This work aims at analyzing the problem of losses by absorption in seismic reflection data and test three correction methods available in the literature. We use the modeling of the absorption presented by Romanelli Rosa, with the concept of instantaneous frequency, and analyzed the following correction methods: Q compensation, Varela s method and Duarte s method, which is a recursive filter. We note that Duarte s method is computationally faster than the others. However, we can use the Fourier Transform to make it faster in cases where the recursion is interrupted at a step M, smaller than the number of samples N in the seismic data and greater than ln N. Finally, we test the performance of the methods in a marine seismic line in Sergipe-Alagoas Basin, provided by the Agência Nacional do Petróleo, Gás Natural e Biocombustíveis (ANP). The line was reprocessed, with the correction of the losses by absorption applied before stacking, for each method studied. In order to compare the results, the data was also processed without correction of absorption. We observe an increase in the resolution of the geological subsurface in all methods tested in comparison with the data without correction. We also observe the computational advantage of Duarte s method.