Search of the chemical change of the119mSn (T1/2=293 days) radioactive decay rate

1983 ◽  
Vol 13 (1-3) ◽  
pp. 237-248 ◽  
Author(s):  
K. Makariūnas ◽  
E. Makariūnienė ◽  
A. Dragūnas
Author(s):  
Victor Panchelyuga ◽  
Maria Panchelyuga ◽  
Olga Seraya

The evolution of views on the possibility of external influence on the process of radioactive decay is briefly presented. Such an effect can lead to the appearance of periods in the time series of the radioactive decay rate fluctuations, which have been the subject of intensive study in the last decade. Two mechanisms for identifying periods are considered: the study of deviations from the theoretical curve of the radioactive decay law and the study of the properties of fluctuations. It is shown that the latter method leads to a universal spectrum of periods observed not only in the time series of the radioactive decay rate fluctuations, but also in the time series of fluctuations of processes of various nature. The main object of our study are periods in the radioactive decay rate fluctuations. The presence of such periods suggests the possibility of external influence on the process of radioactive decay. Therefore, we briefly consider the evolution of views on the possibility of such an effect. To do this, we distinguish several stages. The division into stages is only partially historical, but, mainly, each stage characterizes a certain ideas that is implemented in it.


1979 ◽  
Vol 7 (1) ◽  
pp. 201-205 ◽  
Author(s):  
K. Makariūnas ◽  
E. Makariūniené ◽  
A. Dragūnas

Metaphysics ◽  
2020 ◽  
pp. 10-34
Author(s):  
V. A Panchelyuga

The subject of this work is periods in time series of the radioactive decay fluctuations. The presence of such periods suggests the possibility of a certain external influence on the parameters of radioactive decay. The evolution of views on the possibility of such an influences are briefly reviewed. A number of stages are considered, each of which expresses a certain circle of ideas, which is realized in it. Experimental works typical for each such stage are considered. The article does not aim to review all works related to the issues discussed in it. This is, first of all, a presentation of ideas that reflect the author's views on the possible mechanisms of the occurrence of periods in the time series of the radioactive decay rate. The links provided in the work are rather illustrative.


2008 ◽  
Vol 5 (4) ◽  
pp. 371-373 ◽  
Author(s):  
V. L. Mikheev ◽  
V. A. Morozov ◽  
N. V. Morozova

2001 ◽  
Vol 53 (3) ◽  
pp. 283-289 ◽  
Author(s):  
L Juodis ◽  
A Plukis ◽  
V Remeikis ◽  
K Makariunas

Science ◽  
2005 ◽  
Vol 310 (5749) ◽  
pp. 839-841 ◽  
Author(s):  
Yuri Amelin

The use of radioactive decay of 176Lu to 176Hf to study the evolution of the Earth requires a precise and accurate value for the 176Lu decay constant. Recent determinations of this decay constant by age comparison to the more precisely calibrated U-Pb isotopic system produced internally consistent but discrepant values between terrestrial minerals and meteorites. New highly radiogenic Lu-Hf data for phosphate minerals from Richardton (ordinary chondrite) and Acapulco (primitive achondrite) yield decay constant values of 1.864 × 10–11 ± 0.016 × 10–11 and 1.832 × 10–11 ± 0.029 × 10–11 year–1, respectively, identical to the value determined from terrestrial minerals.


2007 ◽  
Vol 98 (25) ◽  
Author(s):  
T. Ohtsuki ◽  
K. Ohno ◽  
T. Morisato ◽  
T. Mitsugashira ◽  
K. Hirose ◽  
...  

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