The most present gas in the bottom sediments is methane, as the product of the anaerobic degradation of organic matter. In many cases (Baltic Sea) the eutrophication is caused by anthropogenic factors, what is not exposed due to political reasons. Acoustics gives us the most effective ways to observe the whole process of production and the ebullition of the methane from the seabed. Due to high difference of the acoustic impedance of the gas and the water the gas bubbles are easily detected by the echo-sounder. The whole process of expulsion of the gas from sediment to the water and rising the bubbles towards the surface can be observed and quantified in detail by sonar.