Meteorite Phosphates Show Constant 176Lu Decay Rate Since 4557 Million Years Ago

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.

1959 ◽  
Vol 14 (4) ◽  
pp. 334-342 ◽  
Author(s):  
F. Begemann

The terrestrial decay rate of “natural” tritium has been re-determined from measurements of the tritium content of old snow samples from Greenland. The finding by CRAIG and BEGEMANN and LIBBY has been confirmed that the tritium decay rate is about 10 times higher than was anticipated previously.Two mechanisms to explain the discrepancy are discussed,a) production by the low energy component of the cosmic radiation andb) the accretion of solar tritium by the earth, as suggested by FELD and ARNOLD.It is shown that in case all the tritium is produced by cosmic radiation the tropospheric production rate may be expected to vary in antiphase with the sunspot cycle, whereas in case of accretion of solar tritium by the earth the variation should be in phase with the sunspot cycle. In both cases a phase shift between the stratospheric production rate and the amount of tropospheric tritium is to be expected because of the residence time of tritium in the stratosphere. A measurement of the phase shift should allow to determine this residence time.The data obtained on the Greenland samples appear to show such a variation of the production rate. The results can be explained best by assuming that all the tritium is produced by cosmic radiation. This result, however, is only preliminary. More systematic measurements are required to decide between the two possibilities.


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.


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

2020 ◽  
Vol 66 (257) ◽  
pp. 447-456 ◽  
Author(s):  
Heinz W. Gäggeler ◽  
Leonhard Tobler ◽  
Margit Schwikowski ◽  
Theo M. Jenk

Abstract210Pb is an environmental radionuclide with a half-life of 22.3 years, formed in the atmosphere via radioactive decay of radon (222Rn). 222Rn itself is a noble gas with a half-life of 3.8 days and is formed via radioactive decay of uranium (238U) contained in the Earth crust from where it constantly emanates into the atmosphere. 210Pb atoms attach to aerosol particles, which are then deposited on glaciers via scavenging with fresh snow. Due to its half-life, ice cores can be dated with this radionuclide over roughly one century, depending on the initial 210Pb activity concentration. Optimum 210Pb dating is achieved for cold glaciers with no – or little – influence by percolating meltwater. This paper presents an overview which not only includes dating of cold glaciers but also some special cases of 210Pb applications in glaciology addressing temperate glaciers, glaciers with negative mass balance, sublimation processes on glaciers in arid regions, determination of annual net snow accumulation as well as glacier flow rates.


2020 ◽  
Author(s):  
Bin Gong ◽  
Chun‘an Tang ◽  
Tiantian Chen ◽  
Zhanjie Qin ◽  
Hua Zhang

<p>Alternative cooling and warming have occurred many times in the history of Earth since its formation. In the meantime, active and quiescent periods of geological activity have also alternatively occurred in this same planet. When Earth became hotter, it shows widespread geological activities, such as LIPs, whereas during the colder stage, it became relatively quiet without too much magma activities. Although various models have been used to explain the trigger for each of these activities, there is no consensus about the fundamental relationships between the thermal cycles and episodically geological processes. The major energy sources for Earth after ~3.8 Ga include primordial heat left from the accretion, differentiation, and the radioactive decay of heat-producing elements. Surface tectonics and magmatism control the transport of heat from the interior to the surface and most surface tectonic features of Earth are the expression of their interior dynamics. Supercontinental breakup and aggregation have occurred for many times in the Earth history, accompanied by episodic cooling and warming on the Earth surface. This breakup and aggregation regime is known as plate tectonics and is characterized by high average surface heat flow fluctuations. Based on the thermodynamic principle, a thermodynamic equilibrium equation describing the earth’s thermal cycles is established. We realized that this thermal cycle may drive Earth itself to evolve, and is the fundamental reason for the periodicity or rhythmicity of geological events such as tectonic movements, orogenies, glacial periods and biological extinctions. Following this principle, we then introduced a project of Wall Chat to compile global data or evidences using a variety of literatures in Geology of early investigations of geological events to explore the relationship between geological events and Earth’s thermal cycles. The data includes the supercontinent cycle, tectonic movement, plate tectonics, extremely hot event, extremely cold event, evaporite, marine red bed, biological evolution and extinction, sea level fluctuation, etc. The Wall Chat reveals that most of the geological events have their relation to the Earth’s thermal cycles. We found that there may exist a good correlation between the occurrence of evaporites and marine red beds and the higher temperature periods, which then provides a new perspective to understand the triggering of these events. The Wall Chat also raises an interest and important question on why are the two Great Oxidation Events (GOE) both related to the two snowball events? We have several clear objectives for the future. First, we are currently cooperating with some of the related institutes of geology to obtain additional evidence data to fill in many of the gaps in the chat; targeted areas include Paleontology, Glaciology, evaporite and red beds. Second, to understand fully the relationship between thermal cycles and, at least, most of the great geological events. Such studies, when sufficiently constrained by event data, should lead to a greatly improved understanding of the earth evolution.</p>


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

1963 ◽  
Vol 41 (11) ◽  
pp. 1911-1923 ◽  
Author(s):  
E. R. Kanasewich ◽  
J. C. Savage

It has long been recognized that Dirac's principle might imply that the rate of β decay would vary with the age of the universe. If so, the radioactive ages of meteorites and terrestrial rocks as indicated on the one hand by α decay and on the other by β decay should differ. However, the comparison of these ages is complicated by a large uncertainty in the decay constant for Rb87. Thus the age data must be analyzed to determine the decay constant most compatible with the particular theory of β decay which is used. Using this best decay constant for each theory, we find that the data are more consistent with a β decay rate independent of the age of the universe than with the dependence implied by the Dirac principle.


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.


2021 ◽  
Author(s):  
Shawn Eastmond

The radioactive decay law was first formulated by Ernest Rutherford and Frederick Soddy in 1902. As a well-known law, one of its primary applications is to determine the dates of ancient specimens. The process is known as radiocarbon dating and is subjected to the known properties of radioactive nuclei. In this paper, we implement quantum calculus to express the solution of the radioactive decay equation in symmetrized q-exponential form. Also, we explore a q-analog of the decay constant using Tsallis logarithmic function for various miscellaneous q-values. Furthermore, the factor-label method was applied to our analysis to show that the correct units remained intact under the application of quantum calculus. In conclusion, our work suggests that a variation of the q-parameter was akin to the production of a new isotope for all q in (0,1); the superadditive regime.


Author(s):  
Victor Panchelyuga ◽  
Kharlampiy Tiras ◽  
Kirill Novikov ◽  
Maria Panchelyuga ◽  
Svetlana Nefedova ◽  
...  

A local fractal analysis by all permutations method (APM) was developed. APM-analysis of noise-like time series of alpha decay rate fluctuations made it possible to reveal the spectrum of periods in the range of 1-120 min. The connection of this spectrum with the spectrum of the Earth natural oscillations was shown, and an assumption was made about its universal character, which means that it is present in fluctuations of processes of various nature. In this work, the APM method was used to study the noise-like time series of planarium chemiluminescence fluctuations. A spectrum of periods ranging from minutes to two hours has been obtained. A detailed coincidence of the found spectrum with the spectrum that we found earlier is shown. The results of present study confirm this earlier assumption about the universal nature of the detected spectrum of periods. For the mentioned range of periods, there were shown not only the close relationship of the found spectrum with the spectrum of the Earth's natural oscillations, but also its universal character: the spectra of the periods found for fluctuation in the systems of various nature (physical, chemical, biological) always coincided with the corresponding part of the found spectrum.


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