# Radiometric dating equation used

This predictability allows the relative abundances of related nuclides to be used as a clock to measure the time it takes for the parent atom to decay into the daughter atom(s).

Accurate radiometric dating generally requires that: is the decay constant of the parent isotope, equal to the inverse of the radioactive half-life of the parent isotope times the natural logarithm of 2. Calculate the mass of Cs-137 that will be left after 90 years. First half-life (30 years): 100 grams of Cs-137 decays and 50 grams are left.

The methods work because radioactive elements are unstable, and they are always trying to move to a more stable state. This process by which an unstable atomic nucleus loses energy by releasing radiation is called radioactive decay.

The thing that makes this decay process so valuable for determining the age of an object is that each radioactive isotope decays at its own fixed rate, which is expressed in terms of its half-life.

Radiometric dating, often called radioactive dating, is a technique used to determine the age of materials such as rocks.

It is based on a comparison between the observed abundance of a naturally occurring radioactive isotope and its decay products, using known decay rates.

Radiometric dating, or radioactive dating as it is sometimes called, is a method used to date rocks and other objects based on the known decay rate of radioactive isotopes.

In many cases, the daughter nuclide is radioactive, resulting in a decay chain.It is the principal source of information about the absolute age of rocks and other geological features, including the age of the Earth itself, and it can be used to date a wide range of natural and man-made materials.The best-known radiometric dating techniques include radiocarbon dating, potassium-argon dating, and uranium-lead dating.The final decay product, lead-208 (208Pb), is stable and can no longer undergo spontaneous radioactive decay.Systems that have been exploited for radiometric dating have half-lives ranging from only about 10 years (e.g., tritium) to over 100 billion years (e.g., Samarium-147).

This chain eventually ends with the formation of a stable, nonradioactive daughter nuclide.