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Radiometric dating is a means of determining the "age" of a mineral specimen by determining the relative amounts present of certain radioactive elements. By "age" we mean the elapsed time from when the mineral specimen was formed. Radioactive elements "decay" that is, change into other elements by "half lives. The formula for the fraction remaining is one-half raised to the power given by the number of years divided by the half-life in other words raised to a power equal to the number of half-lives. If we knew the fraction of a radioactive element still remaining in a mineral, it would be a simple matter to calculate its age by the formula.

The sum of protons plus neutrons is the mass number. We designate a specific group of atoms by using the term "nuclide. Only K40 is radioactive; the other two are stable. K40 can decay in two different ways: it can break down into either calcium or argon. The ratio of calcium formed to argon formed is fixed and known.

Therefore the amount of argon formed provides a direct measurement of the amount of potassium present in the specimen when it was originally formed. Because argon is an inert gasit is not possible that it might have been in the mineral when it was first formed from molten magma. Any argon present in a mineral containing potassium must have been formed as the result of radioactive decay.

F, the fraction of K40 remaining, is equal to the amount of potassium in the sample, divided by the sum of potassium in the sample plus the calculated amount of potassium required to produce the amount of argon found. The age can then be calculated from equation 1. In spite of the fact that it is a gas, the argon is trapped in the mineral and can't escape. Creationists claim that argon escape renders age determinations invalid. However, any escaping argon gas would lead to a determined age younger, not older, than actual. The creationist "argon escape" theory does not support their young earth model.

Examples of Radiometric Dating Uranium-lead (U-Pb) dating: Radioactive uranium comes in two forms, uranium and uranium The number refers to the number of protons plus neutrons. Uranium's atomic number is 92, corresponding to its number of protons. which decay into lead and lead respectively. Carbon, uranium, and potassium are just a few examples of elements used in radioactive dating. Each element is made up of atoms, and within each atom is a central particle called a nucleus. Within. Rubidium/Strontium Dating Example. For geologic dating, the age calculation must take into account the presence of the radioactive species at the beginning of the time interval. If there is a non-radiogenic isotope of the daughter element present in the mineral, it can be used as a reference and the ratios of the parent and daughter elements plotted as ratios with that .

The argon age determination of the mineral can be confirmed by measuring the loss of potassium. In old rocks, there will be less potassium present than was required to form the mineral, because some of it has been transmuted to argon. The decrease in the amount of potassium required to form the original mineral has consistently confirmed the age as determined by the amount of argon formed. Carbon dating: See Carbon 14 Dating in this web site.

## What are some examples of radioactive dating?

Rubidium-Strontium dating: The nuclide rubidium decays, with a half life of Strontium is a stable element; it does not undergo further radioactive decay. Do not confuse with the highly radioactive isotope, strontium Strontium occurs naturally as a mixture of several nuclides, including the stable isotope strontium If three different strontium-containing minerals form at the same time in the same magma, each strontium containing mineral will have the same ratios of the different strontium nuclides, since all strontium nuclides behave the same chemically.

Note that this does not mean that the ratios are the same everywhere on earth. It merely means that the ratios are the same in the particular magma from which the test sample was later taken. As strontium forms, its ratio to strontium will increase. Strontium is a stable element that does not undergo radioactive change.

In addition, it is not formed as the result of a radioactive decay process. The amount of strontium in a given mineral sample will not change. It turns out to be a straight line with a slope of The corresponding half lives for each plotted point are marked on the line and identified. Search for:. Dating Using Radioactive Decay. Learning Objective Calculate the age of a radioactive sample based on the half-life of a radioactive constituent.

Key Points The best-known techniques for radioactive dating are radiocarbon dating, potassium-argon dating and uranium-lead dating. In any material containing a radioactive nuclide, the proportion of the original nuclide to its decay products changes in a predictable way as the original nuclide decays over time. Show Sources Boundless vets and curates high-quality, openly licensed content from around the Internet. Licenses and Attributions. Using the radioactive decay equation as above, this becomes. Such a line is called an isochron since all the different minerals are presumed to have crystallized together and therefore have the same age since solidification. The age can then be calculated from that slope as follows:. For geologic dating, the age calculation must take into account the presence of the radioactive species at the beginning of the time interval. If there is a non-radiogenic isotope of the daughter element present in the mineral, it can be used as a reference and the ratios of the parent and daughter elements plotted as ratios with that reference isotope. The slope of the curve then gives the time interval. Radioactive Dating Because the radioactive half-life of a given radioisotope is not affected by temperature, physical or chemical state, or any other influence of the environment outside the nucleus save direct particle interactions with the nucleus, then radioactive samples continue to decay at a predictable rate and can be used as a clock.

For geologic dating, where the time span is on the order of the age of the earth and the methods use the clocks in the rocksthere are two main uncertainties in the dating process: What was the amount of the daughter element when the rocks were formed?

Rubidium-Strontium dating: The nuclide rubidium decays, with a half life of billion years, to strontium Strontium is a stable element; it . These radioactive timekeepers is used in radioactive dating the half-life for geologic dating, called radioactive isotope, along with the. Absolute age of fossils are two hikers discovered a few examples include uranium, there. After 86 minutes, will help scientists use the. 8 rows  Effective Dating Range (years) Dating Sample: Key Fission Product: Lutetium .

Have any of the parent or daughter atoms been added or removed during the process?     ## 1 thoughts on “Examples of radioactive dating”

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