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AbstractAbstract
[en] For a given product concentration, choice of the cascade structure is presented. For the cascade, having the minimum number of columns for the desired production, the operation curves and other characteristics are calculated. (author)
Original Title
Calculul unei cascade de termodifuzie (TD) destinata separarii 36Ar
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74 refs.
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Journal Article
Journal
Studii si Cercetari de Fizica; ISSN 0039-3940;
; v. 30(2); p. 131-135

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AbstractAbstract
[en] For minerals of metal pegmatite, the K, Ar content and the 40Arsub(ex)/sup(36)Arsub(capt) ratio are measured. An apparent value of age reaches 1010 years. Based on Rb-Sr measurements, absolute time sequence of mineral crystallization, Δ t, is calculated. The plot sup(40)Arsub(ex)/sup(36)Arsub(capt) vs Δ t has been constructed from a typical form of which an assumption has been made on the existence of radioactive decay of two elements. A half-life period calculated for the first element, supposedly EcCs, is equal to 1 x 106 years, and that for the second one, supposedly EcRa, is 7x106 years. Application of these half-lives to treatment of literature data on the content of excess argon leads an analogous - up to 70x106 years - succession of mineral crystallization. A conclusion is drawn on the radiogenic nature of excess argon
Original Title
O radiogennoj prirode izbytochnogo argona v mineralakh
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Source
For English translation see the journal Soviet Radiochemistry (USA).
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Journal Article
Journal
Radiokhimiya; ISSN 0033-8311;
; v. 22(4); p. 554-560

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AbstractAbstract
No abstract available
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Journal Article
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Geochimica et Cosmochimica Acta; v. 39(8); p. 1127-1134
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Odin, G.S.; Velde, B.; Bonhomme, M.
Proceedings of the Fourth European Colloquium of Geochronology, Cosmochronology and Isotope Geology held at Amsterdam, The Netherlands, 5-10 Apr 19761976
Proceedings of the Fourth European Colloquium of Geochronology, Cosmochronology and Isotope Geology held at Amsterdam, The Netherlands, 5-10 Apr 19761976
AbstractAbstract
No abstract available
Primary Subject
Source
Laboratorium voor Isotopen-Geologie, Amsterdam (Netherlands); Rijksuniversiteit Groningen (Netherlands). Lab. voor Isotopen-Fysica; p. 71; 1976; 4. European colloquium of geochronology, cosmochronology and isotope geology; Amsterdam, The Netherlands; 5 Apr 1976; Published in summary form only.
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Report
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Conference
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AbstractAbstract
No abstract available
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Source
3. lunar science conference; Houston, Texas, USA; 10 Jan 1972; See CONF-720121--(Vol.3).
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Journal Article
Literature Type
Conference
Journal
Geochimica et Cosmochimica Acta; v. Suppl. 3 p. 2867-2881
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AbstractAbstract
[en] The construction of UHV metal-gas line is described. The instrumental set-up comprises the following units; (1) double vacuum crucible for Ar extraction, which is made of tantalum and can be heated by resistance oven to 1500 C; (2) 38Ar isotope spike container with gas pipette for the isotope dilution technique; (3) two ovens - filled with CuO for oxidation of hydrogen and hydrocarbons and another filled with Ti shaving for cleaning all the reactive gases; (4) getter pump for final cleaning of argon and (5) 180 C-sector mass spectrometer for quantitative analysis of argon isotopes. (author). 11 refs, 8 refs
Original Title
Lubelska aparatura UHV do wydzielania, oczyszczania i analizy masowo-spektrometrycznej argonu do datowania mineralow
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Loehle, U.
Freiburg Univ. (F.R. Germany). Fakultaet fuer Physik1973
Freiburg Univ. (F.R. Germany). Fakultaet fuer Physik1973
AbstractAbstract
No abstract available
Original Title
γ-Spektroskopie in 34Ar
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Source
Apr 1973; 62 p; 12 figs.; 3 tabs.; 35 refs. Available from the library of the Freiburg Univ.; Diss. (D.Sc).
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Report
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Thesis/Dissertation
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AbstractAbstract
[en] The 35Cl(p, γ)36Ar reaction was studied in the proton energy range E/subp/ = 2.36--2.42 MeV. Yield curves were obtained using NaI(Tl) and Ge(Li) detectors. The E/subx/ = 10854.2 +- 1.6 keV level, populated at the E/subp/ = 2414.4 +- 1.5 keV resonance, decays to the E/subx/ = 7711 and 8133 keV levels with branching ratios of (35 +- 15) % and (65 +- 15) %, respectively. From resonance strength and angular distribution measurements as well as from the comparison with the γ-decay scheme of the lowest T = 2 state of 36Cl, the E/subx/ = 10854 keV level can be assigned definitely (J/sup pi/, T) = (0+, 2)
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Journal Article
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Phys. Rev., C; v. 13(5); p. 1786-1791
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AbstractAbstract
[en] Discussion is made on the origin of the atmosphere, the mass balance of rare gases, the isotopic abundance ratio of Ar, and the model of the evolution of the atmosphere. The relative abundance of rare gases in the atmosphere is much different from that of the sun. For example, 40Ar is present in the air at the concentration of about 1%. This concentration is much higher than the solar abundance. This extraordinarily high concentration of Ar in the air is now attributed to the formation of 40Ar by the decay of 40K contained inside the earth. The isotopic abundance ratio of Ar, namely the abundance ratio of 40Ar:36Ar was estimated to have been about 10-4, 4500 million years ago, whereas the ratio is now 99.6:0.337. This increase of the amount of 40Ar is attributable to the decay of 40K. The abundance of potassium in the earth is estimated to be about 130 ppm. The continuous degasification model cannot explain the change of the abundance of 40Ar. On the other hand, the catastrophic degassification model well explains the change of 40Ar in the atmosphere. (Fukutomi, T.)
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Journal Article
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Seibutsu Kagaku; v. 27(2); p. 59-63
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AbstractAbstract
[en] Complete text of publication follows. The exotic shapes of atomic nuclei has attracted much attention recently both from the experimental and from the theoretical sides. E.g. the superdeformed (SD) shape in N = Z nuclei were observed experimentally during the last decade. In particular the SD band of the 36Ar nucleus was detected in 2000 [1]. Following the experimental observation a considerable theoretical effort has been concentrated on this band. In [2] e.g. the possible binary clusterizations of this state was studied systematically. Similar studies have been done also for the ground, and the hyperdeformed band. The latter one had been predicted from alphacluster model calculations [3]. The possible binary cluster-configurations are important not only for the better understanding of the structure of the shape isomers, but also from the viewpoint of predicting the favoured reaction channels to populate these states. This is the straightforward consequence of the close relation between the clusterization and reaction channels. (In fact, a cluster-configuration is defined by the reaction channel in which it can be observed.) One of the interesting conclusions of the work [2] was, that the hyperdeformed (HD) state of the 36Ar nucleus could be populated in the 24Mg+12C and 20Ne+16O reactions. A recent analysis of the 24Mg+12C elastic scattering [4] revealed the fact that the cross section can be described only by supposing resonances on top of the potential scattering. This very careful analysis incorporated phase-shift study, as well as Regge-pole and energy-dependent resonance calculations. The existence of five resonances have been proved, which have angular momenta 2, 4, 6, 7, 8. These states together with the resonances from the 20Ne+16O reactions seem to establish a rotational band, as shown in the upper part of Fig. 1. Its moment of inertia is in a very good agreement with that of the HD shape predicted from alpha-cluster model [3]. The similarity of the (predicted and observed) moments of inertia, and the fact that the resonances were seen in exactly those reactions, which define the preferred cluster-configurations of the HD shape suggest that the recently observed band in Fig. 1. is a good candidate for the hyperdeformed shape isomer of the 36Ar nucleus. For comparison also the ground and superdeformed bands are indicated in Fig. 1. Since a candidate for the HD state showed up, the exciting question arises if such a shape can be seen in shell-model calculation as well. In [5] we have carried out Nilssonmodel+ quasi-dynamical SU(3) calculation in order to find the answer. In this kind of study the shape isomers are obtained from the SU(3) symmetries, not from the minima of the potential energy surface. They are determined as the horizontal plateus of the stair-like functions, shown in Fig. 2. (In lighter nuclei, where detailed comparison could be made, the two method gave results in very good agreement with each other.) As it is seen in Fig. 2. in addition to the ground and superdeformed states the shell model predicts two candidates (a slightly triaxial, and a cylindrical one) for the hyperdeformed shape. The cylindrical state has exactly the same symmetry as that from the alpha-cluster model, and consequently the same moment of inertia, as well. To sum up: from cluster studies [2,3] we have predicted [2] the 24Mg+12C and 20Ne+16O channels to populate the HD state in the 36Ar nucleus. Recently a highly-deformed rotational band has been observed [4] experimentally in these reactions. The moment of inertia is in complete agreement with the prediction. Furthermore, the same state has been found in Nilsson-model calculation [5]. Therefore, we conclude that it is a good candidate for the hyperdeformed band in the 36Ar nucleus, as shown in Fig. 1. Thus it might very well be that the 36Ar nucleus is the first N = Z nucleus in which the ground, superdeformed and hyperdeformed bands have been observed.
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5 refs.
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