Methods for trace analysis of the 5f actinide elements are reviewed. Emphasis is on the non-radioactive methods of analysis such as absorption and laser induced spectroscopies, precipitation and/or sorption, ion exchange and solvent extraction. Particular attention is given to methods which allow measurement of the relative concentrations of the different oxidation states of a cation such as plutonium as they occur in nature. Comparisons are given of the sensitivities of these methods with that of traditional radioactivity counting.Keywords Actinide, solvent extraction, luminescence, ion exchange, trace analysis, plutoniumThe radioactivity released to the atmosphere from nuclear testing has been estimated as about 200 EBq whereas that from reactor operation is ca. 3.3 EBq. By comparison, the Chernobyl accident released ca. 2 EBq and the TMI accident, 10-6 EBq. Most of the fission products are short lived and within a few years of the release, the radioactivity is dominated by 90Sr and 137Cs decay. However, over a longer time (> 1000 years), the actinide elements become the major source of residual radioactivity. Neptunium, plutonium, and americium are the major elements of long term concern, both from the weapon release and from the nuclear waste being generated by reactors. One ton of irradiated fuel from the present PWR reactors has 10.4 kg Pu, 0.48 kg Np and 0.16 kg Am. Although it is unlikely that releases from the nuclear fuel cycle are expected to be much less than the radioactivity in the environment from nuclear weapons tests, we must ensure this by careful management of the mining and reprocessing technology and by safe disposal of the final nuclear wastes.The hydrolytic, complexation (C032-, P043-, F-, humate, etc.), and sorption tendencies of actinides in natural waters increase the problems of determination of the nature and concentrations of the dissolved species. Particularly for plutonium is the speciation made difficult by the ease of redox reactions between the III, IV, V and VI oxidation states and the possibility of the coexistence of several of these oxidation states occurring simultaneously. We can use studies of the environmental behavior of the radioactivity released by weapons tests, previous reactor operations and the Chernobyl accident to predict the fate of future release. Since the concentrations are very low, trace analytical methods are required. In this paper, some methods for separation and analysis of trace concentrations of actinides in different oxidation states are reviewed. Developing reliable separation methods for ion which easily undergo redox is difficult and the use of "oxidation analogs" has been of major value in such work.