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Reservoir EngineeringReservoir Volumetrics

Original Water In Place with Net-to-Gross Formula

W=7758AhgNTGϕSwiBwiW=\frac{7758Ah_gNTG\phi S_{wi}}{B_{wi}}

Original Water In Place with Net-to-Gross calculates original water in place for reservoir volumetrics workflows in reservoir engineering.

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How engineers use this formula

Use this formula when the listed inputs (A, h_g, NTG, phi, S_wi, B_wi) are known and the assumptions behind the cited reservoir volumetrics relationship match the engineering case being checked.

Assumptions

  • Input values are representative for the well, reservoir, fluid, or equipment case being evaluated.
  • The declared units match the field-unit constants used in the formula.
  • The cited formula applies to the selected petroleum engineering workflow.

Limitations

  • The calculation does not replace a full engineering model or operating procedure.
  • Accuracy depends on the source correlation, assumptions, input quality, and unit consistency.

Common mistakes

  • Mixing unit systems without converting the inputs.
  • Using default example values as field recommendations.
  • Applying the formula outside the source assumptions.

Default example

Using the default inputs, W equals 2,464,305.882353 STB.

Aacres

160

h_gft

60

NTGfraction

0.75

phifraction

0.18

S_wifraction

0.25

B_wibbl/STB

1.02

Inputs

A

acres

Mapped Reservoir Area

h_g

ft

Average Gross Reservoir Thickness

NTG

fraction

Net-to-Gross Thickness Ratio

phi

fraction

Average Reservoir Porosity

S_wi

fraction

Average Initial Water Saturation

B_wi

bbl/STB

Initial Water Formation Volume Factor

Outputs

W

STB

Original Water In Place

A

acres

Mapped Reservoir Area

h_g

ft

Average Gross Reservoir Thickness

NTG

fraction

Net-to-Gross Thickness Ratio

phi

fraction

Average Reservoir Porosity

S_wi

fraction

Average Initial Water Saturation

B_wi

bbl/STB

Initial Water Formation Volume Factor

Source and review

reviewed

Penn State PNG 301. Estimation of STOOIP Using the Volumetric Method, Equations 4.02-4.04c.

Source

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