Recompression Index Calculator
Recompression (swell/reload) index Cr = Cs = (e1 - e2) / log10(sigma2' / sigma1') measured on an unload-reload loop of an oedometer test. Void ratios dimensionless, effective stresses in kPa.
Description
Recompression (swell/reload) index Cr = Cs = (e1 - e2) / log10(sigma2' / sigma1') measured on an unload-reload loop of an oedometer test. Void ratios dimensionless, effective stresses in kPa.
Recompression Index Calculator: Recompression (swell/reload) index Cr = Cs = (e1 - e2) / log10(sigma2' / sigma1') measured on an unload-reload loop of an oedometer test. Void ratios dimensionless, effective stresses in kPa.
When to use Recompression Index
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.
- e1
- Void ratio e1 at the start of the reload increment.
- e2
- Void ratio e2 at the end of the reload increment.
- sigma1'
- Effective vertical stress sigma1' in kPa.
- sigma2'
- Effective vertical stress sigma2' in kPa.
How Recompression Index works
Recompression (swell/reload) index Cr = Cs = (e1 - e2) / log10(sigma2' / sigma1') measured on an unload-reload loop of an oedometer test. Void ratios dimensionless, effective stresses in kPa. 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
- Cr
- Recompression index Cr (dimensionless).
Limitations and assumptions
- Geological models are scale-, site-, method-, and calibration-dependent. Heterogeneity, anisotropy, sampling, diagenesis, pressure-temperature history, instrument response, boundary conditions, and empirical-correlation range can dominate the result.
- 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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Geology — Wikipedia contributors
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