Thorium astatine from

Astatine is a radioactive element that occurs in nature in uranium and thorium ores, but only to a minute extent. Samples are made by bombarding bismuth with a particles in a cyclotron, which accelerates the particles to a very high speed. Astatine isotopes do not exist long enough for its properties to be studied, but it is thought from spectroscopic measurements to have properties similar to those of iodine. 

Iodine is obtained by oxidizing iodides from seawater or brines using Cl2, concentrated H2S04, Fe3+, or other oxidizing agents. Astatine is produced naturally by the radioactive decay of uranium or thorium. Production of At is also accomplished by bombarding Bi with alpha particles,... 

Astatine is the heaviest member of group 17 and is known only in the form of radioactive isotopes, all of which have short half-lives. The longest lived isotope is At (fi = 8.1 h). Several isotopes are present naturally as transient products of the decay of uranium and thorium minerals At is formed from the 3-decay of Po, but the path competes with decay to Pb (the dominant decay, see Figure 2.3). Other isotopes are artificially prepared, e.g. "At (an a-... 

C. It occurs naturally by radioactive decay from uranium and thorium isotopes. Astatine forms at least 20 isotopes, the most stable astatine-210hasahalf-lifeof8.3 hours. It can also be produced by alpha bombardment of bismuth-200. Astatine is stated to be more metallic than iodine at least 5 oxidation states ate known in aqueous solutions. It will form interhalogen compounds, such as Atl and AtCl. The existence of At2 has not yet been established. The element was synthesized by nuclear bombardment in 1940 by D. R. Corson, K. R. Mac-Kenzie, and E. Segre at the University of California. 

Most of the elements found in nature have several isotopes. Elements with atomic number 83 (bismuth) and lower have at least one stable isotope, although some are also radioactive and unstable. From element number 84 (polonium) and upwards, all the elements lack stable isotopes. The nine elements 84-92 are called naturally occurring radioactive elements. They are polonium, astatine, radon, francium, radium, actinium, thorium, protactinium and uranium. They are all treated in this chapter. There are also an additional two radioactive elements, number 43 technetium and 61 promethium. However, they have been described in Chapter 28 Technetium and Chapter 17 Rare earths, respectively. 

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