Ac, a radioactive chemical element in the Group III of the Mendeleev periodic table, atomic number 89. No stable isotopes.
Actinium was discovered in 1899 by the French chemist A. Debierne while he was studying uranium ore tailings. The ten known radioactive isotopes of actinium have mass numbers ranging from 221 to 230. The longest-lived actinium isotope, 227Ac (half-life T½=21.8 years), emits beta particles (98.8 percent) and alpha particles (1.2 percent). The isotopes 227Ac and 228Ac (T½=6.13 h; also known as mesothorium II, MsThll) occur naturally in uraniferous and thoriferous ores as members of the naturally occurring radioactive families. The surface layer of the earth’s crust (thickness 1.6 km) contains 11,300 tons of 227Ac, but the actinium content in the earth’s crust is very small compared to that of other elements (6.10-10 percent by mass).
The element actinium is a silvery white metal with a face-centered cubic lattice (Tm=1050° ± 50°C, Tb probably about 3300°C); it glows faintly in the dark because of its high radioactivity. In moist air it becomes coated with a white film of oxide which prevents further oxidation of the metal. Actinium is trivalent in chemical compounds. Almost all actinium salts are white and are colorless in solution. Most of them (except AcP04) are isomorphic with the corresponding lanthanum compounds. Actinium forms the same insoluble compounds as does La (hydroxide, phosphate, oxalate, carbonate, fluosilicate). Actinium hydroxide Ac(OH)3 is more basic than lanthanum hydroxide La(OH)3. Because of the extraordinary similarities between the chemical properties of actinium and lanthanum, isolation of actinium in pure form from its natural hosts (containing La and other rare earths) involves great difficulties, and therefore milligram amounts of actinium (227Ac) are obtained artificially through neutron bombardment of radium 226Ra. Since probability of 227Ac decay with alpha emission is low, and the energy of beta particles emitted by this isotope is very small (46 keV), any emission accompanying the radioactive decay of 227Ac went undetected for a long time; until 1935 it was assumed that radioactive decay of 227Ac occurred without emission. Modern instruments are capable of identifying such soft beta radiation, but it is still quite difficult to make quantitative measurements; therefore, the behavior of 227Ac is usually monitored in terms of the activity of its daughters, in experiments involving trace amounts of the radionuclide. Mixed with beryllium, 227Ac is used in the preparation of neutron sources, in which neutrons are formed by irradiating 9Be nuclei with alpha particles emitted by 227Ac daughters.
S. S. BERDONOSOV