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Bournazel Jeanson Vertical Well Water Breakthrough Dimensionless Time Formula

td=(ρwρo)gkvtBTfmμoϕeht_d=\frac{(\rho_w-\rho_o)gk_vt_{BT}f_m}{\mu_o\phi_eh}

Bournazel Jeanson Vertical Well Water Breakthrough Dimensionless Time calculates dimensionless breakthrough time for well performance workflows in reservoir engineering.

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How engineers use this formula

Use this formula when the listed inputs (rho_w, rho_o, g, k_v, t_BT, f_m, mu_o, phi_e, h) are known and the assumptions behind the cited well performance 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, t_d equals 52,121.88 dimensionless.

rho_wg/cc

1

rho_og/cc

0.85

gft/s^2

32.174

k_vmD

50

t_BTs

3600

f_mdimensionless

1.2

mu_ocP

2

phi_efraction

0.2

hft

50

Inputs

rho_w

g/cc

Water Density

rho_o

g/cc

Oil Density

g

ft/s^2

Gravitational Acceleration

k_v

mD

Vertical Permeability

t_BT

s

Water Breakthrough Time

f_m

dimensionless

Mobility Function Ratio

mu_o

cP

Oil Viscosity

phi_e

fraction

Effective Porosity

h

ft

Oil Column Thickness

Outputs

t_d

dimensionless

Dimensionless Breakthrough Time

t_BT

s

Water Breakthrough Time

k_v

mD

Vertical Permeability

f_m

dimensionless

Mobility Function Ratio

Source and review

reviewed

Bournazel, C. and Jeanson, B. 1971. Fast Water-coning Evaluation Method. SPE-AIME, New Orleans, Louisiana.

Source

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