Natural abundance

From Wikipedia, the free encyclopedia

Jump to: navigation, search

In chemistry, natural abundance (NA) refers to the prevalence of isotopes of a chemical element as naturally found on a planet. The relative atomic mass (a weighted average) of these isotopes is the atomic weight listed for the element in the periodic table. The abundance of an isotope varies from planet to planet but remains relatively constant in time.

As an example, uranium has three naturally occurring isotopes: U-238, U-235 and U-234. Their respective NA is 99.2745%, 0.72% and 0.0055%. For example, if 100,000 uranium atoms were analyzed, one would expect to find approximately 99,275 U-238 atoms, 720 U-235 atoms, and no more than 5 or 6 U-234 atoms. This is because U-238 is much more stable than U-235 or U-234, as the half-life of each isotope reveals: 4.468×109 years for U-238 compared to 7.038×108 years for U-235 and 245,500 years for U-234.

[edit] See also


af:Natuurlike verspreiding

ar:توافر طبيعي للنظائر الكيميائية ast:Abondanza natural ca:Abundància natural de:Natürliche Häufigkeit es:Abundancia natural ko:자연존재비 it:Abbondanza isotopica hu:Természetes előfordulás ms:Kelimpahan semulajadi nl:Relatieve aanwezigheid ja:天然存在比 nds:Vörkamen in de Natur pt:Abundância natural ro:Stare naturală sl:Pogostost izotopa zh:丰度

Views
Personal tools

Toolbox