Calculating Pore Pressure From Well Logs

Pore Pressure Calculator from Well Logs

Estimate pore pressure using Eaton-based workflows from sonic or resistivity logs. Enter depth, stress gradients, and observed log response to generate pressure, gradient, mud weight equivalent, and a pressure profile chart.

Target depth at the calculation point.
Depth is internally converted to feet for pressure equations.
Typical range: 0.95 to 1.10 psi/ft depending on lithology and basin.
Hydrostatic baseline commonly near 0.433 to 0.465 psi/ft.
Used to estimate drilling window at this depth.
Select the log family used for trend and observation.
For sonic: normal transit time (us/ft).
For sonic: observed transit time (us/ft).
Sonic often uses exponent near 3.0.
Results will appear here after calculation.

Expert Guide: Calculating Pore Pressure from Well Logs

Pore pressure prediction is one of the most important geomechanics tasks in exploration and development drilling. It directly influences mud weight, casing design, well control risk, rate of penetration strategy, and even the economics of trajectory selection. A robust workflow is not just about plugging values into a formula. It requires a calibrated understanding of compaction trends, basin context, data quality, and the physical link between stress and rock properties. This guide explains how engineers and geoscientists estimate pore pressure from log data with practical precision.

Why pore pressure matters operationally

If mud pressure is below pore pressure, formation fluids can enter the wellbore and lead to kicks or blowouts. If mud pressure is too high, formations may fracture, causing losses and potentially reducing well integrity. The safe drilling window is therefore constrained between pore pressure and fracture pressure. In deep, young, undercompacted basins, this window can become very narrow and requires accurate pre-drill and while-drilling updates.

  • Well control: underestimation of pore pressure increases influx risk.
  • NPT reduction: better pressure models reduce stuck pipe, losses, and sidetracks.
  • Casing optimization: accurate pressure prediction improves shoe depth decisions.
  • Reservoir appraisal: pressure regimes help interpret seal integrity and fluid contacts.

Core concept: effective stress and log response

The foundation is Terzaghi-style effective stress behavior. In sedimentary sections, increasing depth usually increases compaction, decreases porosity, and changes log responses in a predictable way. If pore pressure rises abnormally, effective stress decreases relative to normal compaction, and logs depart from normal trends. Sonic slowness often increases, and resistivity often decreases versus normal compaction expectations. Eaton methods transform these departures into pressure estimates using overburden and normal pressure references.

Data required for log-based pore pressure estimation

  1. Depth framework: true vertical depth and consistent datum handling.
  2. Overburden stress model: often built from density logs, seismic velocity inversion, and regional rock density assumptions.
  3. Normal pore pressure reference: commonly hydrostatic gradient adjusted for formation water salinity and temperature.
  4. Normal compaction trend (NCT): baseline trend of sonic or resistivity in normally compacted shale.
  5. Observed log values: quality-controlled sonic or resistivity at the target depth.
  6. Calibration points: MDT/RFT pressure tests, LOT/FIT, mud losses, and drilling events.

Eaton method overview

The calculator above supports the two most common variants:

  • Sonic Eaton: Pp = Sv – (Sv – Pn) × (NCT/Observed)n
  • Resistivity Eaton: Pp = Sv – (Sv – Pn) × (Observed/NCT)n

Where:

  • Pp = pore pressure at depth
  • Sv = overburden stress at depth
  • Pn = normal pressure at depth
  • n = Eaton exponent (commonly around 3.0 for sonic, around 1.2 for resistivity in many basins)

The exponent is not universal. It should be calibrated by basin and formation age. Using a default exponent without calibration can shift predicted pressure significantly.

Typical pressure and gradient statistics used in field workflows

Parameter Common Value or Range Operational Interpretation
Freshwater hydrostatic gradient 0.433 psi/ft Base normal pressure reference in low salinity systems.
Brine hydrostatic gradient 0.445 to 0.465 psi/ft Used in saline formations and many offshore settings.
Overburden gradient (sedimentary basins) 0.95 to 1.10 psi/ft Defines upper confining stress used in Eaton equations.
Equivalent mud weight conversion 1.0 ppg = 0.052 psi/ft Converts pressure gradient directly to mud weight target.
Abnormal pressure screening threshold Often above 0.55 psi/ft Formation likely overpressured; verify with multiple indicators.

These values are widely used in petroleum engineering practice and align with common industry references and field datasets, but they should always be adjusted to local geology and fluid properties.

Worked calculation logic at a single depth

Assume depth 10,500 ft, overburden gradient 1.00 psi/ft, normal pressure gradient 0.465 psi/ft, sonic NCT 80 us/ft, observed sonic 110 us/ft, exponent 3.0.

  1. Compute Sv = 1.00 × 10,500 = 10,500 psi.
  2. Compute Pn = 0.465 × 10,500 = 4,882.5 psi.
  3. Ratio = 80/110 = 0.7273.
  4. Ratio3 = 0.384.
  5. Pp = 10,500 – (10,500 – 4,882.5) × 0.384.
  6. Pp ≈ 8,343 psi; gradient ≈ 0.794 psi/ft; equivalent mud weight ≈ 15.27 ppg.

This result indicates strong overpressure relative to hydrostatic conditions and would require careful mud and casing planning.

Method comparison and sensitivity statistics

Case Method Inputs Exponent Estimated Pore Gradient (psi/ft) Equivalent Mud Weight (ppg)
Base sonic case NCT 80 us/ft, observed 110 us/ft 3.0 0.794 15.27
Sonic lower exponent sensitivity NCT 80 us/ft, observed 110 us/ft 2.5 0.762 14.65
Resistivity case NCT 2.0 ohm-m, observed 1.2 ohm-m 1.2 0.766 14.73

Even moderate exponent changes can shift equivalent mud weight by several tenths of ppg. In narrow windows, that is a meaningful operational difference.

How to build a defensible normal compaction trend

NCT quality often controls final model quality. Avoid fitting trend lines through mixed lithology or obvious pressure transitions. Best practice is to isolate shale intervals with reliable log quality, then fit trend families by age/depositional package. In many projects, a single basin-wide NCT is less accurate than stratigraphically segmented trends.

  • Perform shale volume filtering before trend fitting.
  • Exclude washout-affected intervals from sonic.
  • Correct resistivity for temperature where necessary.
  • Use offset wells to stabilize trend uncertainty.
  • Tie trends to measured pressure tests whenever possible.

Common pitfalls and how to avoid them

  1. Ignoring lithology: sand-rich zones and cemented streaks can mimic pressure effects. Always interpret with petrophysical context.
  2. Overtrusting a single log: combine sonic, resistivity, drilling parameters, and direct pressure tests.
  3. Bad depth matching: small depth shifts can create major pressure interpretation errors across steep gradients.
  4. Uncalibrated exponents: generic exponents are starting points, not final answers.
  5. No uncertainty envelope: always provide low, base, and high scenarios for operations planning.

Integrating the calculator into drilling workflows

The most useful workflow is iterative:

  1. Build pre-drill pressure model from offsets, seismic velocity, and regional trends.
  2. Update during drilling with LWD/MWD logs and drilling events.
  3. Recalibrate at each pressure test and LOT/FIT checkpoint.
  4. Track movement of pore pressure and fracture gradients simultaneously.
  5. Convert outputs to equivalent mud weight and compare against active mud program.

By treating pressure prediction as a continuously updated model rather than a one-time estimate, teams reduce surprises and improve well delivery consistency.

Quality control checklist before finalizing a pressure estimate

  • Are all pressure calculations referenced to the same vertical datum?
  • Is overburden based on the best available density control?
  • Are NCT picks limited to normal compaction intervals?
  • Is the selected exponent justified by local calibration?
  • Do predicted pressures agree with mud weight events and measured tests?
  • Is uncertainty captured with operationally useful low and high cases?

Practical recommendation: when the estimated equivalent mud weight approaches the local fracture-equivalent mud weight margin, run sensitivity on exponent, NCT selection, and overburden assumptions before making program changes.

Authoritative technical references and regulatory context

For high-confidence engineering decisions, always review government and university resources in addition to internal standards:

Final takeaways

Calculating pore pressure from well logs is a high-value geomechanics task that combines physics, calibration, and operational judgment. Eaton methods remain practical and widely used because they connect measurable log departures to effective stress changes in a transparent way. The calculator on this page gives a fast estimate and visualization, but its strongest use is as part of a larger calibrated workflow with offset analogs, direct pressure measurements, and real-time drilling feedback. If you maintain strict data quality controls and explicitly manage uncertainty, you can significantly improve well safety and drilling performance.

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