Carbon-14



Carbon-14
General
symbol radiocarbon,14C
Neutrons 8
Protons 6
Nuclide data
Natural abundance 1 part per trillion
Half-life 5730 ± 40 years
Isotope mass 14.003241 u
Decay mode Decay energy
Beta .156476[1] MeV

Carbon-14, 14C, or radiocarbon, is a radiocarbon dating method to date archaeological, geological, and hydrogeological samples.

There are three naturally occurring isotopes of carbon on Earth: 99% of the carbon is half-life of carbon-14 is 5730±40 years. It decays into nitrogen-14 through beta-decay.[2] The activity of the modern radiocarbon standard[3]is about 14 disintegrations per minute (dpm) per gram carbon [4].

The carbon-13 atoms) in order to trace them along chemical reactions involving the given compound.

Origin and radioactive decay of carbon-14

Carbon-14 is produced in the upper layers of the troposphere and the stratosphere by thermal neutrons absorbed by neutrons. The resulting neutrons (1n) participate in the following reaction:

1n + 14N → 14C + 1H

The highest rate of carbon-14 production takes place at altitudes of 9 to 15 km (30,000 to 50,000 feet) and at high geomagnetic latitudes, but the carbon-14 readily mixes and becomes evenly distributed throughout the atmosphere and reacts with carbon dioxide. Carbon dioxide also dissolves in water and thus permeates the oceans.

Carbon-14 can also be produced in oxygen.

Carbon-14 then goes through radioactive beta decay.

\mathrm{~^{14}_{6}C}\rightarrow\mathrm{~^{14}_{7}N}+ e^- + \bar{\nu}_e

By emitting an electron and an anti-neutrino, carbon-14 (half life of 5730 years) decays into the stable, non-radioactive isotope nitrogen-14.

Radiocarbon dating

See main article: Radiocarbon dating

Radiocarbon dating is a Nobel Prize in chemistry for this work. One of the frequent uses of the technique is to date organic remains from archaeological sites. Plants fix atmospheric carbon during photosynthesis, so the level of C-14 in plants at the time wood is laid down, or in animals at the time they die, equals the level of C-14 in the atmosphere at that time. However, it decreases thereafter from radioactive decay, allowing the date of death or fixation to be estimated. The initial C-14 level for the calculation can either be estimated, or else directly compared with known year-by-year data from tree-ring data (dendrochronology) to 10,000 years ago, or from cave deposits (speleothems), to about 45,000 years of age. A calculation or (more accurately) a direct comparison with tree ring or cave-deposit carbon-14 levels, gives the wood or animal sample age-from-formation. The technique has limitations within the modern industrial era, due to fossil fuel carbon (which has little carbon-14) being released into the atmosphere in large quantities, in the past several centuries.

Carbon-14 and fossil fuels

Most man-made chemicals are made of isotopic signature of a sample of carbonaceous material therefore indicates its possible contamination by biogenic sources or the decay of radioactive material in related geologic strata.

Carbon-14 and nuclear tests

  The above-ground nuclear tests that occurred in several countries between 1955 and 1963 dramatically increased the amount of carbon-14 in the atmosphere and subsequently in the biosphere; after the tests ended the atmospheric concentration of the isotope began to decrease. This enabled the determination of the birth year of a deceased individual: the amount of carbon-14 in tooth enamel is measured with accelerator mass spectrometry and compared to records of past atmospheric carbon-14 concentrations. Since teeth are formed at a specific age and do not exchange carbon thereafter, this method allows age to be determined to within 1.6 years. This method only works for individuals born after 1943,[7][8] and it must be known whether the individual was born in the Northern or the Southern Hemisphere.

Carbon-14 in the human body

Since essentially all sources of human food are derived from plants, the carbon that comprises our bodies contains carbon-14 at the same concentration as the atmosphere. The beta-decays from this internal radiocarbon contribute approx 1 mrem/year (.01 mSv /year) to each person's radon (which vary).

Carbon-14 can be used as a radioactive tracer in medicine. In the urea breath test, a diagnostic test for carbon dioxide, which can be detected by low-level counting of the patient's breath.[10]

See also

References

  1. ^ A.H Waptstra, G. Audi, and C. Thibault. AME atomic mass evaluation 2003. Retrieved on 2007-06-03.
  2. ^ What is carbon dating?. National Ocean Sciences Accelerator Mass Spectrometry Facility. Retrieved on 2007-06-11.
  3. ^ Carbon 14:age calculation. C14dating.com. Retrieved on 2007-06-11.
  4. ^ Class notes for Isotope Hydrology EESC W 4886: Radiocarbon 14C. Martin Stute's homepage at Columbia. Retrieved on 2007-06-11.
  5. ^ Arnold, J. R. and Libby, W. F. (1949) Age Determinations by Radiocarbon Content: Checks with Samples of Known Age, Science 110, 678–680.
  6. ^ Atmospheric δ14C record from Wellington. Oak Ridge National Laboratory. Retrieved on 2007-06-11.
  7. ^ Radiation in Teeth Can Help Date, ID Bodies, Experts Say, National Geographic News, 22 September 2005
  8. ^ Spalding KL, Buchholz BA, Bergman LE, Druid H, Frisen J. Forensics: age written in teeth by nuclear tests. Nature. 2005 Sep 15;437(7057):333-4. PMID 16163340
  9. ^ NCRP Report No. 93 (1987). Ionizing Radiation Exposure of the Population of the United States. National Council on Radiation Protection and Measurements.  (excerpt)
  10. ^ Society of Nuclear Medicine Procedure Guideline for C-14 Urea Breath Test (2001-06-23). Retrieved on 2007-07-04.
  • Kamen, Martin D. (1985). Radiant Science, Dark Politics: A Memoir of the Nuclear Age (foreword by Edwin M. McMillan), University of California Press, USA.
  • What is Carbon Dating?, Woods Hole Oceanographic Institute
 
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