Underwater Acoustic Characterisation Of Unexploded Ordnance Disposal Using Deflagration 🆓 🎯

Acoustic characterisation further reveals a crucial spectral shift. While detonation deposits energy uniformly across a wide band (10 Hz to >100 kHz), deflagration concentrates its energy in the low-frequency regime, typically below 500 Hz. This frequency content is governed by the bubble pulse—the oscillation of the hot gas bubble created by the deflagration. Unlike the violent, high-frequency collapse of a detonation bubble, a deflagration bubble undergoes slower, larger-amplitude oscillations. For marine mammals, this low-frequency bias is a double-edged sword. Many baleen whales communicate in these low frequencies, meaning deflagration could potentially mask vocalisations over long distances. However, the lack of high-frequency energy is beneficial for smaller cetaceans and fish, which are often more sensitive to frequencies above 1 kHz. Moreover, the low frequencies attenuate more slowly in water, but because the absolute source level is lower, the overall radius of impact for physiological harm is dramatically reduced.

The legacy of past conflicts and military training exercises is a hidden hazard lying silent on the seabed: unexploded ordnance (UXO). Millions of tons of shells, bombs, and mines contaminate marine environments worldwide, posing significant risks to human safety, offshore construction (e.g., wind farms, pipelines), and marine ecosystems. Traditional disposal methods, such as high-order detonation using donor charges, are effective but increasingly controversial. They generate intense shockwaves, devastating acoustic trauma to marine mammals, fish, and invertebrates. In response, the defence and environmental communities have turned to low-order deflagration—a rapid, controlled burning rather than a supersonic explosion. However, to validate deflagration as a viable, quieter alternative, a rigorous underwater acoustic characterisation is essential. This essay argues that the acoustic signature of deflagration is fundamentally distinct from that of detonation, characterised by lower peak pressures, a shift in energy to lower frequencies, and a longer rise time, making it a potentially transformative but still challenging technology for UXO disposal. Unlike the violent, high-frequency collapse of a detonation

To understand the acoustic benefits of deflagration, one must first contrast it with the physics of detonation. A high-order detonation involves a supersonic reaction front that generates a discontinuous pressure wave—a shock. In water, which is nearly incompressible, this shock propagates with devastating efficiency. The key acoustic parameters of a detonation are extremely high peak pressure (often exceeding 200 dB re 1µPa at 1m), a very short rise time (microseconds), and a high-amplitude, broad-frequency spectrum extending into ultrasonic ranges. This impulsive sound is particularly harmful to marine life, causing barotrauma (tissue damage from pressure changes), temporary or permanent hearing loss, and behavioural disruption over vast areas (tens of kilometres). However, the lack of high-frequency energy is beneficial