Half-Life: The half-life is the time it takes for half of the radioactive isotopes in a sample to decay into a stable daughter product. Different isotopes have different half-lives, ranging from fractions of a second to billions of years.
Parent and Daughter Isotopes: In radiometric dating, the original radioactive isotope is known as the parent isotope, and the stable product of the decay is known as the daughter isotope.
Uranium-238 and Uranium-235: Used for dating rocks and minerals, with long half-lives of 4.5 billion and 704 million years, respectively.
Steps in Radiometric Dating
Sample Collection: A sample of the material to be dated is collected, such as a rock or fossil.
Isotope Measurement: The concentration of the parent and daughter isotopes in the sample is measured using specialized instruments, such as massspectrometers or Geiger counters.
Calculating Age: By knowing the half-life of the isotope and the ratio of parent to daughter isotopes, the age of the sample can be calculated using the decay equation.
Applications of Radiometric Dating
Radiometric dating has many practical applications in various fields, including:
By mastering these concepts, you'll have a solid understanding of radiometric dating and its significance in the study of Earth'shistory and the evolution of life on our planet.
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.