Search for K isomers in 252,254 No and 260 Sg and investigation of their nuclear structure

Study of K isomerism in the transfermium region around the deformed shells at N=152, Z=102, and N=162, Z=108 provides important information on the structure of heavy nuclei. Recent calculations suggest that the K-isomerism can enhance the stability of such nuclei against alpha emission and spontaneous fission. Nuclei showing K isomerism have neutron and proton orbitals with large spin projections on the symmetry axis which is due to multi quasiparticle states with aligned spins K. Quasi-particle states are formed by breaking pairs of nucleons and raising one or two nucleons in orbitals near the Fermi surface above the gap, forming high K (multi)quasi-particle states mainly at low excitation energies. Experimental examples are the recently studied two quasi-particle K isomers in 250,256-Fm, 254-No, and 270-Ds. Nuclei in this region, are produced with cross sections ranging from several nb up to µb, which are high enough for a detailed decay study. In this work, K isomerism in Sg and No isotopes was studied at the velocity filter SHIP of GSI, Darmstadt. The data were obtained by using a new data acquisition system which was developed and installed during this work. 252,254-No and 260-Sg were produced in fusion evaporation reactions of 48-Ca and 54-Cr projectiles with 206,208-Pb targets at beam energies close to the Coulomb barrier. A new K isomer was discovered in 252-No at excitation energy of 1.25 MeV, which decays to the ground state rotational band via gamma emission. It has a half-life of about 100 ms. The population of the isomeric state was about 20% of the ground state population. Detailed investigations were performed on 254-No in which two isomeric states (275 ms and 198 µs) were already discovered by R.-D. Herzberg, but due to the higher number of observed gamma decays more detailed information about the decay path of the isomers was obtained in the present work. In 260-Sg, we observed no statistically significant component with a half life different from that of the ground state. A comparison between experimental results and theoretical calculations of the single particle energies shows a fair agreement. The structure of the here studied nuclei is in particular important as single particle levels are involved which are relevant for the next shell closure expected to form the region of the shell stabilized superheavy elements at proton numbers 114, 120, or 126 and neutron number 184. K isomers, in particular, could be an ideal tool for the synthesis and study of these isotopes due to enhanced spontaneous fission life times which could result in higher alpha to spontaneous fission branching ratios and longer half lifes.

Bestimmung der Analysierstärke des A4-Compton-Rückstreupolarimeters zur Messung der longitudinalen Spinpolarisation des MAMI-Elektronenstrahls

Das A4-Experiment bestimmt den Beitrag der Strangequarks zu den elektromagnetischen Formfaktoren des Nukleons durch Messung der Paritätsverletzung in der elastischen Elektron-Nukleon-Streuung. Diese Messungen werden mit dem spinpolarisierten Elektronenstrahl des Mainzer Mikrotrons (MAMI) bei Strahlenergien zwischen 315 und 1508 MeV ndurchgeführt. Die Bestimmung des Strahlpolarisationsgrades ist für die Analyse der Daten unerläßlich, um die physikalische Asymmetrie aus der gemessenen paritätsverletzenden Asymmetrie extrahieren zu können. Aus diesem Grund wird von der A4-Kollaboration ein neuartiges Compton-Laserrückstreupolarimeter entwickelt, das eine zerstörungsfreie Messung der Strahlpolarisation, parallel zum laufenden Paritätsexperiment erlaubt. Um den zuverlässigen Dauerbetrieb des Polarimeters zu ermöglichen, wurde das Polarimeter im Rahmen dieser Arbeit weiterentwickelt. Das Datenerfassungssystem für Photonen- und Elektronendetektor wurde neu aufgebaut und im Hinblick auf die Verarbeitung hoher Raten optimiert. Zum Nachweis der rückgestreuten Photonen wurde ein neuartiger Detektor (LYSO) in Betrieb genommen. Darüber hinaus wurden GEANT4-Simulationen der Detektoren durchgeführt und eine Analyseumgebung für die Extraktion von Comptonasymmetrien aus den Rückstreudaten entwickelt. Das Analyseverfahren nutzt die Möglichkeit, die rückgestreuten Photonen durch koinzidente Detektion der gestreuten Elektronen energiemarkiert nachzuweisen (Tagging). Durch die von der Energiemarkierung eingeführte differentielle Energieskala wird somit eine präzise Bestimmung der Analysierstärke möglich. In der vorliegenden Arbeit wurde die Analysierstärke des Polarimeters bestimmt, so daß nun das Produkt von Elektronen- und Laserstrahlpolarisation bei einem Strahlstrom von 20 muA, parallel zum laufenden Paritätsexperiment, mit einer statistischen Genauigkeit von 1% in 24 Stunden bei 855 MeV bzw. <1% in 12 Stunden bei 1508 MeV gemessen werden kann. In Kombination mit der Bestimmung der Laserpolarisation in einer parallelen Arbeit (Y. Imai) auf 1% kann die statistische Unsicherheit der Strahlpolarisation im A4-Experiment von zuvor 5% auf nun 1,5% bei 1508MeV verringert werden. Für die Daten zur Messung der paritätsverletzenden Elektronenstreuung bei einem Viererimpulsübertrag von $Q^2=0,6 (GeV/c)^2$ beträgt die Rohasymmetrie beim derzeitigen Stand der Analyse $A_{PV}^{Roh} = ( -20,0 pm 0,9_{stat} ) cdot 10^{-6}$. Für eine Strahlpolarisation von 80% erhält man einen Gesamtfehler von $1,68 cdot 10^{-6}$ für $Delta P_e/P_e = 5 %$. Als Ergebnis dieser Arbeit wird sich dieser Fehler durch Analyse der Daten des Compton-Laserrückstreupolarimeters um 29% auf $1,19 cdot 10^{-6}$ ($Delta P_e/P_e = 1,5 %$) verringern lassen.

Palaeo wind system reconstruction of the last glacial period over Europe, using high resolution proxy data and model-data-comparison

The atmosphere is a global influence on the movement of heat and humidity between the continents, and thus significantly affects climate variability. Information about atmospheric circulation are of major importance for the understanding of different climatic conditions. Dust deposits from maar lakes and dry maars from the Eifel Volcanic Field (Germany) are therefore used as proxy data for the reconstruction of past aeolian dynamics.rnrnIn this thesis past two sediment cores from the Eifel region are examined: the core SM3 from Lake Schalkenmehren and the core DE3 from the Dehner dry maar. Both cores contain the tephra of the Laacher See eruption, which is dated to 12,900 before present. Taken together the cores cover the last 60,000 years: SM3 the Holocene and DE3 the marine isotope stages MIS-3 and MIS-2, respectively. The frequencies of glacial dust storm events and their paleo wind direction are detected by high resolution grain size and provenance analysis of the lake sediments. Therefore two different methods are applied: geochemical measurements of the sediment using µXRF-scanning and the particle analysis method RADIUS (rapid particle analysis of digital images by ultra-high-resolution scanning of thin sections).rnIt is shown that single dust layers in the lake sediment are characterized by an increased content of aeolian transported carbonate particles. The limestone-bearing Eifel-North-South zone is the most likely source for the carbonate rich aeolian dust in the lake sediments of the Dehner dry maar. The dry maar is located on the western side of the Eifel-North-South zone. Thus, carbonate rich aeolian sediment is most likely to be transported towards the Dehner dry maar within easterly winds. A methodology is developed which limits the detection to the aeolian transported carbonate particles in the sediment, the RADIUS-carbonate module.rnrnIn summary, during the marine isotope stage MIS-3 the storm frequency and the east wind frequency are both increased in comparison to MIS-2. These results leads to the suggestion that atmospheric circulation was affected by more turbulent conditions during MIS-3 in comparison to the more stable atmospheric circulation during the full glacial conditions of MIS-2.rnThe results of the investigations of the dust records are finally evaluated in relation a study of atmospheric general circulation models for a comprehensive interpretation. Here, AGCM experiments (ECHAM3 and ECHAM4) with different prescribed SST patterns are used to develop a synoptic interpretation of long-persisting east wind conditions and of east wind storm events, which are suggested to lead to an enhanced accumulation of sediment being transported by easterly winds to the proxy site of the Dehner dry maar.rnrnThe basic observations made on the proxy record are also illustrated in the 10 m-wind vectors in the different model experiments under glacial conditions with different prescribed sea surface temperature patterns. Furthermore, the analysis of long-persisting east wind conditions in the AGCM data shows a stronger seasonality under glacial conditions: all the different experiments are characterized by an increase of the relative importance of the LEWIC during spring and summer. The different glacial experiments consistently show a shift from a long-lasting high over the Baltic Sea towards the NW, directly above the Scandinavian Ice Sheet, together with contemporary enhanced westerly circulation over the North Atlantic.rnrnThis thesis is a comprehensive analysis of atmospheric circulation patterns during the last glacial period. It has been possible to reconstruct important elements of the glacial paleo climate in Central Europe. While the proxy data from sediment cores lead to a binary signal of the wind direction changes (east versus west wind), a synoptic interpretation using atmospheric circulation models is successful. This shows a possible distribution of high and low pressure areas and thus the direction and strength of wind fields which have the capacity to transport dust. In conclusion, the combination of numerical models, to enhance understanding of processes in the climate system, with proxy data from the environmental record is the key to a comprehensive approach to paleo climatic reconstruction.rn