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Fracture pressure and gradient (Eaton)

Formation fracture pressure by Eaton's method: the minimum horizontal stress from the overburden and pore pressures through Poisson's ratio. The gradient is given in kPa/m or as an equivalent density.

Formula
P_frac = ν / (1 − ν) · (σ_v − P_p) + P_pG_frac = P_frac / H

Uniaxial-strain model: tectonic stresses are ignored, so in tectonically active areas the fracture pressure is higher. The result is close to the minimum stress, the fracture opening pressure; the tensile strength of the rock is not included. Calibrate with a mini-frac or a leak-off test.

Source: Eaton, "Fracture gradient prediction and its application in oilfield operations", JPT (1969); with ν = 0.25 and σ_v/H = 1 psi/ft it equals the Hubbert & Willis (1957) minimum

Inputs

You can change a field's unit: the value is converted to the formula's units automatically.

σ_v

Integral of the density log; roughly 0.0226 MPa/m × H (average bulk density 2.3 g/cm³, 1 psi/ft).

P_p

The current one: fracture pressure drops as the reservoir depletes.

ν

From sonic logs or core: sandstones 0.2–0.3, shales 0.3–0.45; in Eaton's chart it rises with depth towards 0.5.

H
Unit converter for this formulaPressure · Length · Pressure gradient and equivalent density
Metric
  • MPa1
  • kPa1,000
  • bar10
  • atm9.86923
  • kgf/cm²10.1972
  • mmHg7,500.62
  • MPa(g)0.898675
  • barg8.98675
US field units
  • psi145.038
  • psia145.038
  • psig130.342
  • ksi0.145038

psi and psia are absolute pressure; gauge units (barg, MPa(g), psig) are above atmospheric (101.325 kPa = 14.696 psi). Pressure differences in the formulas do not depend on this.

All units
Result
P_fracFracture pressure
Fill in all fields
  • G_fracFracture gradient
  • ν/(1 − ν)Effective stress ratio

More in Fracturing and acidizing

Results are engineering estimates from standard formulas; for design decisions check them against the codes, project documents and specialists' calculations. The formulas carried over from the original set are unchanged, and their errors are described in the notes.