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2016, Applied Physics A
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4 pages
1 file
The atmospheric tests of nuclear weapons caused a sudden increase in the radiocarbon concentration in the atmosphere from 1955, reaching its maximum value in 1963-1965. Once the nuclear tests in the atmosphere were halted, the 14 C concentration started to decrease. This behavior of the radiocarbon concentration is called the ''Bomb Peak'', and it has successfully been used as a tool for high-precision radiocarbon measurements, in forensic sciences and biology. In the art field, the possibility of dating canvas, wood and paper, widely used as supports for paintings, may be an invaluable tool in modern art studies.
Radiocarbon
ABSTRACTRadiocarbon (14C) dating has previously been applied to modern paintings on canvas from the 20th century to identify potential modern forgeries, and dates indicate a time lag of several years between the harvesting of plant fibers for making canvas, and completion of a painting. This study investigated both the length of this time lag and the potential of 14C dating to inform about an individual artist’s mode of working (for example long-term storage or reuse of canvases, or extended reworking on a single canvas) and/or to establish a chronology for a corpus of work. Two pre-bomb and 16 post-bomb artworks by 17 mid-20th-century Scandinavian artists were 14C dated. The majority of post-bomb samples indicated a time lag of 2–5 years between the harvesting of the plants and completion of a painting, but some samples recorded lags of up to 10 years, and others produced much earlier results, potentially indicating the use of much older canvases or challenges removing contaminatio...
Proceedings of the National Academy of Sciences, 2019
MRS Proceedings, 1990
The use of a particle accelerator to measure the 14C content of carbon-containing materials is briefly described. The application of the method to the determination of the age of some artistic artifacts is discussed.
Quaternary Geochronology, 2009
The past few hundred years have seen large fluctuations in atmospheric 14 C concentration. In part, these have been the result of natural factors, including the climatic changes of the Little Ice Age, and the Spö rer and Maunder solar activity minima. In addition, however, changes in human activity since the middle of the 19th century have released 14 C-free CO 2 to the atmosphere. Moreover, between c. 1955 and c. 1963, atmospheric nuclear weapon testing resulted in a dramatic increase in the concentration of 14 C in the atmosphere. This was followed by a significant decrease in atmospheric 14 C as restrictions on nuclear weapon testing began to take effect and as rapid exchange occurred between the atmosphere and other carbon reservoirs. The large fluctuations in atmospheric 14 C that occurred prior to 1955 mean that a single radiocarbon date may yield an imprecise calibrated age consisting of several possible age ranges. This difficulty may be overcome by obtaining a series of 14 C dates from a sequence and either wigglematching these dates to a radiocarbon calibration curve or using additional information on dated materials and their surrounding environment to narrow the calibrated age ranges associated with each 14 C date. For the period since 1955 (the bomb-pulse period), significant differences in atmospheric 14 C levels between consecutive years offer the possibility of dating recent samples with a resolution of from one to a few years. These approaches to dating the recent past are illustrated using examples from peats, lake and salt marsh sediments, tree rings, marine organisms and speleothems.
Analytical Chemistry, 2009
This isa preprintof apaper intended for publication ina joumalorproceedings. Since changes may be made before publication, this preprint is made available with the understanding that it will not be cited or reproduced without the permission of the author.
2015
The ICR (Institute for Creation Research) recently spent eight years on a project known as RATE (Radioisotopes and the Age of The Earth). The RATE team claims the results have yielded convincing and irrefutable scientific evidence of a young earth. John Baumgardner, a geophysicist with expertise in tectonic modeling, presents experimental data claiming to show that all biological material contains intrinsic radiocarbon, no matter how old that material may be thought to be [1, 2]. He makes additional claims that even non-biological carbonaceous material contains intrinsic radiocarbon. He suggests that this radiocarbon is residual from the material's creation. If true, his claims would have far-reaching implications for the ages of these materials. Baumgardner presents two classes of data. The first is a set of 90 previously published radiocarbon AMS dates of old samples (most >100k years) that he has re-analyzed. The second is a set of new samples that the RATE team collected and sent to a leading radiocarbon AMS laboratory to be dated. In both cases, I am convinced that the "intrinsic radiocarbon" is nothing more than contamination and instrument background. Modern Radiocarbon Dating New Methods Allow Smaller Samples Willard Libby discovered radiocarbon dating in the late 1940s. He received the Nobel Prize in Chemistry for this discovery in 1960. The technique arises from radiocarbon being continually produced in the upper atmosphere by cosmic rays while it is continually decaying, so the atmospheric concentration has reached a fairly steady equilibrium. Plants are in equilibrium with atmospheric radiocarbon through respiration. This equilibrium continues through plants to herbivores and through them to carnivores. Once an organism dies, its carbon ceases exchanging with atmospheric carbon but continues decaying with a half-life of about 5730 years. Thus, measurement of the radiocarbon concentration can give the time that the organism died. Early measurements were done by counting the beta particles (high energy electrons) liberated in radiocarbon decay. The age limit was roughly 30k years, due both to poor statistics from low decay count rates and to cosmic ray backgrounds. Richard Muller proposed a new measurement technique, called "accelerator mass spectrometry" (AMS), in 1976 [3]. Muller suggested that particle accelerators be used to separate the atoms, allowing the radiocarbon atoms to be counted directly instead of waiting for them to decay. It was hoped that this would enable dating of much smaller and perhaps much older samples. This technique has indeed allowed use of much smaller samples and has become the dominant method of radiocarbon dating. However, the original anticipation of 100,000-year background levels has been "unrealized due to a variety of sample processing and instrument-based experimental constraints" [4].
Radiocarbon, 1971
Dates listed below are based on measurements made from June 1968 to May 1970 by the liquid scintillation technique using benzene. In general, the experimental procedure is as described previously (Barker, Burleigh, and Meeks, 1969a) with a few changes in detail. Data are now processed by computer using a comprehensive Algol program written by Andrew Barker, King's College, Univ. of London. There is no need to standardize on any particular sample weight and, as the benzene synthesizer can also deal with samples in the range up to the equivalent of 9 gm of carbon in a single synthesis, the amount of sample available is now less critical. However, for older material, a minimum of 1 gm of carbon is required. Another factor contributing to efficiency of operation is the "bomb" technique for sample combustion (Barker, Burleigh, and Meeks, 1969b), also mentioned in the previous date list. Finally, during 1969, an MS20 double collection mass spectrometer was acquired and all dates (but not all those in this list) are now corrected for isotopic fractionation. Samples were pretreated for removal of contaminants, with dilute hydrochloric acid and, where appropriate, with dilute alkali also. Bone and antler samples were demineralized in low vacuum with 0.75 N hydrochloric acid at ambient temperature, leaving only the protein fractiori (collagen) which was washed and dried before combustion. Dates were calculated using the Libby half-life for C14 of 5568 years. Descripdons, comments, and references to publications are based on information supplied by the persons who contributed the samples. ACKNOWLEDGMENT Thanks are due to Miss G. I. Hassall, National Physical Laboratory, for isotopic fractionation measurements made in connection with the investigation of C14 age discrepancies using well-dated Egyptian materials.
Radiocarbon, 2001
Initially, radiocarbon dating by bomb14C was used to check vintages of wine and whisky and to estimate the turnover times of carbon in various biological tissues. However, this technique has never been widely used for routine dating, although it has a wide field of application in geriatric medicine and forensic investigations. Fifteen years' experience in this field has shown the potential and limits of this technique. Taking into account the decisive biological factors, such as growth and aging, a complicated picture is obtained. Recent human bones cannot be dated with a constant precision. Despite an incomplete understanding of the process of incorporation of14C into human bones, the present dating technique is still more precise than most estimates by geriatric experts, for conventional14C dating follows that14C dates of bone collagen represent the years of the termination of puberty rather than those of death.Another application is the identification of furs of illegally hun...
The 1950s, era of the first radiocarbon revolution, saw famous clashes between confidence in the old chronologies and the new results from radiocarbon, which sometimes appeared ‘archaeologically unacceptable’. The same issues continue in respect of the radiocarbon dating of rock art, where the sheer technical difficulty of securing a dating number in which one can have confidence, remains a large real obstacle.
The article addresses the methodological question of the potential of the radiocarbon method in the dating of historical events. The archaeological investigations in Yaroslavl (Central Russia) are an example. The IARAS has been conducting excavations at the site for many years, and many archaeological complexes dating to different times have come to light. The most interesting of them are connected with the founding of the city by prince Yaroslav the Wise (the first fortifications) and with the devastation of the town by the Tatar Mongols in 1238 (sanitary mass burials of the town's inhabitants).
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