Echo sounding

Hydroacoustic assessments have traditionally employed mobile surveys from boats to evaluate fish biomass and spatial distributions.

[1][2][3] Meanwhile, in France, physicist Paul Langevin (connected with Marie Curie and better known for his research work in nuclear physics) was recruited by French Navy laboratories at the beginning of World War 2 and conducted (then secret) research on active sonars for anti-submarine warfare (using a piezoelectric transmitter).

Though a fully operational échosondeur (sonar) was not ready for use in wartime, there were successful trials both off Toulon and in the English Channel as early as 1920, and French patents taken for civilian uses.

Oceanographic ships and French high-sea fishing assistance vessels were equipped with Langevin-Florisson and Langevin Marti recording sonars as early as the mid/late 1920s.

[5] Distance is measured by multiplying half the time from the signal's outgoing pulse to its return by the speed of sound in water, which is approximately 1.5 kilometres per second.

For high accuracy depths, usually restricted to special purpose or scientific surveys, a sensor may be lowered to measure the temperature, pressure and salinity.

Using that data, it's able to determine the distance from the strongest echo, which can be the seafloor, a concrete structure, or other larger obstacle.

As well as an aid to navigation (most larger vessels will have at least a simple depth sounder), echo sounding is commonly used for fishing.

Therefore, it is especially important when sounding in deep water, as the resulting footprint of the acoustic pulse can be very large once it reaches a distant sea floor.

In order to meet these standards, the surveyor must consider not only the vertical and horizontal accuracy of the echo sounder and transducer, but the survey system as a whole.

Different hydrographic organisations will have their own set of field procedures and manuals to guide their surveyors to meet the required standards.

Illustration of echo sounding using a multibeam echosounder .
The MTVZA sounder received from the Meteor M2-2 satellite by an amateur station
Diagram showing the basic principle of echo sounding
beam shape of a single-beam echosounder on a USV
Multibeam sonar is used to map the ocean floor
An example of a precision dual frequency echosounder, the Teledyne Odom MkIII
A screen grab of the difference between single and dual frequency echograms