Shrinkage Ratio Calculator

Compute soil shrinkage ratio as oven-dry density divided by water density, and shrinkage limit from the mass and volume lost while drying.

Description

Compute soil shrinkage ratio as oven-dry density divided by water density, and shrinkage limit from the mass and volume lost while drying.

Shrinkage Ratio Calculator: Compute soil shrinkage ratio as oven-dry density divided by water density, and shrinkage limit from the mass and volume lost while drying.

When to use Shrinkage Ratio

Use this geological calculation for a transparent first-pass interpretation of measured rock, soil, fluid, well, stratigraphic, isotopic, geophysical, or seismic data under an explicitly selected model.

Wet volume
Initial wet volume V1 in cm3.
Dry volume
Oven-dry volume V2 in cm3.
Wet mass
Initial wet mass M1 in g.
Dry mass
Oven-dry mass M2 in g.
Water density (g/cm³)
Water density in grams per cubic centimeter.

How Shrinkage Ratio works

Compute soil shrinkage ratio as oven-dry density divided by water density, and shrinkage limit from the mass and volume lost while drying. The tool evaluates the supplied inputs together and returns the named outputs below; it does not infer omitted operating conditions or change the units shown.1

Shrinkage ratio
Shrinkage ratio SR (dimensionless, equals dry density over water density when drying is fully saturated).
Shrinkage limit
Shrinkage limit SL as a water content in percent.

Limitations and assumptions

  • Radiometric ages require the correct decay constants, isotopic ratios, standards, common-component correction, closure interpretation, initial composition, and analytical uncertainties. Disturbance, inheritance, diffusion, alteration, and model choice can make a calculated number differ from the geological event age.
  • Use finite inputs in the displayed units and preserve more precision than the final presentation requires. Independently verify safety-critical, financial, compliance, or production decisions.

Alternative or Complementary approaches

Compare independent measurements and models, retain units and analytical metadata, propagate uncertainty, and validate interpretations against logs, cores, maps, laboratory data, or field observations.

References

  1. Geochronology — Wikipedia contributors

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    Compute the shrinkage limit SL in percent from the initial water content (percent), wet and dry pat volumes (cm3), oven-dry mass (g) and water density (g/cm3).

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  • Water Content Calculator

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