In peatlands of Western Siberia, bubbles of greenhouse gases tend to accumulate in a layer of 40-60 cm in peat deposits. The peculiarities of spatial localization of the bubbles of greenhouse gases in peat deposits have been studied by the direct method of peat boring and by the method of electrical sounding. A good agreement between the results obtained by these two methods and definite advantages of electrophysical methods (preservation of peat thickness, lower labor expenses, and high reproducibility of the results) allow us to recommend electrical sounding for studying spatial localization of the bubbles of greenhouse gases in peat bogs.
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