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Sub-Bottom Profiler Chirp Calculator engineering
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Sub-Bottom Profiler Chirp Calculator

Marine geophysics & offshore geotechnical engineering: Compute chirp pulse compression processing gain, vertical sediment bed resolution, and acoustic attenuation.

Chirp Acoustic Signal Parameters

Lower sweep limit
Upper sweep limit
Transmitted sweep duration
Soft clay ~1500, sand ~1700 m/s
Hamilton empirical attenuation
Sub-seabed penetration depth

Resolution & Processing Performance

Vertical Layer Resolution (Δr)
-
Δr = c_sed / (2 · B)
Pulse Compression Gain (G)
-
-
Two-Way Attenuation Loss
-
2 · z · α · f_mid
Compressed Pulse Width (τ_c)
-
τ_c = 1 / Bandwidth
Chirp Sweep Bandwidth (B)
-
f_end - f_start
Center Frequency (f_mid)
-
(f₁ + f₂) / 2

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Frequently Asked Questions

Why do Chirp systems offer better resolution than traditional pingers?

Traditional pingers face a direct tradeoff: short pulses give high resolution but low energy and poor penetration, while long pulses give deep penetration but terrible vertical resolution. Chirp decouples resolution from pulse length by sweeping over a wide frequency band and compressing the received signal via matched filtering.

How does sediment type influence acoustic penetration depth?

Fine-grained cohesive sediments like soft clays and organic muds have low attenuation (0.1 - 0.3 dB/m/kHz), allowing Chirp penetration up to 50 - 100 meters. Coarse gravels, dense sands, and gassy sediments scatter and absorb sound rapidly, restricting penetration to a few meters.

What is the Rayleigh criterion for bed thickness detection?

The Rayleigh criterion states that two adjacent sedimentary interfaces can be resolved as distinct acoustic reflections only if their vertical separation is greater than one-quarter of the dominant acoustic wavelength (λ/4).