Coda Q Scattering Intrinsic Split Calculator
Split total attenuation into intrinsic and scattering parts via 1/Q_total = 1/Q_intrinsic + 1/Q_scattering.
Description
Split total attenuation into intrinsic and scattering parts via 1/Q_total = 1/Q_intrinsic + 1/Q_scattering.
Coda Q Scattering Intrinsic Split Calculator is a focused tool for the following task. Split total attenuation into intrinsic and scattering parts via 1/Q_total = 1/Q_intrinsic + 1/Q_scattering. It reports Qt, Qs% from the values you provide rather than inventing measurements, coefficients, or professional judgment that are not part of the input.
When to use Coda Q Scattering Intrinsic Split
Use this seismology calculation to reproduce a stated convention, screen observations, or compare scenarios whose units, coordinate conventions, catalog selection, and model assumptions are known.
- Qi
- Required number. Intrinsic quality factor.
- Qs
- Required number. Scattering quality factor.
The cited overview of Seismic wave supplies background for the terminology and domain context used by this tool.1
How Coda Q Scattering Intrinsic Split works
Split total attenuation into intrinsic and scattering parts via 1/Q_total = 1/Q_intrinsic + 1/Q_scattering. Inputs are interpreted exactly in the displayed units and the calculation returns the following fields without presentation rounding.
- Qt
- Returned number. Total quality factor.
- Qs% (%)
- Returned number in %. Scattering share of total attenuation.
Limitations and assumptions
- Earth structure, source geometry, path effects, site response, instrument response, catalog completeness, uncertainty, and the fitted range can dominate the accuracy of simplified seismic calculations.
- Qi must be at least 0.
- Qs must be at least 0.
- Use finite inputs in the displayed units, preserve source measurements and assumptions, and independently verify consequential decisions.
Alternative or Complementary approaches
For analysis or hazard decisions, retain uncertainty and provenance and compare the result with waveform processing, calibrated regional models, and guidance from qualified seismologists or the responsible agency.
References
-
Seismic wave — Wikipedia contributors
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