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
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Geochronology — Wikipedia contributors
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