Bubble Nucleation Supersaturation Drop
Screen Laplace critical radius after a caller decompression while gas-equivalent pressure remains fixed; homogeneous nucleation barriers/kinetics and eruption triggering are not established.
Description
Surface tension opposes bubble growth through Laplace pressure.
Surface tension opposes bubble growth through Laplace pressure. A larger supersaturation permits a smaller critical bubble radius.
Screen Laplace critical radius after a caller decompression while gas-equivalent pressure remains fixed; homogeneous nucleation barriers/kinetics and eruption triggering are not established.
When to use Bubble Nucleation Supersaturation Drop
Use this tool to screen Laplace critical radius after a caller decompression while gas-equivalent pressure remains fixed; homogeneous nucleation barriers/kinetics and eruption triggering are not established.
Gather the relevant observations and fitted model parameters. Use the stated units and time basis; keep paired observations aligned.
How to use Bubble Nucleation Supersaturation Drop and understand its results
- Gather the relevant observations and fitted model parameters. Use the stated units and time basis; keep paired observations aligned.
- Enter surfaceTensionNPerM, initialGasEquivalentPressurePa, initialAmbientPressurePa, pressureDropPa, preexistingBubbleRadiusM using the field table and calculation rules, then run the tool.
- Read finalSupersaturationPressurePa, criticalBubbleRadiusM, callerNucleusCanGrowUnderModel. The explanation below defines the units, signs, ordering and any flags or placeholder values.
- If the tool reports an input issue, correct the values and run it again. Apply the stated assumptions when interpreting a successfully returned result.
| Input field | Meaning | Value type; see rules below | Requirement |
|---|---|---|---|
| surfaceTensionNPerM | Surface tension n per m | number | Required |
| initialGasEquivalentPressurePa | Initial gas equivalent pressure Pa | number | Required |
| initialAmbientPressurePa | Initial ambient pressure Pa | number | Required |
| pressureDropPa | Pressure drop Pa | number | Required |
| preexistingBubbleRadiusM | Preexisting bubble radius m | number | Required |
Use positive tension, pressures and nucleus radius, and nonnegative decompression. Require final ambient pressure and gas-minus-ambient excess positive. Compare nucleus radius at or above the critical radius.1
critical radius = 2 × surface tension/final supersaturation pressure Units, indexing, boundary conditions and exceptional cases are defined in the calculation rules above.
| Output field | Meaning | Value type |
|---|---|---|
| finalSupersaturationPressurePa | Final supersaturation pressure Pa | number |
| criticalBubbleRadiusM | Critical bubble radius m | number |
| callerNucleusCanGrowUnderModel | Caller nucleus can grow under model | boolean |
{
"input": {
"surfaceTensionNPerM": 0.1,
"initialGasEquivalentPressurePa": 200000,
"initialAmbientPressurePa": 190000,
"pressureDropPa": 10000,
"preexistingBubbleRadiusM": 0.00001
},
"output": {
"finalSupersaturationPressurePa": 20000,
"criticalBubbleRadiusM": 0.00001,
"callerNucleusCanGrowUnderModel": true
}
} Limitations and assumptions
Gas-equivalent pressure stays fixed; nucleation barriers, kinetics and eruption triggering are excluded.
Numbers and computed results must be finite; overflow produces an error. Missing required fields, extra fields, wrong value types and violations of the calculation rules are input errors. A successfully returned false flag is an evaluated outcome; its meaning is explained above.
Alternative or Complementary methods
Use Volatile Solubility Degassing Fraction: Solve single-volatile closed-system exsolution conserving nonvolatile melt while saturation is defined on residual melt mass; not a naive initial-fraction difference or a pressure-solubility reference table. For a complementary task, use Limnic CO2 Overturn Nyos Risk Checker: Compare total caller Henry-equivalent gas pressure to local absolute hydrostatic confinement; this equilibrium supersaturation screen cannot establish lake overturn, nucleation, eruption probability or safety.
References
-
Bubble Nucleation Supersaturation Drop — tool.io
Similar or alternative tools
- Volatile Solubility Degassing Fraction
Solve single-volatile closed-system exsolution conserving nonvolatile melt while saturation is defined on residual melt mass; not a naive initial-fraction difference or a pressure-solubility reference table.
- Limnic CO2 Overturn Nyos Risk Checker
Compare total caller Henry-equivalent gas pressure to local absolute hydrostatic confinement; this equilibrium supersaturation screen cannot establish lake overturn, nucleation, eruption probability or safety.