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Showing 1 to 10 of 10 (0.051 seconds)Spelling suggestions: "subject:"radioactive isotope""
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Comparison of tumor localizing properties of COBALT-57 bleomycin and four analogues: bleomycinic acid, phleomycin, pepleomycin and tallysomycinHall, Jack Norman January 1981 (has links)
No description available.
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Estudo do espalhamento elástico dos isótopos 7Be, 9Be e 10Be em alvo de 12C / Study of elastic scattering of the isotopes 7Be, 9Be and 10Be on 12C targetCardona, Juan Carlos Zamora 18 May 2011 (has links)
Nesse trabalho medimos e analisamos distribuições angulares do espalhamento elástico para os isótopos 7Be, 9Be e 10Be em alvo de 12C. A distribuição do 7Be foi medida a uma energia de 18.8 MeV, em dois laboratórios, com o sistema TWINSOL, na Universidade de Notre dame, e com o sistema RIBRAS, na Universidade de São Paulo, onde foi completada a distribuição angular. As distribuições para o 9Be e 10Be foram medidas completamente no sistema RIBRAS, em energias de 26.0 e 23.2 MeV, respectivamente. Cada uma dessas distribuições angulares foi analisada considerando no modelo ótico e também o formalismo dos canais acoplados. Testamos múltiplos potenciais óticos em cada distribui9ção, com a finalidade de descrever a seção de choque elástica de cada sistema. Para os sistemas que envolvem núcleos fracamente ligados (7Be, 9Be e 8B) foram feitos cálculos com acoplamento do contínuo (CDCC), enquanto que para o núcleo 10Be, que é fortemente ligado, acoplamos os dois primeiros estados ligados. Também, a partir da análise de cada uma das distribuições elásticas, foi possível obter a seção total de reação, que foi comparada sistematicamente com outros núcleos leves espalhados em carbono. Dessa análise foi possível concluir que o canal do break up Coulombiano, nesses sistemas leves, não é fortemente influente na seção de choque total de reação, o que implica que a interação entre alvo e projétil é dominada pelo potencial nuclear. / In the present work, we measured elastic scattering angular distributions for teh isotopes 7Be, 9Be and 10Be on 12C target. The angular distribution of 7Be at 18.8 MeV, was measured in two laboratories, with the TWINSOL system, in Notre Dame University, and the RIBRAS system, in São Paulo University, where the angular distribution was completed. The angular distribution for 9Be and 10Be isotopes measured completely in the RIBRAS system at 26.0 and 23.2 MeV, respectively. All angular distribution were analized considering optical model and coupled channel formalism. We tested multiple optical potentials on each distribution to describe the elastic cross section for these systems. For the weakly bound projectiles (7Be, 9Be and 8B)calculations with continous coupling (CDCC) were performed, while for the 10Be nucleus, which is tghtly bound nucleus, we coupled the first two bound states. We also performed a systematic analysis of the total reaction cross section obtained from elastic scattering distribution of several light particles on 12C. From this analysis, we concluded that the Coulomb break up channel, in these light systems, does not have a strong influence on the total reaction cross section, what implies that the projetile-target interaction is dominated by the nuclear potential.
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Estudo do espalhamento elástico dos isótopos 7Be, 9Be e 10Be em alvo de 12C / Study of elastic scattering of the isotopes 7Be, 9Be and 10Be on 12C targetJuan Carlos Zamora Cardona 18 May 2011 (has links)
Nesse trabalho medimos e analisamos distribuições angulares do espalhamento elástico para os isótopos 7Be, 9Be e 10Be em alvo de 12C. A distribuição do 7Be foi medida a uma energia de 18.8 MeV, em dois laboratórios, com o sistema TWINSOL, na Universidade de Notre dame, e com o sistema RIBRAS, na Universidade de São Paulo, onde foi completada a distribuição angular. As distribuições para o 9Be e 10Be foram medidas completamente no sistema RIBRAS, em energias de 26.0 e 23.2 MeV, respectivamente. Cada uma dessas distribuições angulares foi analisada considerando no modelo ótico e também o formalismo dos canais acoplados. Testamos múltiplos potenciais óticos em cada distribui9ção, com a finalidade de descrever a seção de choque elástica de cada sistema. Para os sistemas que envolvem núcleos fracamente ligados (7Be, 9Be e 8B) foram feitos cálculos com acoplamento do contínuo (CDCC), enquanto que para o núcleo 10Be, que é fortemente ligado, acoplamos os dois primeiros estados ligados. Também, a partir da análise de cada uma das distribuições elásticas, foi possível obter a seção total de reação, que foi comparada sistematicamente com outros núcleos leves espalhados em carbono. Dessa análise foi possível concluir que o canal do break up Coulombiano, nesses sistemas leves, não é fortemente influente na seção de choque total de reação, o que implica que a interação entre alvo e projétil é dominada pelo potencial nuclear. / In the present work, we measured elastic scattering angular distributions for teh isotopes 7Be, 9Be and 10Be on 12C target. The angular distribution of 7Be at 18.8 MeV, was measured in two laboratories, with the TWINSOL system, in Notre Dame University, and the RIBRAS system, in São Paulo University, where the angular distribution was completed. The angular distribution for 9Be and 10Be isotopes measured completely in the RIBRAS system at 26.0 and 23.2 MeV, respectively. All angular distribution were analized considering optical model and coupled channel formalism. We tested multiple optical potentials on each distribution to describe the elastic cross section for these systems. For the weakly bound projectiles (7Be, 9Be and 8B)calculations with continous coupling (CDCC) were performed, while for the 10Be nucleus, which is tghtly bound nucleus, we coupled the first two bound states. We also performed a systematic analysis of the total reaction cross section obtained from elastic scattering distribution of several light particles on 12C. From this analysis, we concluded that the Coulomb break up channel, in these light systems, does not have a strong influence on the total reaction cross section, what implies that the projetile-target interaction is dominated by the nuclear potential.
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Geochemistry of soils from the Shackleton Glacier region, Antarctica, and implications for glacial history, salt dynamics, and biogeographyDiaz, Melisa A. January 2020 (has links)
No description available.
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Nuclear forces at the extremes / Les forces nucléaires aux extrêmesRevel, Aldric 27 September 2018 (has links)
L’émission de paires de neutrons par les noyaux riches en neutrons 18C et 20O (isotones N = 12) est étudié par réactions de knock-out d’un nucléon des faisceaux secondaires 19N et 21O, peuplant ainsi des états non liés jusqu’à 15 MeV au-dessus de leur seuil d’émission deux neutrons. L’analyse des corrélations des triples coïncidences fragment+n+n montre que la décroissance 19N(−1p)→18C → 16C+n+n est clairement dominée par l’émission directe de paires. Les corrélations n-n, les plus grandes jamais observées, suggèrent la prédominance d’un coeur de 14C entouré de quatre neutrons arrangés en paires très corrélées. De plus, une importante compétition du mode de décroissance séquentiel est observée dans la décroissance 21O(−1n) → 20O → 18O+n+n, interprétée par la déformation causée par le knock-out d’un neutron très lié ayant pour effet de casser le cœur de 16O et ainsi de réduire le nombre de paires.De plus, les états non liés du 26F et 28F sont étudiés. Les deux systèmes étant peuplés par knock-out d’un nucléon du 27F dans le cas du 26F et du 29Ne ou du 29F pour 28F. Cinq états ont été observés pour 26F avec en particulier l’état de plus basse énergie (0.39 MeV) identifié comme l’état 3+ résultant du couplage d5/2 ⊗ d3/2 . Pour 28F, cinq états ont aussi été observés et l’état fondamental (200 keV) a été identifié comme étant de parité négative, plaçant ainsi 28F dans l’îlot d’inversion. / The emission of neutron pairs from the neutron-rich N = 12 isotones 18C and 20O has been studied by high-energy nucleon knockout from 19N and 21O secondary beams, populating unbound states of the two isotones up to 15 MeV above their two-neutron emission thresholds. The analysis of triple fragment-n-n correlations shows that the decay 19N(−1p) → 18C → 16C+n+n is clearly dominated by direct pair emission. The two-neutron correlation strength, the largest ever observed, suggests the predominance of a 14C core surrounded by four neutrons arranged in strongly correlated pairs. On the other hand, a significant competition of a sequential branch is found in the decay 21O(−1n) → 20O → 18O+n+n, attributed to its formation through the knockout of a deeply-bound neutron that breaks the 16O core and reduces the number of pairs.Moreover, unbound states in 26F and 28F have been studied. The two systems were probed using single-nucleon knockout reaction from secondary beams of 27F respectively in the case of 26F, and 29Ne and 29F for 28F. Five possible states have been identified in 26F, with in particular the lowest energy one (0.39 MeV) being identified as the 3+ state resulting from the d5/2 ⊗ d3/2 coupling. In the case of 28F, five unbound state have also been observed and in particular its ground state (200 keV) has been identified as a negative parity state, meaning that 28F is located inside the island of inversion.
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The TITAN electron beam ion trap: assembly, characterization, and first testsFroese, Michael Wayne 19 September 2006 (has links)
The precision of mass measurements in a Penning trap is directly proportional to an ion's charge state and can be increased by using highly charged ions (HCI) from an Electron Beam Ion Trap (EBIT). By bombarding the injected and trapped singly charged ions with an intense electron beam, the charge state of the ions is rapidly increased. To use this method for short-lived isotopes, very high electron beam current densities are required of the TITAN EBIT, built and commissioned at the Max-Planck-Institute for Nuclear Physics in Heidelberg, Germany and transported to TRIUMF for the TITAN on-line facility. This EBIT has produced charge states as high as Kr34+ and Ba54+ with electron beams of up to 500 mA and 27 keV. Once the EBIT is operational at full capacity (5 A, 60 keV), most species can be bred into a He-like configuration within tens of ms. / October 2006
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The TITAN electron beam ion trap: assembly, characterization, and first testsFroese, Michael Wayne 19 September 2006 (has links)
The precision of mass measurements in a Penning trap is directly proportional to an ion's charge state and can be increased by using highly charged ions (HCI) from an Electron Beam Ion Trap (EBIT). By bombarding the injected and trapped singly charged ions with an intense electron beam, the charge state of the ions is rapidly increased. To use this method for short-lived isotopes, very high electron beam current densities are required of the TITAN EBIT, built and commissioned at the Max-Planck-Institute for Nuclear Physics in Heidelberg, Germany and transported to TRIUMF for the TITAN on-line facility. This EBIT has produced charge states as high as Kr34+ and Ba54+ with electron beams of up to 500 mA and 27 keV. Once the EBIT is operational at full capacity (5 A, 60 keV), most species can be bred into a He-like configuration within tens of ms.
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The TITAN electron beam ion trap: assembly, characterization, and first testsFroese, Michael Wayne 19 September 2006 (has links)
The precision of mass measurements in a Penning trap is directly proportional to an ion's charge state and can be increased by using highly charged ions (HCI) from an Electron Beam Ion Trap (EBIT). By bombarding the injected and trapped singly charged ions with an intense electron beam, the charge state of the ions is rapidly increased. To use this method for short-lived isotopes, very high electron beam current densities are required of the TITAN EBIT, built and commissioned at the Max-Planck-Institute for Nuclear Physics in Heidelberg, Germany and transported to TRIUMF for the TITAN on-line facility. This EBIT has produced charge states as high as Kr34+ and Ba54+ with electron beams of up to 500 mA and 27 keV. Once the EBIT is operational at full capacity (5 A, 60 keV), most species can be bred into a He-like configuration within tens of ms.
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Migration of Recharge Water Downgradient from the Santa Catalina Mountains into the Tucson Basin AquiferBarger, Erin E. January 1996 (has links)
Aquifers in the arid alluvial basins of the southwestern U.S. are recharged predominantly by infiltration from streams within the basins and by water entering along the margins of the basins from surrounding mountains (mountain -front recharge). The Tucson Basin of Southeastern Arizona is such a basin. The Santa Catalina Mountains form the northern boundary of this basin and receive more than twice as much precipitation (about 70 cm/yr) as the basin does (about 30 cm/yr). In this study environmental isotopes were employed to investigate the migration of precipitation basinward through joints and fractures. Water samples were obtained from springs in the Santa Catalina Mountains. Stable isotopes and thermonuclear bomb-produced tritium enabled qualitative characterizations of flow paths and flow velocities. Stable isotopic measurements fail to display a direct altitude effect. Tritium values indicate that although a few springs discharge pre-bomb water, most springs discharge waters from the 1960's or later.
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A Re-Os Study of Sulfides from the Bagdad Porphyry Cu-Mo Deposit, Northern Arizona, USABarra-Pantoja, Luis Fernando January 2001 (has links)
Use of Re-Os systematics in sulfides from the Bagdad porphyry Cu-Mo deposit provide information on the timing of mineralization and the source of the ore -forming elements. Analyzed samples of pyrite, chalcopyrite and molybdenite mainly from the quartz monzonite and porphyritic quartz monzonite units are characterized by a moderate to strong potassic alteration (secondary biotite and K- feldspar). Rhenium concentrations in molybdenite are between 330 and 730 ppm. Two molybdenite samples from the quartz monzonite and porphyritic quartz monzonite provide a Re-Os isotope age of 71.7 ± 0.3 Ma. A third sample from a molybdenite vein in Precambrian rocks yields an age of 75.8 ± 0.4 Ma. These molybdenite ages support previous suggestions of two mineralization episodes in the Bagdad deposit. An early event at 76 Ma and a later episode at 72 Ma. Pyrite Os and Re concentrations range between 0.008-0.016 and 3.9-6.8 ppb, respectively. Chalcopyrite contains a wide range of Os (6 to 91 ppt) and Re (1.7 to 69 ppb) concentrations and variable ¹⁸⁷Os/¹⁸⁸Os ratios that range between 0.13 to 22.27. This variability in the chalcopyrite data may be attributed to different copper sources, one of them the Proterozoic volcanic massive sulfides in the district, or to alteration and remobilization of Re and Os. Analyses from two pyrite samples yield an eight point isochron with an age of 77 ± 15 Ma and an initial ¹⁸⁷Os/¹⁸⁸Os ratio of 2.12. This pyrite Re-Os isochron age is in good agreement with the molybdenite ages. We interpret the highly radiogenic initial 1870s/188Os as an indication that the source of Os and, by inference, the ore-forming elements for the Bagdad deposit, was mainly the crust. This conclusion agrees with previous Pb and Nd isotope studies and supports the notion that a significant part of the metals and magmas have a crustal source.
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