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21.
J. D. M. Dewi Ph. Podsiadlowski A. Sena 《Monthly notices of the Royal Astronomical Society》2006,368(4):1742-1748
We present the results of a systematic exploration of an alternative evolutionary scenario to form double neutron star (DNS) binaries, first proposed by Brown (1995) , which does not involve a neutron star passing through a common envelope. In this scenario, the initial binary components have very similar masses, and both components have left the main sequence before they evolve into contact; preferably the primary has already developed a CO core. We have performed population synthesis simulations to study the formation of DNS binaries via this channel and to predict the orbital properties and system velocities of such systems. We obtain a merger rate for DNSs in this channel in the range of 0.1–12 Myr−1 . These rates are still subject to substantial uncertainties such as the modelling of the contact phase. 相似文献
22.
A. Kh. Zil’bershtein V. S. Semenov V. A. Glebovitsky V. N. Dech 《Izvestiya Physics of the Solid Earth》2014,50(2):305-309
The probable implications of the injection of additional batches of melt into the magma chamber and the correlation of ore formation to these processes are considered. The assumed model of hydraulic impact (stamp) explains a number of the structural features of layered basite-hyperbasite intrusions and, in particular, formation of microgranular rocks, whose structure indicates a high rate of crystallization, and, probably, platinum group element (PGE) mineralization in the Lukkulaisvaara layered intrusion, North Karelia. It is shown that intrusion of additional batches of magma can lead to thermodiffusion, which is most effective in the vicinity of the contact between the chamber and the portion of magma. This, in turn, should result in the redistribution of chemical components in this zone and, probably, to anomalous concentrations of productive components at early penetration stages. 相似文献
23.
D. Bugai V. Kashparov L. Dewiére Yu. Khomutinin S. Levchuk V. Yoschenko 《Environmental Geology》2005,47(6):869-881
Several radiometric and geophysical methods were applied to characterize the subsurface geometry and radioactivity distribution (especially 137Cs) in a trench with low-level wastes at the Chernobyl site. While surface dose rate measurements and electromagnetic soil conductivity survey produced uninterpretable fields of signals, the ground penetrating radar appeared to be an efficient method for characterization of the subsurface geometry of the waste burial. It was established that the trench had the following dimensions: the length was 70 m; average width 6–8 m, and depth 2–2.5 m. Data on 137Cs distribution in the trench were obtained by means of a borehole gamma-logging technique. The total inventory of 137Cs was estimated at 600±200 GBq. Geostatistical analysis using the semivariogram function has shown regular spatial correlation patterns for the logarithm-transformed 137Cs activity of waste material. The correlation length along the trench was 17 m, while across the trench, and in the vertical direction, it was 4 m. The observed correlation patterns supposedly were caused by the method used to dispose the contaminated topsoil: the bulldozing in the direction perpendicular to a trench axis. Obtained results may be useful for selecting a characterization method and for optimization of sampling strategies for similar waste sites. 相似文献
24.
研究对2011年7月采自印度尼西亚卡利安达岛近岸热泉的样品,进行了细菌和古菌16S rRNA基因和细菌氢酶基因克隆文库的构建、序列测定和多样性分析。结果表明:热泉系统的细菌和古菌由16个门组成,Proteobacteria为热液流体和沉积物的优势类群,丰度分别为59.5%和73.3%,Cyanobacteria为菌苔的优势类群(丰度,56.5%);具有氨氧化作用的Crenarchaeota为古菌的优势类群。热泉系统中,70%以上的种类与海洋细菌的亲缘关系最近,说明该系统具有海洋特性;约20%的种类与陆地热泉中嗜热或中等嗜热细菌的亲缘关系最近,这些种类可能来源于高温地层内部,并参与了铁氧化还原、氢氧化、硫氧化和硝酸还原等过程。热泉系统中,NAD(P)-关联的双向NiFe-氢酶基因和FeFe-氢酶基因的组成分布也受到温度和盐度分布变化的影响。研究为揭示浅海热液系统提供理论参考。 相似文献