Andrassys, M.

Bruchertseifer, H.

Nitsche, H.

Novgorodov, A. F.

Schumann, D.

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Radiochimica Acta 79, 217 - 2 2 0 (1997) © R. Oldenbourg Verlag, München 1997 Sorption Behaviour of Uranium on Cation and Anion Exchange Resins from HCl/HF-Containing Aqueous Solutions: Model Experiments for the Determination of Chemical Properties of Element 106 (Seaborgium) By D. Schumann', M. AndrassyS H. Nitsche', A. F. Novgorodov^ and H. Bruchertseifer® ' Institut für Analytische Chemie, FG Radiochemie, Technische Universität Dresden, D-01062 Dresden, Germany ^ Joint Institute for Nuclear Research, Dubna, Russia ^ Paul-Scherrer Institut, Villigen, Switzerland (Received April 25, 1997; accepted in revised form July 1, 1997) Uranium / Ion exchange / HCl/HF solutions / Chemical properties of element 106 Summary ^"U was used for batch studies of its Sorption behaviour on DOWEX 50X8 and DOWEX 1X8 from diluted HCl/HF contain-ing Solution. It was shown that uranium remains, similar to sub-group IV Clements, completely on the cation exchanger in the concentration ränge of 1 0 " - l O ^ M HF and lO-^- l .OM HCl, whereas it is not at all sorbed on the anion exchanger. This be-haviour differs completely from that of tungsten and molyb-denum under similar conditions. With this chemical system it is possible to determine the chemical properties of element 106 (seaborgium) by comparing its Sorption behaviour on the cation exchanger with that of tungsten, molybdenum, and uranium. Introduction Batch experiments with carrier-free isotopes of sub-group IV, V and VI Clements showed that ion ex-change on cation exchange resins (e.g. DOWEX 50WX8 or AMINEX A6) from diluted HCl/HF-con-taining solutions are applicable for fast on-line experi-ments aiming to separate seaborgium. The suitable concentration interval for the Separation of the hexa-valent Clements tungsten and molybdenum from zir-conium, hafnium and lanthanides was found to be 0.05-0.1 M HCyi0"^-10^ M HF [1]. This chemical system was successfully applied in on-line experi-ments with short-hved tungsten, hafnium and lutetium isotopes [2]. On-line studies with and using the ARCA apparatus obtained similar results for HCl/HF and HNGj/HF-containing solutions [3]. A first Separation of seaborgium in aqueous Solu-tion with the ARCA III apparatus was carried out in 1995 at the UNILAC accelerator (GSI Darmstadt). In this experiment, 0.1 M HNOj/S X lO"'' M HF was used to adsorb element 104 and heavy actinides on the cat-ion exchanger AMINEX A6. Two decay chains corre-sponding to the decay of '^"'No were found in the aqueous phase. This clearly indicates that the 104 must come from the decay of seaborgium and is therefore proof for the presence of Sg in Solution. Ele-ment 104 that was produced during the production of seaborgium also is expected to be completely ad-sorbed on the cation exchanger under these conditions. This result is a first proof that element 106 behaves like its lighter homolog tungsten in solutions contain-ing HCl/HF or HNO3/HF [4]. However, due to relativistic effects, similarities of the chemical properties of the transactinide elements with the corresponding actinides can also be expected. It was shown that element 105 has similar properties to subgroup V elements [5—7] but also behaves some-times like Pa [8, 9]. Therefore, further chemical ex-periments with seaborgium should also consider the possibly uranium-like behaviour of this element. The Sorption behaviour of carrier-free uranium from di-luted HCl/HF or HNO3/HF solutions used in Üie ex-periments that were described above is yet unknown. To compare the chemical properties of seaborgium with those of uranium, we investigated the Sorption behaviour of '^^ U on cation and anion exchangers from HCITHF solutions under the conditions used in [1]. Our present experiments were carried out in "batch" modus where the experimental time is rather long in comparison to the reaction time. This method ensures that chemical equilibrium is being reached between the element and its reaction partners in Solution. A disad-vantage of our batch experiments is that the reaction time cannot be decreased below 5 min. Fast on-line separations require only less than one minute. They have to be tested with model elements in order to establish whether or not the reaction reaches equi-librium before the fast Separation is being carried out. Experimental Carrier-free ^^ U^ was obtained as a decay product of '^^ Pa (ß~\ Tia = 1.31 a), which was produced via the nuclear reaction "'Th(p,n)"^Pa(^-) in 1976 at the Phasotron "F" (Laboratory for Nuclear Problems, JINR, Dubna, Russia). After the complete decay of ^^ ^Pa, a pure product was obtained which contained 218 D. Schumann, M. Andrassy, H. Nitsche, A. F. Novgorodov and H. Bruchertseifer only ^^ ^U and its decay products. ^^ ^U decays via the following decay chain: 232U 228J1J ^ 224Ra 220Rjj ^ 216po o 6,y a, ß ß,a and its daughter products were separated im-mediately before the experiments by sorbing the ^^ U^ on DOWEX 1X8 from 9 M HCl Solution. ""^ Th passes through the column without sorption. The column was several times washed with 9 M HCl to remove all traces of thorium. '^^ U was eluted from the column with 2 M HCl. This stock Solution was diluted to the required HCl concentration as needed. For the batch experiments, 5 mL of the radioactive Solution were contacted for one hour with 200 mg of each ion exchange resin (DOWEX 50WX8, DOWEX 1X8, 20-50 mesh). Then the phases were separated. The distribution of ^^ U^ was determined by evaporat-ing 0.1 mL of the Solution before and after the experi-ment and measuring the a-activity (^'^U: E^ = 5139, 5263, 5329 keV, all daughter products in the decay chain have higher a energies) using a Si(Au) detector (12 cm^, resolution 35 keV). The distribution coefficients were calculated as reported previously [1, 10]. Results and discussion The suitable concentration interval of 0.05—0.1 M HCl/10-' '-10'M HF for the Separation of subgroup VI from subgroup IV elements on cation exchange re-sins was developed using molybdenum and tungsten, zirconium and hafnium, respectively, as model ele-ments [1]. Predictions of the sorption properties of ele-ments in ultra trace amounts are difficult because the tracers may behave very different than macroscopic amounts under identical conditions. Speciation calcu-lations using literature data for zirconium hydrolysis [11] and fluoride complexation [12] showed that ZrFl^ and ZrF^ are the main species in 0.05—0.1 M HCl/lO-'^-lO-^ M HF Solution [13], According to this speciation, the subgroup IV elements zirconium and hafnium should sorb on cation exchange resins, which we could recently confirm experimentally [1]. Literature data on complex stability constants of mononuclear complexes for subgroup VI elements are very sparse, so that no preliminary calculations can be done to determine the species for the conditions of interest. For uranium, however, the stability constants for the complexation with fluoride and chloride are well known [14], Fig. 1 shows the calculated composi-tion of uranium species as a function of the HF con-centration at several constant HCl concentrations. The following formation constants were used: IgA'i = 4.54, XgK^  = 3.34, Ig/i:, = 2.57 and lg^4 = 1-34 that are given by the NEA Thermodynamic Data Bank [14]. The cations UOi^ and UO2F+ are the main species between l O - ' - l O ^ ' M HF, and, therefore, should be 100n 90 80 70 o 60 2 c 50 o 40 ra E L— 30 o «4- 20 10 0 0.1 M HCl UO,F,(aq) TT, I n-T-r-rr 10"® lO"* lO"' 10"' HF concentration [mol L"^ ] 1 0 " ' Fig. 1. Formation ratios of U(VI) fluoride species as a function of HF concentration, [H^] = 0.1 M, no consideration of mixed-ligand Compounds. 0.1 M HCl Mo.D0WEX50xa • Mo.DOWEXIxS W. DOWEX50j«e O W, DOWEXIxa U, DOWEX S0j<8 A U. DOWEX 1*8 1E-5 0,01 c„HF Fig. 2. Distribution coefficients of U, W and Mo on DOWEX 50X8 and DOWEX 1X8 as a function of the HF concentration at 0.1 M HCl. adsorbed on cation exchangers. The calculations show that Chloride complexation plays only a minor role in this concentration ränge, and was therefore not consid-ered. Adsorption of uranium, tungsten and molybdenum on anion exchange resins from mixed HCl/HF solu-tions was studied by Kraus et al. [15, 16]. They found a minimum adsorption for uranium at a HCl concen-tration of 0.1 M at a constant HF concentration of 1.0 M. Only slight sorption of uranium was found with 0.1 M HCl/O.l M HF [17]. This means that in this con-centration ränge the formation of positively charged fluoride-containing complexes takes place, which are destroyed if the fluoride or chloride concentration in-creases and neutral and anionic complexes are formed. For molybdenum and tungsten, such a minimum in the adsorption behaviour exists only at high HCl concen-trations (2—8 M, [16]). Very diluted HF concentrations (<10"' M) have not been stodied at all. The experimentally determined sorption behaviour of uranium under the selected conditions can be seen in Fig. 2. The sorption of '^^ U on DOWEX 50X8 and Sorption Behaviour of Uranium on Cation and Anion Exchange Resins from HCl/HF-Containing Aqueous Solutions 219 DOWEX 1X8 is shown as a function of the HF con-centration at constant HCl concentrations of 0.1 M. To compare this behaviour with that of tungsten and molybdenum, their sorption behaviour is also depicted in this figure. These sorption studies were carried out earlier under the same conditions as the uranium study; the details of sample preparation and Perfor-mance were given earlier [1]. Uranium is sorbed onto the cation exchanger over a wide ränge of HF concen-trations. Only at HF concentrations higher than O.Ol M, desorption of uranium from the cation ex-change resin takes place. This behaviour confirms our calculations. On the anion exchanger, there is no sorp-tion up to HF concentrations of O.Ol M, then slight sorption begins. These results confirm the values of Faris et al. [17] and also expand the knowledge about the chemical properties at concentration ranges be-tween 10'® and 0.1 M HF. The sorption behaviour of molybdenum and tung-sten completely differs from that of uranium on both the cation and the anion exchange resins. This is prob-ably due to the different electronic structure of the ura-nyl ion in comparison with molybdenum and tungsten Compounds. Available f-orbitals lead to a linear geo-metry of the O-U-0 group. Due to participation of n-bonding the bonding length is very short. The conse-quence is very strong bonding of the oxygen atoms and high stability of the UOr-group [18]. Such a structure cannot be explained with pure d-orbital bond-ing and is not known for tungsten and molybdenum. The absence of a dipol moment and the more basic character of the uranyl ion due to its larger ionic ra-dius, in comparison to tungsten and molybdenum, re-sult in a low tendency to hydrolyze. Because of this, for instance, anions of the form MO^ are not known for uranium. This higher stability of cationic uranium species is the reason for its stronger sorption on cation exchangers in comparison to tungsten and molyb-denum. To further study the chemical properties of trace amounts of uranium in this system, we determined lg D values on DOWEX 50X8 and on DOWEX 1X8 in dependence on the HCl concentration at constant HF concentrations of 10"" M and 10"' M, respectively (Fig. 3). Desorption of uranium from the cation ex-changer takes only place at HCl concentrations above 0.5 M. Simultaneously the sorption onto the anion ex-changer increases, which is due to the formation of negatively charged Chloride complexes at high HCl concentrations. This also agrees very well with litera-ture data [16]. We reported the behaviour of tungsten and molybdenum under these conditions earlier [1]. Their adsorption on both the cation and the anion ex-changer differs completely from that of uranium over a Wide ränge of HCl concentrations. Pershina et al. [19] predicted on the basis of DS DVM calculations analog behaviour between seabor-gium and molybdenum and tungsten, and no simi-larities with uranium. Our experimental results on the sorption behaviour of uranium in diluted HCl/HF sys-c„HCI Fig. 3. Distribution coefficients of U on DOWEX 50X8 and DOWEX 1X8 as a function of the HCl concentration at 1.0X 10"" M HF and I .OXIO- 'MHR tems confirm this assumption. From the results on the sorption behaviour of seaborgium in 0.1 M HNO3/ 5 X 10"" M HF [4] follows that it is a typical member of subgroup VI and does not behave like the pseudo-homolog uranium. Summary Batch studies with '^^ U showed that in the concen-tration intervals 10""-10" 'M HF and 10"^-1.0M HCl uranium is completely adsorbed onto the strongly acid cation exchanger DOWEX 50X8 in contrast to molybdenum and tungsten that show completely dif-ferent sorption properties under these conditions [1]. Since seaborgium could be successfully separated from a similar Solution [4], we concluded that it be-haves like its lighter homologs tungsten and molyb-denum and not like the pseudohomolog uranium. Therefore, the system is not only well-suited for the Separation and Identification of seaborgium but also for the determination of its chemical properties. Under some conditions even mngsten and molybdenum show slight different sorption properties on DOWEX 50X8 in these solutions [1]. This should open the possibility to distinguish also between a tungsten or molybdenum like behaviour of seaborgium, if conditions could be found under which the sorption of these two elements completely differs from each other. References 1. Schumann, D., Fischer, S., Dressler, R., Taut, St., Kitsche, H., Trautmann, N., Schädel, M., Brüchle, W, Schausten, B., Novgorodov, A. F., Misiak, R., Eichler, B., Gäggeler, H., Jost, D., Türler, A., Bruchertseifer, H., Radiochim: Acta 72, 137 (1996). 2. Schumann, D., Dressler, R., Fischer, S., Taut, St., Binder, R., Szeglowski, Z., Kubica, B., Guseva, L. I., Tikhomirova, G. S., Constantinescu, M., Domanov, V. R, Constantinescu, M., Dinh Thi Lien, Oganessian, Yu. Ts., Brudanin, V. B., Bruchertseifer, H.: Radiochim. Acta 69, 135 (1995). 3. Günther, R., Paulus, W., Posledni, A., Kratz, J. V., Schädel, M., Brüchle, W., Jäger, E., Schimpf, E., Schausten, B., Schumann, D., Binder, R. GSI-Scientific Report 1994, p. 302. 220 D. Schumann, M. Andrassy, H. Nitsche, A. F. Novgorodov and H. Bruchertseifer 4. Schädel, M., Alstad, J., Andrassy, M., Brüchle, W., Dressler, R., Eberhardt, K., Eichler, B., Fricke, B., Gäggeler, H. W., Gärtner, M., Günther, R., Gregorich, K. E., Heimann, R., Hoffman, D. C., Hübener, S., Jäger, E., Jost, D. T., Kadkho-dayan, B., Kratz, J. V, Lee, D. M., Malmbeck, R., Mendel, M., Misiak, R., Nähler, A., Nagame, Y, Omtvedt, J. R, Oura, Y, Paulus, W., Pershina, V., Rocker, F , Schausten, B., Schimpf, E., Schumann, D., Seibert, A., Skamemark, G., Sylvester, E., Taut, St., Timokhin, S., Tharun, U., Thörle, R, Trautmann, N., Tiirler, A., Wiehl, N., Wierczinski, B., Wirth, G., Yakuschew, A., Zauner, S.: Chemistry with El-ement 106, Seaborgium - The Isotopes ^«Sg and ^''Sg, GSI Scienüfic Report 1995, May 1996, S. 10. 5. Kratz, J. V., Zimmermann, H. R, Scherer, U. W., Schädel, M., Brüchle, W., Gregorich, K. E., Gannett, C. M., Hall, H. L., Henderson, R. A., Lee, D. M., Leyba, J. D., Nurmia, M. J., Gäggeler, H., Jost, D., Baltensperger, U., Ya Nai-Qi, Türler, A., Lienen, Ch.: Radiochim. Acta 48, 121 (1989). 6. Gäggeler, H., Jost, D., Kovacs, J., Scherer, U. W., Weber, A., Vermeulen, D., Türler, A., Gregorich, K. E., Henderson, R. A., Czerwinski, K. R., Kadkhodayan, B., Lee, D. M., Nurmia, M. J., Hoffmann, D. C., Kratz, J. V., Gober, M. K., Zimmermann, H. P., Schädel, M., Brüchle, W, Schimpf, E., Zvara, L: Radiochim. Acta 57, 93 (1992). 7. Schädel, M., Brüchle, W, Schimpf, E., Zimmermann, H. R, Gober, M. K., Kratz, J. V., Trautmann, N., Gäggeler, H., Jost, D., Kovacs, J., Scherer, U. W., Weber, A., Gregorich, K. E., Türler, A., Czerwinski, K. R., Hannick, N. J., Kadkh-odayan, B., Lee, D. M., Nurmia, M. J., Hoffman, D. C.: Radiochim. Acta 57, 85 (1992). 8. Gregorich, K. E., Henderson, R. A., Lee, D. M., Nurmia, M. J., Chasteler, R. M., Hall, H. L., Bennett, D. A., Gannett, C. M., Chadwick, R. B., Leyba, J. D., Herrmann, G., Hoff-man, D. C.: Radiochim. Acta 43, 223 (1988). 9. Zimmermann, H. R, Kratz, J. V, Gober, M. K., Schädel, M., Brüchle, W., Schimpf, E., Gregorich, K. E., Türler, A., Czerwinski, K. R., Hanninck, N. J., Kadkhodayan, B., Lee, D. M., Nurmia, M. J., Hoffman, D. C., Gäggeler, H., Jost, D., Kovacs, J., Scherer, U. W., Weber, A.: Radiochim. Acta 60, 11 (1993). 10. Schumann, D., Fischer, S., Taut, St., Novgorodov, A. F., Misiak, R., Lebedev, N. A., Bruchertseifer, H.: J. Radioanal. Nucl. Chem. Lett. 187, 9 (1994). 11. Baes, C. F., Mesmer, R. E.: The Hydrolysis ofCations, John Wiley and Sons, New York 1976, p. 412. 12. Sillen, L. G., Martell, A. E.: Stability Constants of Metal-lon Complexes, Burlington House, London 1971. 13. Taut, St.: Ph D. Thesis, „Computergestützte Elektromigra-tions- und lonenaustauschexperimente", TU Dresden, Dres-den 1993. 14. Grenthe, I., Fuger, J., Konings, R. J. M., Lemire, R. J., Mül-ler, A. B., Chinh Nguyen-Trung Cregu, Wanner, H.: NEA-TDB, Chemical Thermodynamics of Uranium, 1992, OECD Nuclear Energy Agency, Databank. 15. Kraus, K. A., Nelson, F : ASTM Spec. Tech. Publ. No. 195, 27 (1958). 16. Kraus, K. A., Nelson, F., Moore, G. E.: J. Am. Chem. Soc. 77, 3972 (1955). 17. Faris, J. R: ANL-78-78 (1978) 1/34. 18. Connick, R. E., Hugus, Z. Z.: J. Am. Chem. Soc. 74, 6012 (1952). 19. Pershina, V., Fricke, B.: Complex Formation of Element 106 in Aqueous HCl and HCl + HF Solutions. GSI-Scien-tific Report 1995, p. 14. 

Sorption Behaviour of Uranium on Cation and Anion Exchange Resins from HCl/HF-Containing Aqueous Solutions: Model Experiments for the Determination of Chemical Properties of Element 106 (Seaborgium)

Sorption Behaviour of Uranium on Cation and Anion Exchange Resins from HCl/HF-Containing Aqueous Solutions: Model Experiments for the Determination of Chemical Properties of Element 106 (Seaborgium)

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