. Can. J . Chem. 67, 517 (1989). The Raman spectra of acidified aqueous iron(II1) chloride solutions have been measured between 25 and 300°C. When Fe3' concentrations are in the range 0.75 to 1.0 mol kg-' and ~l -/~e~+ ratios, R, in the range 3 to 9.5, the dominant species at 2S°C is tran~- [Fe(H~O) Introduction The nature and relative importance of species existing in aqueous solutions of ferric chloride have been studied by numerous investigators over many years using a variety of experimental techniaues. Most of the work has involved studies at or close to room temperature, with the notable exception of some recent glassy state (-196°C) Raman work (1). Higher temperature investigations have been limited to the hydrated melt of FeC13.6H20 (2, 3), at approximately 35-4O0C, and to some aqueous solutions at 50°C (4). Because of the general interest in high temperature aqueous systems involving geochemically important elements, hydrometallurgy, corrosion of high temperature reactors, etc. ( 3 , we have utilized Raman spectroscopic methods to study several such systems up to 300°C, with applied pressures up to 9 MPa to maintain the liquid phase (6, 7). We report here the results of a variable temperature investigation of several aqueous ferric chloride systems, between 25 and 300°C.Although earlier workers have used Raman spectroscopy to study similar systems at room temperature (4,8,9) there is still disagreement concerning the interpretation of their results. Indeed such disagreements are not confined to Raman investigations. For example, various X-ray studies arrive at conflicting conclusions as to the major species present. A succinct summary of the major work through 1984 has appeared recently (lo), and readers are referred to this paper for a discussion of the earlier work and possible reasons for the disagreements cited. It is clear that the nature of the species present, and their relative populations, stability constants, etc., are influenced to