absolute age
By looking at the half-life of a radionuclide (as well as its chemistry), we can select which one will be best for determining the age of rock. The longer the half-life, the "farther back" in time we can measure to discover some things about when it originated.
Abiotic factor.
The absolute age of a rock is determined by the amount of decay of certain elements as interpreted from their known half-life. The absolute age is stated in a number of years with a margin of error, as opposed to the relative age, which is more of a range of years in which the rock could have formed, based on index fossil evidence and the law of superposition.
Plutonium has 20 isotopes; each isotope has another half-life. Please read: http://en.wikipedia.org/wiki/Isotopes_of_plutonium.
An element can be created in a particle accelerator or fusion reactor. It can also be "made" by waiting out the half-life of an element further down on the periodic table.
relative age
answer is b
Absolute Age
The half-life can be used to determine the absolute age because the original amount of the elements can be calculated from the current value.
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The time it takes for half the atoms in a sample of a radioactive element to decay is called the half life.
The length of time depends on the element and isotope, but the point at which half of the sample has decayed is known as the half-life.
Half life of an element can't be changed.. It is a characteristic of a radioactive element which is independent of chemical and physical conditions.. Half life is that time in which half of radioactive sample( i.e., a radioactive element) decomposes. So no matter what amount you take half life of an element remains same.
The most important is the half life; also the type of decay, energy of released particles.
The half-life of an isotope is how long it takes for half of the atoms in a mass to undergo radioactive decay. Say you have 40g of an elements isotope with a half-life of one year. After 1 year, there would be 20g of that isotope left, and 20g of a different isotope/element. After 2 years, there would be 10g, and so on...
The half-life is the time that it takes for 1/2 of a material to decay.
No, the half life remains exactly the same throughout