The New Element Berkelium (Atomic Number 9'7)*
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NEW ELE MENT BE RKELI U M 781 From peak XI in Fig. 6 and IX in Fig. 7, which are V. CONCLUSION due to the elastic scattering of alpha-particles from The 1.0-Mev level in C" has been conlrmed, and a gold, it was found necessary to modify the range-energy new level at 6.8 Mev has been determined. The proton of Lattes' Other evidence as to curve at higher energies. group giving rise to the 1.0-Mev level is small statis- alpha-alpha-bom- a need for modification came from an tically, consisting of only approximately 11 tracks at bardment when the recoil.ing and scattered particles 115', yet this number is large compared to the expected were recorded at small angles. The observed ranges fell background at this range and is an appreciable fraction short of the predicted ranges when Lattes' curve was of the 33 proton tracks observed which resulted from used. This was true for the three aforementioned cases C" in the ground state. A level in C" at 3.58 Mev has even after all possible corrections were made. If the been found at 90' but the results are doubtful because beam energy were lower than 20 Mev, i.e., 17.5 Mev, of non-appearance at 115' and 155' or under alpha- then XI in Fig. 6 and IX in Fig. 7 would be correctly particle bombardment. The relative scattering of deu- identi6ed but then the other in 6 and 7 peaks Figs. terons and alpha-particles from nuclei in the ground would be displaced too far to the right. Therefore it was state and in the various nuclear energy levels are illus- assumed that the bombarding energy was 20 Mev, that trated. The results indicate that 10-Mev deuterons are the lower portion of the alpha-energy range curve, more effective in studying energy levels than are 20-Mev below 10 Mev, was correct, but that above 10 Mev a the modification was necessary. This modification was alpha-particles. Finally alpha-particle range-energy Ilford E-1 nuclear has made from the proton range-energy curve by assuming curve, as applied to emulsions, that an alpha-particle and a proton of the same velocity been modihed at higher energies for alpha-particles. have the same range. The corrected curve has already This author wishes to thank Messrs. Chia-Hua Chang been published. and Wen-Jsao Yang for their careful reading of the plates, and Dr. Robert N. Varney for his constructive g Lattes, Fowler, and Cuer, Proc. Phys. Soc. London 59, 883 (1947). criticism. P H YSI CAL R EVI EW VOLUME 80, NUMBER 5 DECEMBER 1, 1950 The New Element Berkelium (Atomic Number 9'7)* S. G. THoMPsoN, A. GHIoRso) AND G. T. SEABoRG Radiation Laboratory and Department of Chemistry, University of California, Berkeley, California (Received July 24, 1950) An isotope of the element with atomic number 97 has been discovered as a product of the helium ion bombardment of americium. This isotope decays with the emission of alpha-particles of maximum energy 6.72 Mev (30 percent) and it emits lower energy alpha-particles of energies 6.55 Mev (53 percent) and 6.20 Mev (17 percent). The half-life of this isotope is 4.6+0.2 hr. and it decays primarily by electron cap- ture with about 0.1 percent branching decay by alpha-particle emission. The mass number is probably 243 as indicated by chemical separation of the alpha-particle and electron-capture daughters. The name berkelium, symbol Bk, is proposed for element 97. The chemical separation of element 97 from the target material and other reaction products was made by combinations of precipitation and ion exchange adsorption methods making use of its anticipated (III) and (IV) oxidation states and its position as a member of the actinide transition series. The distinctive chemical properties made use of in its separation and the equally distinctive decay properties of the particular isotope constitute the principal evidence for the new element. The isotope Cm~~ is identified experimentally as a result of its production as a decay product of Bk'~. The Cm'~ decays by the emission of alpha-particles of maximum energy 5.89 Mev {15percent) and lower energy alpha-particles of energy 5.79 Mev (85 percent); the half-life for alpha-particle emission is estimated to be roughly 100 yr. I. INTRODUCTION Seaborg, James, and Morgan. ' The search for trans- curium elements was begun us in the fall of 1945. ~ 'HE transuranium elements numbers 96, curium, by It was anticipated' that element 97 as eka-terbium in and 95, americium, were discovered in 1944, the the actinide transition series would possess oxidation first by Seaborg, James, and Ghiorso, ' the second by states (III) and (IV) with properties similar to curium *This work was performed under the auspices of the AEC. in the (III) oxidation state and to plutonium (IV) in ' Seaborg, James, and Ghiorsor The Transuranium E/ements: Re- search Papers (McGraw-Hill Book Company, Inc., New York, ' Seaborg, James, and Morgan, National Nuclear Energy Series, 1949), Paper No. 22.2, National Nuclear Energy Series, Plutonium see reference 1, Paper No. 22.1. Project Record, Vol. 148. ' G. T. Seaborg, Nucleonics 5, No. 5, 16 (1949). THOM PSON, GH IORSO, AN D SEABORG its (IV) oxidation state. It was more diKcult to esti- prior to December, 1949, were unsuccessful for many mate the oxidation potential of the (III)~(IV) couple reasons which may be grouped into three classes. First, but it was expected. that element 97 would be somewhat the methods of predicting the properties of the new easier to oxidize than terbium (III) which is not oxidiz- isotopes were relatively undeveloped and the experi- able to higher states in aqueous solution at all. The ments were never done with sufhcient speed. The fur- salient point is that if element 97 could not be con- ther development of the alpha-decay systematics4 made verted to an oxidation state higher than (III) in solu- it possible to estimate energies and half-lives for alpha- tions it would be extremely dificult to separate in a particle decay. The resulting estimated alpha-particle short period of time from rare earth elements and from decay energies could be used in calculating by closed the actinide elements from which it would be produced. decay cycles the total energies for electron-capture Americium is very difFicult and curium probably im- decay or beta-particle decay. An empirical method of possible to oxidize above the (III) state in aqueous estimating electron-capture half-lives from disintegra- solution. ' In other words, it appeared that it might be tion energies was also developed' which, although very necessary to use tedious rare earth separations in order rough due to uncertainties in the degree of prohibition to separate and identify the new element, the isotopes of this mode of decay in any given case, was very useful of which do not exist in nature and whose neutron- in making half-life estimates. deficient isotopes as produced by alpha-particle and The second major difhculty was that of obtaining deuteron bombardments would have short half-lives as suQiciently large amounts of americium and curium as a result of considerable instability toward alpha-par- sources for the production of element 97. Eventually ticle emission and electron-capture decay. americium became available in milligram amounts In view of the fact that sufFiciently intense beams of through neutron irradiation of plutonium. The isola- energetic particles of nuclear charge greater than two tion of the americium from the plutonium required were not available at the time of this research, it is tedious chemical procedures. The curium was produced obvious that there were only two methods of approach in smaller amounts by the irradiation of americium with to the production of element 97. The first approach was neutrons. " through the bombardment of americium with helium The intense radioactivity of the americium and ions or the bombardment of curium with deuterons or curium source materials presented the third major helium ions. The second (not yet successful) was through difhculty. This radioactivity necessitated not only the intensive neutron irradiations of curium in order to design and development of advanced techniques and produce eventually through successive (n, y) reactions equipment' for its safe handling, but also made it a curium isotope of mass sufhcient to be unstable toward necessary to attain enormous separation factors in the negative beta-particle decay and so to produce an iso- isolation of the new element from the target material tope of element 97. in order to be able to detect the small amounts of radio- Both methods were employed in attempting to ob- activity due to it. Furthermore, this high degree of serve element 97 and for each, diBerent chemical pro- separation had to be carried out in good yield in a cedures were used. Some of these procedures were de- short length of time. signed to separate the new element in oxidation states Essentially three chemical steps were developed to greater than (III) and others were used on the assump- solve these chemical problems. The conversion of the tion that element 97 existed in solution under most americium to a hexapositive oxidation state' was used conditions in the tripositive oxidation state. in the rapid removal of the bulk of the bombarded Although the broad assumptions made when the americium. An ion exchange method involving the work was started were all correct, the experiments done separation of the actinide elements as a group from the rare earth 6ssion products by elution with concentrated HCl from a cation exchange column' was exploited for the rapid separation of the tripositive actinide ele- ments.