Geology Fracture Transmissivity Cubic Law Calculator

Fluid-dependent cubic-lawρgb³/(12μ) fracture transmissivity; distinct from intrinsic b²/12. Caller independently establishes matching units, evidence, method edition and applicability; output is not compliance, diagnosis, work-safety approval, geological identity or validated hazard prediction.

Description

The cubic law models laminar flow through an idealized parallel-plate fracture.

The cubic law models laminar flow through an idealized parallel-plate fracture.1

Hydraulic transmissivity includes fluid density, gravity and viscosity, unlike intrinsic permeability or permeability-times-width alone. Use this tool to calculate fracture transmissivity cubic law from the supplied measurements and assumptions.

When to use Geology Fracture Transmissivity Cubic Law Calculator

Use this tool to calculate fracture transmissivity cubic law from the supplied measurements and assumptions. Establish the measurement units, sampled interval, calibration or model edition and geological assumptions before entering data.

How to use Geology Fracture Transmissivity Cubic Law Calculator and understand its results

  1. Establish the measurement units, sampled interval, calibration or model edition and geological assumptions before entering data.
  2. Enter hydraulicApertureM, fluidDensityKgM3, gravityMSecond2, viscosityPaSecond, using the field meanings and rules below, then run the tool.
  3. Read fractureTransmissivityM2Second. Interpret the fields using their units, signs and evidence conventions below.
  4. If input validation fails, correct the reported field and run again. Before applying the result, check reference scope, model assumptions and any missing evidence or placeholder values.
Input fieldMeaningValue typeRequirement
hydraulicApertureMHydraulic aperture mnumberRequired
fluidDensityKgM3Fluid density kg m3numberRequired
gravityMSecond2Gravity m second2numberRequired
viscosityPaSecondViscosity pa secondnumberRequired

Require positive aperture in meters, density in kg/m³, gravity in m/s² and viscosity in Pa·s. Apply the cubic law and return hydraulic transmissivity in m²/s. Roughness, channel contact and nonlaminar corrections are not modeled.

T_m²/s=density×gravity×aperture³/(12×viscosity)

Use the exact units, boundary rules, ordering and missing-evidence conventions above.

Output fieldMeaningValue type
fractureTransmissivityM2SecondFracture Transmissivity M2 Second; follow the units, sign, ordering and evidence convention stated abovenumber
json
{
  "input": {
    "hydraulicApertureM": 0.01,
    "fluidDensityKgM3": 1000,
    "gravityMSecond2": 10,
    "viscosityPaSecond": 0.01
  },
  "output": {
    "fractureTransmissivityM2Second": 0.08333333333333336
  }
}

Limitations and assumptions

Hydraulic transmissivity includes fluid density, gravity and viscosity, unlike intrinsic permeability or permeability-times-width alone. Interpretation depends on the units, sampling scope and exact model described above.

All listed fields require explicit values. Unexpected fields, incorrect types, nonfinite numbers and sparse evidence arrays fail validation; the specific bounds and alignment requirements are stated above. Extremely large inputs or outputs can also be rejected. An input error is distinct from a successful result reporting false, no matches or missing evidence.

Alternative or Complementary methods

Use Geology Hydraulic Fracture Conductivity Calculator for this related task: Fracture conductivity is the product of intrinsic permeability and an effective fracture width in the adopted model.

Use Geology Fracture Permeability Parallel Plate Calculator when its separate inputs and assumptions fit the question: An ideal parallel-plate fracture has intrinsic permeability proportional to the square of its aperture.

References

  1. Geology Fracture Transmissivity Cubic Law Calculator — tool.io

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