Chemical Identification of Dubnium as a Decay Product of Element 115

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UCRL-CONF-217831 Chemical Identification of Dubnium as a Decay Product of Element 115 D. A. Shaughnessy, J. M. Kenneally, K. J. Moody, J. H. Landrum, P. A. Wilk, M. A. Stoyer, N. J. Stoyer, J. F. Wild December 20, 2005 Pacifichem 2005 Honolulu, HI, United States December 15, 2005 through December 20, 2005

Disclaimer This document was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor the University of California nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or the University of California. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or the University of California, and shall not be used for advertising or product endorsement purposes.

Chemical Identification of Dubnium as a Decay Product of Element 115 Dawn A. Shaughnessy, Jacqueline M. Kenneally, Kenton J. Moody, Jerry H. Landrum, Philip A. Wilk, Mark A. Stoyer, Nancy J. Stoyer, and John F. Wild Chemical Biology and Nuclear Science Division Lawrence Livermore National Laboratory Pacifichem 2005 Honolulu, HI, December 18, 2005

Nuclear chemistry experiments are a (huge) international team effort Joint Institute for Nuclear Research, Dubna, Russia Yu. Ts. Oganessian, V. K. Utyonkov, Yu. V. Lobanov, F. Sh. Abdullin, A. N. Polyakov, I. V. Shirokovsky, Yu. S. Tsyganov, G. G. Gulbekian, S. L. Bogomolov, B. N. Gikal, A. N. Mezentsev, S. Iliev, V. G. Subbotin, A. M. Sukhov, A. A. Voinov, G. V. Buklanov, K. Subotic, V. I. Zagrebaev, S. N. Dmitriev, S. V. Shishkin, A. V. Yeremin, V. I. Chepygin, E. A. Sokol, G. K. Vostokin, N. V. Aksenov, M. Hussonnois and M. G. Itkis LLNL K. J. Moody, J. M. Kenneally, J. Landrum, R. W. Lougheed, D. A. Shaughnessy, M. A. Stoyer, N. J. Stoyer, J. F. Wild and P. A. Wilk Paul Scherrer Institute, Villigen, Switzerland D. Schumann, H. Bruchertseifer, R. Eichler, B. Eichler and H. W. Gaeggeler

The discovery of heavy elements helps to answer fundamental physics questions The Liquid Drop Model successfully explains gross nuclear properties, but does not account for extra stability associated with magic numbers of protons or neutrons Magic numbers arise from second-order particle-particle interactions, resulting in shell structure in the level spacing of protons and neutrons (analogous to closed electronic shells) The magic numbers (so far) are 2, 8, 20, 28, 50, 82 and 126 Magic and doubly-magic nuclei are more stable (resistant to decay) than their surrounding neighbors Elements with magic numbers of protons have more stable isotopes (e.g., Sn has 10) Doubly magic 132 Sn drives spontaneous fission toward asymmetric fission fragments Calculating the next magic numbers remains a challenge for theorists!

Experimental data is needed to validate model calculations With increasing nuclear charge, decay by alpha emission becomes favored over decay by spontaneous fission as one approaches the vicinity of the closed nuclear shells The signature of the decay of a superheavy nucleus is a series of alpha decays followed by a spontaneous fission The heaviest known nuclei (circa 1998) superimposed on the calculated shell corrections to the liquid drop model

The most current theories place the next magic numbers at Z=114, N=184 Half-lives of these magic nuclei could be from seconds to days (model dependent) Current experiments are designed to try and identify the next magic numbers - the Island of Stability

Experiments are performed at the Flerov Lab of Nuclear Reactions at JINR, Dubna, Russia 48 Ca 5+ beam supplied by the U400 Cyclotron with high intensities Total beam dose over the course of an experiment is ~10 18 particles Dubna Gas-Filled Recoil Separator (DGFRS) Thin (0.35 mg/cm 2 ) rotating actinide oxide targets electroplated onto 1.5- µm Ti backing DGFRS suppression factors are >10 15 and >10 4 for beam- and targetlike particles, respectively Transmission Efficiency = 35 40 % for Z = 114 116 nuclei

Heavy element production and detection unique decay signatures actinide target 48 Ca 5+ projectile compound nucleus evaporation residue (EVR) + + neutrons or charged particles fission products Position-sensitive silicon detector array 293 116 10.55 MeV 61 ms 296 116* 289 114 9.82 MeV 2.6 s 1. EVR is implanted in the detector after separation from background products 281 Ds 285 112 9.15 MeV 29 s 2. After evaporation of 3-4 neutrons, the nucleus undergoes successive alpha decays on a very short time scale alpha particle efficiency = 87% coincident fission fragment efficiency = 45% SF 11.1 s 3. The last nucleus in the decay chain undergoes spontaneous fission

Chart of the nuclides 2004 hot fusion cold fusion

Elements 113 and 115 (2003) continue to map the neutron-deficient side of the Island of Stability 48 Ca + 243 Am 291 115*, 243 Am (99.9%) = 0.360 mg/cm 2 8.6 10 18 48 Ca ions total, beam energies = 248 and 253 MeV Production cross section ( 288 115) 2.7 pb Two new isotopic chains and two very longlived dubnium isotopes observed

The long-lived Dubnium (105) isotopes allow us to perform chemistry Understanding the chemical properties of the elements is the most basic problem of chemistry. Relativistic effects in the heavy elements dominate even in the valence orbitals Simple extrapolation of periodic trends may not be valid. These effects can change the shape and energy of the electronic orbitals, affecting the chemical properties of the element. Data is required to validate models that predict the chemical properties of the transactinides. Knowledge of transactinide chemical properties helps in interpreting chemical properties throughout the periodic table. Isolating the 268 Db daughter offers independent proof of the production of 288 115.

First attempt to identify the long-lived 288 115 decay daughter 268 Db (t 1/2 16 hours) 48 Ca 243 Am 288 115 Cu catcher block (2.5 7.5) x 10 17 ions 24 hour irradiations 1 mg/cm 2 3 n Chemistry was developed and performed by D. Schumann of PSI Once collected in the Cu block, 288 115 undergoes five alpha decays to 268 Db The surface (10 µm) of the Cu block is shaved and dissolved in aqua regia. Several tracers ( 177 Ta, 175 Hf, 92m Nb, 89 Zr, 88 Y), La carrier, and NH 4 OH are added. Cu remains in solution, +3, +4 and +5 ions are carried with La(OH) 3 precipitate Precipitate is washed and dissolved in HCl Solution is converted to nitrate form and loaded onto AG 50W-X8 cation exchange resin (nitrate form). Group IV and V are eluted together with 2M HF +3 ions (actinides) remain on the column (no 88 Y detected in eluant) Sample is dried on thin polyethylene foil and counted Solid state detectors surrounded by neutron detectors look for coincident fission fragments and number of neutrons emitted per fission Nb(V) yield 80%, Zr(IV) yield 60%

Results from the first 268 Db chemistry Separation method Separation efficiency Detection method 48 Ca beam energy 48 Ca total beam dose 243 Am target thickness Number of SF events Cross section (Z=115) Half-life (Z=105) TKE of SF fragments DGFRS Experiment (2003) Kinematic separator 35% Decay chains of Z=115 nuclei 246 MeV 4.5 x 10 18 0.36 mg/cm 2 3 2.7 (+4.8/-1.6) pb 16 (+19/-6) h 225 MeV Chemical Experiment (2004) Radiochemical separation 80% SF of Z=105 nuclei 247 MeV 3.4 x 10 18 1.2 mg/cm 2 15 4.2 (+1.6/-1.2) pb 32 (+11/-7) h 230 MeV, <v> = 4.2 But more work needs to be done: This experiment proves the fission events come from the +4/+5 chemical fraction The +4 and +5 ions should be separated to prove the fission events come from 268 Db The +5 ions could also be separated from each other to show the chemical behavior of element 105 as either more Nb-like or more Ta-like

LLNL has developed a new group IV/V separation (deployed in Dubna earlier this month!) Step 1 Lanthanide precipitates to remove copper from the catcher and separate +4 and +5 fractions Using radiotracers of 233 Pa, 95 Zr, 95 Nb and 182 Ta Add H 3 BO 3 and several carriers La 3+ (1mg), Nb 5+ (1µg), Ta 5+ (1µg), and Zr 4+ (10µg) Precipitate La(OH) 3 with excess NH 4 OH in a hot H 2 O bath All tracers carry down with the precipitate Cu left in the supernatant Dissolve precipitate in HCl and repeat Dissolve final La(OH) 3 precipitate in conc. HCl Add H 2 O and conc. HF to form LaF 3 precipitate Distribution of activities in the solid and aqueous phases: Pa Zr Nb Ta LaF 3 ppt. 98.5% 97.5% 11.2% 8.8% F - super. 1.5% 2.5% 88.8% 91.2%

Group IV/V separation continued Step 2 Separate Nb and Ta Fractions using a reverse phase column separation Supernatant from step 1 (6N HCl : 6N HF) is loaded onto a small (2mm inner diameter) Kel-F inert support column pre-conditioned with methyl isobutyl ketone (MIBK) Kel-F is a fluorocarbon-based polymer similar to Teflon made from PolyChloroTriFluoroEthylene (PCTFE) Nb and Ta are eluted separately using HCl:HF and water in a gradient elution Kel-F Reverse Phase MIBK HCl:HF Eluant Total Volume Added (µl) Elements Eluted Tracer Activity 400 350 300 250 200 150 100 50 0 Pa233 Zr95 Nb95 Ta182 6N HCl : 6N HF 3N HCl : 1N HF 1.5N HCl : 0.5N HF 400 200 300 Any residual Pa, Zr not removed by LaF 3 ppt. Any remaining Pa Nb 1 2 3 4 5 6 7 8 9 10 11 12 13 Column Fraction H 2 O 1400 Ta

Group IV/V separation continued Step 3 Separate Zr and Pa fractions from the LaF 3 precipitate formed in step 1 Dissolve LaF 3 in boric acid and conc. HCl Add Sc carrier and NH 4 OH to form La(OH) 3 precipitate Dissolve precipitate in conc. HCl and load onto a 2mm i.d. Dowex 1x8 anion resin column Remove Sc, La, actinides and RE contaminants with conc. HCl Elute Zr and Pa using a gradient elution 600 Dowex 1X8 Eluant Total Volume Added (µl) Elements Eluted Tracer Activity 500 400 300 200 100 Pa233 Zr95 12N HCl 5N HCl 1900 2500 Sc, La, actinides, rare earths, minor Zr (~ 20%) Zr 0 1 3 5 7 9 11 13 15 17 19 21 Column Fraction 2N HCl 5500 Pa

Summary and future work The first attempt to identify the long-lived dubnium daughter of element 115 was successful although some questions remained New chemistry was developed at LLNL to separate the Group IV and V fractions and to isolate the individual Group V elements Learn something about the chemical properties of element 105 in this system does it behave more like Nb, Ta or Pa? Chemistry of element 105 was repeated this month in Dubna In addition to element 105 chemistry, we are currently working on an automated chemistry apparatus for element 114 chemistry experiments

Acknowledgements Russian Foundation for Basic Research under grant # 96-02- 17377 INTAS grant # 96-662 U.S. DOE under Contract # W- 7405-Eng-48 by UC, LLNL 243 Am, 244 Pu, and 248 Cm provided by U.S. DOE through the REDC facility at ORNL 242 Pu and 245 Cm provided by the isotope production facilities at Dmitrograd Work performed in the framework of the Russian Federation/U.S. Joint Coordinating Committee for Research on the Fundamental Properties of Matter