decay constant
decay constant The probability that an atom of a radioactive isotope will decay within a stated period of time. Radioactive decay involves only the nucleus of the parent atom, and thus the rate of its decay is independent of all physical and chemical conditions (e.g. pressure, temperature, etc.) and follows an exponential law. The fundamental equation describing the rate of disintegration may be written as: −(dN/dt) = λN, where λ is the decay constant, representing the probability that an atom will decay in unit time t, and N is the number of radioactive atoms present. It is a fundamental assumption in geochronology that λ is a constant and that the only alteration in the amount of daughter or parent in the system is due to radioactive decay. The constant λ is usually expressed in units of 10^{−10} per year (e.g. ^{235}U is 9.72, ^{40}K is 5.31, ^{87}Rb is 0.139, and ^{238}U is 1.54). The total lifetime of a radioactive parent in a given system cannot be specified; in theory it is infinite. It is a simple matter, however, to specify the time for half of the radioactive parent atoms in a system to decay. This is called the ‘halflife’ (T), which is related to the decay constant by the expression T = 0.693/λ. See also decay curve.
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"decay constant." A Dictionary of Ecology. . Encyclopedia.com. 23 Oct. 2017 <http://www.encyclopedia.com>.
"decay constant." A Dictionary of Ecology. . Encyclopedia.com. (October 23, 2017). http://www.encyclopedia.com/science/dictionariesthesaurusespicturesandpressreleases/decayconstant0
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decay constant
decay constant Radioactive decay involves only the nucleus of the parent atom, and thus the rate of decay is independent of all physical and chemical conditions (e.g. pressure, temperature, etc.). The decay was shown by Rutherford to follow an exponential law. The fundamental equation describing the rate of disintegration may be written as: −(dN/dt) = λN, where λ is the decay constant, representing the probability that an atom will decay in unit time t, and N is the number of radioactive atoms present. It is a fundamental assumption in geochronology that λ is a constant and that the only alteration in the amount of daughter or parent in the system is due to radioactive decay. The constant λ is usually expressed in units of 10^{10} per year (e.g. ^{235}U is 9.72, ^{40}K is 5.31, ^{87}Rb is 0.139, and ^{238}U is 1.54). The total lifetime of a radioactive parent in a given system cannot be specified; in theory it is infinite. It is a simple matter, however, to specify the time for half of the radioactive parent atoms in a system to decay. This is called the ‘halflife’ (T), which is related to the decay constant by the expression T = 0.693/λ. See also DECAY CURVE.
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"decay constant." A Dictionary of Earth Sciences. . Encyclopedia.com. 23 Oct. 2017 <http://www.encyclopedia.com>.
"decay constant." A Dictionary of Earth Sciences. . Encyclopedia.com. (October 23, 2017). http://www.encyclopedia.com/science/dictionariesthesaurusespicturesandpressreleases/decayconstant
"decay constant." A Dictionary of Earth Sciences. . Retrieved October 23, 2017 from Encyclopedia.com: http://www.encyclopedia.com/science/dictionariesthesaurusespicturesandpressreleases/decayconstant