standard Handbook of Petroleum and Natural Gas Engineering, 3rd ed. (Standing–Katz Z-factor correlation); McCain, W.D., The Properties of Petroleum Fluids, 3rd ed. (capillary pressure and relative permeability laboratory data).

Question 2: Interwell Flow Direction and Velocity (20 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given.

Well separation3000 ft
Well A depth / pressure9000 ft ss, 4000 psia
Well B depth / pressure9200 ft ss, 4020 psia
Fluid gradient0.35 psi/ft
Permeability, $k$0.2 Darcy
Viscosity, $\mu$0.6 cP

Find. (a) The direction of flow between the two wells; (b) the Darcy (superficial) fluid velocity along the line joining them, in ft/day.

Well A9000 ft ss, 4000 psiaWell B9200 ft ss, 4020 psia3000 ft apartflow A → B (higher Φ → lower Φ)ground level (schematic, not to scale)
Fig. 1 — The two wells sit at different subsea depths, so a raw pressure comparison is misleading; flow direction requires comparing fluid potential at a common datum.

Approach. Correct each well's pressure to a common datum to get its fluid potential $\Phi$ (flow runs from high $\Phi$ to low $\Phi$), then apply Darcy's linear-flow velocity equation along the line joining the wells, using the true (inclined) separation distance.

  1. Fluid potential and flow direction. Referencing both wells to an arbitrary common datum (sea level, $D=0$) with the given fluid gradient, $\Phi = p - (0.35)D$: $\Phi_A = 4000-0.35(9000)=850$ psia; $\Phi_B = 4020-0.35(9200)=800$ psia. Since $\Phi_A>\Phi_B$, $\boxed{\text{flow is from Well A to Well B}}$, a potential drop $\Delta\Phi=\Phi_A-\Phi_B=50$ psi (the raw pressure difference alone, $4020-4000=20$ psi, would have wrongly suggested B$\to$A).
  2. True separation distance. The wells are offset both horizontally (3000 ft) and vertically ($9200-9000=200$ ft), so the flow path length is $L=\sqrt{3000^2+200^2}=3006.7$ ft (the 200 ft vertical offset changes $L$ by under 0.3%).
  3. Darcy velocity. With $k$ already in Darcy (per the formula sheet's unit convention), the linear-flow velocity is $v=1.127\dfrac{k}{\mu}\dfrac{\Delta\Phi}{L}$ in bbl/day per ft$^2$: $v=1.127\times\dfrac{0.2}{0.6}\times\dfrac{50}{3006.7}=1.127\times0.3333\times0.01663=0.006247$ bbl/day-ft$^2$. Converting to ft/day (1 bbl $=5.615$ ft$^3$): $\boxed{v=0.006247\times5.615=0.0351\ \text{ft/day}}$, directed from A to B.
QuantityValue
(a) Flow directionWell A → Well B
Potential drop, $\Delta\Phi$50 psi
(b) Darcy velocity, $v$0.0351 ft/day