Checking of the hypothesis of the existence of the baryon passive state by calorimeter telescope and the energy spectrum of nuclear-active particles at mountain altitude

1968 ◽  
Vol 46 (10) ◽  
pp. S706-S708
Author(s):  
A. D. Erlykin ◽  
A. K. Kulichenko ◽  
S. K. Machavariani ◽  
R. A. Nam ◽  
S. I. Nikolsky ◽  
...  

In the Tien-Shan underground ionization calorimeter situated at a depth of about 13 m below the big ionization calorimeter (BIC), a search was made for jets which could be the continuation of nuclear cascades arising in BIC. The results obtained are used to check the hypothesis of the existence of the baryon passive state. Preliminary results on the spectrum of nuclear-active particles are given.


1968 ◽  
Vol 46 (10) ◽  
pp. S686-S688 ◽  
Author(s):  
N. L. Grigorov ◽  
V. A. Sobinyakov ◽  
Ch. A. Tretyakova ◽  
V. Ya. Shestoperov ◽  
Kh. P. Babayan ◽  
...  

The results of measurements of the energy spectrum of nuclear-active particles carried out by means of an ionization calorimeter and an installation recording ionization bursts at the altitude of 3 200 m above sea level are presented.



1968 ◽  
Vol 46 (10) ◽  
pp. S328-S331
Author(s):  
A. D. Erlykin ◽  
A. K. Kulichenko

With the Tien-Shan (3 340 m altitude) ionization calorimeter, the spectrum of ionization bursts has been investigated at a depth of 20 m.w.e. underground. The results obtained show that the characteristics of the penetrating component do not differ from those expected of the muon component; there is no evidence for the existence of the "baryon-passive" state, which has been suggested by Smorodin.



1978 ◽  
Vol 68 (4) ◽  
pp. 949-971
Author(s):  
T. G. Rautian ◽  
V. I. Khalturin ◽  
V. G. Martynov ◽  
P. Molnar

abstract This paper reports preliminary results of an analysis of the spectral content of seismic waves from over 1,000 local earthquakes in the Garm, Tadjikistan region. Very low values of Q (∼100) were obtained for the Mesozoic and Cenozoic sedimentary rocks of the Peter I Range compared with those in the crystalline rock of the South Tien Shan (Q ≳ 500). For events with the same low frequency spectra, earthquakes in the South Tien Shan are recorded with more energy at higher frequencies than earthquakes in the Peter I Range, at least in part, because of the greater attenuation of the sedimentary rock in the latter region. There is a wide variety of spectra radiated by earthquakes throughout the Garm region, but a marked difference between spectra radiated by earthquakes from these two regions is not apparent. Nevertheless although calculated stress drops of earthquakes appear to vary considerably throughout the region, there appears to be a dependence on the type of rock in which the earthquakes occurred. The variation in calculated stress drops, however, is greater within either region than between the two. For most regions and for most of the range of seismic moments studied the shape of the spectrum is relatively independent of seismic moment. Consequently, calculated stress drops increase with seismic moment, with the functional dependence varying from region to region. For the largest events, the spectrum shifts to lower frequencies with increasing moment and stress drops become essentially independent of moment. Preliminary results suggest that the stress drops are not detectably different for earthquakes with thrust or normal faulting fault-plane solutions. A limited amount of data are consistent with a change in spectral content and stress drop of earthquakes in the vicinity of and before stronger earthquakes but a clear, consistent pattern is not yet evident. Toward high frequencies, S-wave spectra both begin to decrease at lower frequencies and seem to decrease more rapidly than P-wave spectra, in contrast with predictions of published dislocation models of earthquakes.



Author(s):  
V.A. Ryabov ◽  
V.P. Antonova ◽  
A.P. Chubenko ◽  
A.N. Karashtin ◽  
G.G. Mitko ◽  
...  


2011 ◽  
Vol 20 (supp02) ◽  
pp. 57-60
Author(s):  
ERNESTO KEMP ◽  
BRUNO MIGUEZ ◽  
WALTER FULGIONE

The neutrino telescopes of the present generation, depending on their specific features, can reconstruct the neutrino spectra from a galactic burst. Since the optical counterpart could be not available, it is desirable to have at hand alternative methods to estimate the distance of the supernova explosion using only the neutrino data. In this work we present preliminary results on the method we are proposing to estimate the distance from a galactic supernova based only on the spectral shape of the neutrino burst and assumptions on the gravitational binding energy released an a typical supernova explosion due to stellar collapses.



2017 ◽  
Vol 81 (4) ◽  
pp. 457-459 ◽  
Author(s):  
E. N. Gudkova ◽  
N. M. Nesterova ◽  
N. M. Nikolskaya ◽  
V. P. Pavlyuchenko


1968 ◽  
Vol 46 (10) ◽  
pp. S678-S680 ◽  
Author(s):  
I. N. Fetisov ◽  
A. E. Morozov ◽  
S. A. Slavatinsky

The energy transferred to neutral π mesons in the interaction of nuclear-active particles with the lead nucleus was studied with an ionization calorimeter. The mean value of the energy transferred to π0 mesons is [Formula: see text]. The [Formula: see text] distribution is also presented.



1970 ◽  
Vol 37 ◽  
pp. 88-93
Author(s):  
U. R. Rao ◽  
E. V. Chitnis ◽  
A. S. Prakasarao ◽  
U. B. Jayanthi

Preliminary results of two rocket flights carrying X-ray payloads conducted from Thumba Equatorial Rocket Launching Station (TERLS), Trivandrum, India, on November 3, 1968, and November 7, 1968, respectively, are presented. The results indicate the first evidence for the existence of low energy X-ray flux in the energy range 2–20 keV from Cen-X2 source since the reported extinction in May, 1967. The energy spectrum and the absolute flux of X-rays from Cen-X2, Sco-X1 and Tau-X1 are presented and compared with other observations.



1991 ◽  
Vol 9 (1) ◽  
pp. 111-112
Author(s):  
Heng-Rong Hang ◽  
Zhi-Yun Zang ◽  
Shan-Zhao Liu ◽  
Gui-Qing Ma ◽  
I-Zhong Gong ◽  
...  

AbstractA China-Japan X-ray balloon flight took place in 1988 August. Preliminary results are presented for the energy spectrum of Cyg X-1.



2007 ◽  
Vol 53 (182) ◽  
pp. 368-373 ◽  
Author(s):  
Li Zhongqin ◽  
Li Chuanjin ◽  
Li Yuefang ◽  
Wang Feiteng ◽  
Li Huilin

AbstractWe present preliminary results on the occurrence of Pb, Cd, Zn, Al and Fe in dated samples collected from snow–firn packs at an altitude of 4130 m on Ürűmqi glacier No. 1, eastern Tien Shan. Extreme precautions for avoiding contamination were taken throughout the sampling, processing, transportation and analysis procedures. The concentrations of trace metals were determined by a double-focusing inductively coupled plasma mass spectrometer in an ultra-clean room. The average concentrations for these metals in surface snow are (in ng g–1): Pb, 2.4; Cd, 0.05; Zn, 10.0; Al, 100.0; and Fe, 130.0. These are higher concentrations (especially for Pb and Zn) than those in the polar and/or low-latitude remote areas. The data show that the input of trace metals to the snow has a clear seasonal change. Lower concentrations in surface snow can be found in July through September and higher concentrations from October to March, with an exception for January. The mean concentrations of the elements in the snow–firn pack also indicate seasonal variations and show a marked inverse relationship with temperature, possibly a result of meltwater percolation in the snow–firn pack.



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