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stable isotope
(redirected from Isotopic fractionation)

   Also found in: Encyclopedia, Wikipedia 0.01 sec.
stable isotope
n.
An isotope of an element that shows no tendency to undergo radioactive breakdown.

isotope [i´so-tōp]
a chemical element having the same atomic number as another (i.e., the same number of nuclear protons), but having a different atomic mass (i.e., a different number of nuclear neutrons).
radioactive isotope radioisotope.
stable isotope one that does not transmute into another element with emission of corpuscular or electromagnetic radiations.

isotope (ī´sōtōp),
n one of several nuclides having the same number of protons in their nuclei, and hence having the same atomic number but differing in the number of neutrons, and therefore in the mass number. The isotopes of a particular element have virtually identical chemical properties.
isotope, stable,
n a nonradioactive isotope of an element.

stable,
adj the term applied to a substance that has no tendency to decompose spontaneously. As applied to chemical compounds, it denotes their ability to resist chemical alterations.
stable isotope,
n See isotope.

isotope
a chemical element having the same atomic number as another (i.e. the same number of nuclear protons), but having a different atomic mass (i.e. a different number of nuclear neutrons).

radioactive isotope
one having an unstable nucleus and which emits characteristic radiation during its decay to a stable form. See also radioisotope.
stable isotope
one that does not transmute into another element with emission of corpuscular or electromagnetic radiations.


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A preliminary report on stable carbon and nitrogen isotopic fractionation between diets and tissues of Haliotis discus hannai INO.
However, this technique has also implications on the consistency of isotopic fractionation between the consumer and its diet with the generally accepted fractionation factors in the literature (DeNiro & Epstein 1978, Minagawa & Wada 1984).
The background to the topic is clearly explained by an overview of the isotopic fractionation patterns between seawater and the host minerals, and the possible modifications to seawater isotopic signatures by various diagenetic processes.
 
 
 
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