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The uncertainty of the measurement geometry - absence of information about shape, dimensions, activity distribution, and spatial position of the radioactive cloud relative to the detector location - makes it difficult to perform g spectrometry of radioactive emissions, for example, from nuclear power plants. The combined use of g spectrometer and radar-tracer method, which "visualizes" a radioactive cloud, makes it possible to switch from qualitative analysis of g spectra to determination of quantitative content of radionuclides in the emission. Schemes for radar-spectrometric probing and the basic computational relations for determining the activity of radionuclides are examined.