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It is important to keep in mind that a radiocarbon measurement would also be destructive if mass spectrometry was applicable
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It is important to keep in mind that a radiocarbon measurement would also be destructive if mass spectrometry was applicable.
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84889334287
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As mentioned in the Introduction, almost all natural carbon on Earth is represented by the isotope 12C, thus the concentration 14R can be defined as the ratio between the number of atoms of 14C and atoms of 12C
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As mentioned in the Introduction, almost all natural carbon on Earth is represented by the isotope 12C, thus the concentration 14R can be defined as the ratio between the number of atoms of 14C and atoms of 12C.
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It is important to remember that sometimes
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in spite of the excellent performances of an AMS measurement, the final uncertainty on the true calendar age of a sample is a function of the behaviour of the calibration curve in that time interval: a small error on the radiocarbon age does not necessarily correspond to a small, or a unique, calendar span on the BC/AD axis
-
It is important to remember that sometimes, in spite of the excellent performances of an AMS measurement, the final uncertainty on the true calendar age of a sample is a function of the behaviour of the calibration curve in that time interval: a small error on the radiocarbon age does not necessarily correspond to a small, or a unique, calendar span on the BC/AD axis.
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35
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84889483675
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The reasons will be clearer after Section 16.4
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where AMS radiocarbon sample preparation procedures will be described. Now we would simply like to recall that in preparing graphite pellets for the sputtering source, after a physical-chemical cleaning, samples to be dated are usually combusted to obtain CO2, which is then converted to graphite by a further step. In this process, the main problem with small samples (a few tens of micrograms) is the possible introduction of contamination
-
The reasons will be clearer after Section 16.4, where AMS radiocarbon sample preparation procedures will be described. Now we would simply like to recall that in preparing graphite pellets for the sputtering source, after a physical-chemical cleaning, samples to be dated are usually combusted to obtain CO2, which is then converted to graphite by a further step. In this process, the main problem with small samples (a few tens of micrograms) is the possible introduction of contamination.
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The measurement of both 14C and 12C is necessary to estimate the radiocarbon age on the basis of the isotopic ratio 14R; measuring 13C allows us to evaluate the effects of isotopic fractionation, according to which the measured radiocarbon concentration can be corrected. For details, see Aitken.1
-
The measurement of both 14C and 12C is necessary to estimate the radiocarbon age on the basis of the isotopic ratio 14R; measuring 13C allows us to evaluate the effects of isotopic fractionation, according to which the measured radiocarbon concentration can be corrected. For details, see Aitken.1
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