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Conventional Radiocarbon Age (CRA): The age obtained from a radiocarbon measurement using conventions set out in a paper by Stuiver & Polach (1977).
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Eg the hydrogen nucleus consists of a single proton, so hydrogen has atomic number 1, the carbon nucleus has 6 protons and carbon has atomic number 6.
The atomic number defines each element: the carbon isotopes 12C, 13C and 14C all have atomic number 6.
top B Becquerel: SI unit of radioactivity, defined as one disintegration per second. Bomb Carbon (Bomb Spike): This expression refers to the significant quantity of 14C that was injected into the atmosphere by nuclear weapons testing between 1945 and the mid 1970s.
The increased activity reached its peak around 1963; atmospheric 14C reached twice the normal level in the Northern Hemisphere and increased by about 60% in the Southern Hemisphere. Calibration: The process of converting a conventional radiocarbon age to a "true" or calendar age.
The modern standard activity is defined for 1950, so measurements made at a later time must correct the measured oxalic activity for decay since that year.
For example, in the year 2000, the modern standard activity will have declined from 0.227 Becquerels/gram to 0.225 Becquerels/gram.
Chemical reactions are not the only causes of fractionation.
Evaporation, condensation, diffusion or the passage of vapour through a small aperture can also give rise to isotopic fractionation.
Generally, lighter isotopes will proceed more quickly than heavier isotopes.