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MLL C M.L C M.L M L Obviously the fractions contain salts which increase in solu. bility as one passes from the See also:left to right, and with sufficient care and See also:patience this method permits a See also:complete separation. The salts which have been used include the sulphates, nitrates, chromates, formates, oxalates and malonates. R. J. See also:Meyer (Zeit. anorg. Chem., 1904, 41, p. 97) separates the See also:cerium earths by forming the See also:double See also:potassium See also:carbonates, e.g. K2Ce2(CO,)4. 12H20, which are soluble in potassium carbonate See also:solution, being precipitated in the See also:order lanthanum, praseodymium, cerium and neodymium on diluting the solution; C. A. von Welsbach (Chem. See also:News, 1907, 95, p. 196; 1908, 98, pp. 223, 297) separates the metals of the
See also:ytterbium See also:group by converting the basic nitrates into double ammonium oxalates and fractionating; C. See also: Chem. Soc., 1904, 26, p. 78o) used See also:meta-nitrobenzoic See also:acid ; O. Holmberg separates neodymium, praseodymium and lanthanum (and also See also:thorium) with meta-See also:nitrobenzene sulphonic acid, and has investigated many other organic salts (see Abs. J. C. S., 1907, ii. p. 90), whilst H. See also:Erdmann and F. Wirth (See also:Ann., 1908, 361, p. 18o) employ the 1.8 naphthol sulphonates. In order to determine whether any chosen method for separating these earths is really effective, it is necessary to analyse the fractions. For this purpose two processes are available. We may convert the See also:salt into the oxalate from which the See also:oxide is obtained by See also:heating. A weighed quantity of the oxide is now taken and converted into sulphate by evaporating with dilute sulphuric acid. The sulphate is gently dried until the See also:weight is See also:constant, and from this weight the See also:equivalent of the See also:earth can be calculated. When repeated fractionation is attended by no See also:change in the equivalent we may conclude that only one See also:element is See also:present. This See also:process, however, is only rough, for the elements with which we are dealing have very See also:close equivalents. A more exact method employs the Didymia f Praseodidymia Neodidymia spectra—spark, arc, See also:phosphorescence and absorption; the See also:evidence, however, cannot in all cases be accepted as conclusive, but when taken in See also:conjunction with chemical tests it is the most valuable method. Chemical Relations.—The rare earth metals were at first regarded as divalent, but determinations of the specific heats of cerium by Mendeleeff and See also:Hillebrand and of lanthanum and See also:didymium by Hillebrand pointed to their trivalency; and this view now has See also:general See also:acceptance. They are comparatively reactive: they See also:burn in See also:air to See also:form oxides of the type Me203; combine directly with See also:hydrogen at 2000–3000 to form hydrides of the See also:formula MH2 or MH3; nitrides of the formula MN are formed by passing See also:nitrogen over the oxides mixed with See also:magnesium; whilst carbides of the type MVIC2 are obtained in the electrolytic reduction of the oxides with See also:carbon. In addition to the oxides M203, several, e.g. cerium, See also:terbium and neodymium, form oxides of the formula MO2. The sesquioxides are bases which form salts and increase in basicity in the order Sc, Yb, Tm, Er, Ho, Tb, Gd, Sm, Y, Ce, Nd, Pr, La; the latter hissing with See also:water like quicklime. The placing of these elements in the periodic table has attracted much See also:attention on See also:account of the many difficulties which it presented. The simplest See also:plan of regarding them all as trivalent and placing them in the third group is met by the fact that there is not See also:room for them. Another See also:scheme scatters them in the order of their atomic weights in the last four See also:groups of the See also:system, but See also:grave objections have been urged against this plan. A third See also:device places them in one group as a See also:bridge between See also:barium and See also:tantalum. This was suggested by Benedick in 1904 (Zeit. anorg. Chen., 1904, 39, p. 41), and adopted in See also:Werner's table of 1905 (See also:Bey. 38, p. 914), whilst in 1902 Brauner (ibid. 32, p. 18) placed the group as a bridge on a See also:plane perpendicular to the planes containing the other elements, thus expanding the table into a three-dimensional figure. The question has also been considered by See also:Sir See also: Soc., 1888, 53, p. 487; 1889, 55, pp. 257 et seq.), whose inquiries led him to a new conception of the chemical elements. Additional information and CommentsThere are no comments yet for this article.
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