How are half life and radiocarbon dating used by scientists
It can be applied to most organic materials and spans dates from a few hundred years ago right back to about 50,000 years ago - about when modern humans were first entering Europe.For radiocarbon dating to be possible, the material must once have been part of a living organism.
After rolling the 100 dice until all of the parents have transformed and studying the rate of decay of the imagined isotope, students can work backwards and deduce the age of a sample created by a friend or family member by correlating available data and comparing it to the decay curve.
Students will need a 100 'marked' dice (a piece of tape on one side of each) to conduct the "How Old Is That Rock?
Roll the Dice & Use Radiometric Dating to Find Out" hands-on geology project.
By evaluating the number of parent and daughter isotopes of an element that are present in an artifact, and by relating that number to the known half-life of the isotope, scientists can date the object.
Students often learn about radiocarbon dating, a form of radiometric dating based on the presence of carbon-14, which has a known rate of decay (or half-life).
Another form of radiometric dating involves potassium, which has a half-life of 1.25 billion years and changes to argon as it decays. Roll the Dice & Use Radiometric Dating to Find Out" geology Project Idea helps students better understand how radiometric dating works by using a hands-on game to simulate the process.