Since the material will lose one half the initial amount in the first 12,000 yrs. and then one half the remainder each additional 12,000 yrs, the amount remaining after 36,000 years will be 1/8'th the original amount.
1/2 remains after 12,000, then 1/2 of the half, or 1/4 remains after the second 12,000, and 1/2 the quarter, or 1/8'th after the third 12,000 years.
There is insufficient information in the question to provide a specific answer it.
The equation for radioactive decay is AT = A0 2(-T/H).
For the above equation, AT is the final amount, A0 is the initial amount, T is time elapsed (120 years), and H is the half-life. As you can see, there are three unknown variables. You must have two of them to be able to solve for the third. In this case, if the elapsed time is 120 years, you cannot know how much would be left unless you know the number of years in the half-life.
Let's see. 1g = 1,000 mg
2g = 2,000 mg
half life of tritium is 12 years.
How much will we have after 120 years?
We now have 2,000 mg
After 12 years 1,000 mg
After 24 years 500 mg
After 36 years 250 mg
After 48 years 125 mg
After 60 years 62.5 mg
After 72 years 31.25 mg
After 84 years 15.625 mg
After 96 years 7.8125 mg
After 108 years 3.90625 mg
After 120 years 1.953125 mg
Of course the above includes too many significant figures.
If we start out wit 2 g, we are probably measuring to 2 place accuracy.
The final result would probably look something like this.
We now have 2,000 mg
After 12 years 1,000 mg
After 24 years 500 mg
After 36 years 250 mg
After 48 years 130 mg
After 60 years 63 mg
After 72 years 31 mg
After 84 years 16 mg
After 96 years 7.8 mg
After 108 years 3.9 mg
After 120 years 2. mg
It indicates how long it takes for the material to decay.
They experience radioactive decay. They emit radiation, changing the state of their nucleus, usually by the loss of protons and neutrons. However, this process is completely random; it can only be predicted as a half-life, or the amount of time it takes half of a certain material to decay. This does not predict when an individual atom will decay, it only predicts when approximately half of the material will have decayed.
When a radioactive material undergoes radioactive decay, except spontaneous fission, a daughter product is formed. The daughter may or may not be radioactive. If it is, this daughter product begins its own evolution according to its decay scheme and its own half-life. Any daughter products from that decay event will either be stable or will decay according to how (un)stable the daughter is and what its half-life happens to be. The original radionuclide continues to decay in its own way. You can see a "dynamic" developing here. The fact that a radioactive material has a half-life doesn't speak to what happens to the material or to its daughter products. It is only a measure of the rate of decay of a material. Radioactive materials decay according to what they are, and their daughter products will, if they are not stable, undergo decay as well, each according to its own decay scheme. The half-life only puts a timeline on things. And it (the half-life idea) must be applied to each unstable daughter. A consequence of radioactive decay and inspection of the daughter products allows us to use radioactive decay schemes to date materials. There are a number of radionuclides that are useful in doing this, and the decay schemes are well known. We understand the decay rates of the original material and also its daughters, and by counting all of them, we can "rewind time" to the period when they were isolated and state with good accuracy when the material was sequestered. Different methods of dating materials might be applied, depending on the material and its age.
It is through radioactive decay that a quantity of an unstable element will decay over time. A material that is unstable will undergo this process, and the sample is said to be radioactive.
Radioactive decay may or may not involve electrons. There are different types of radioactive decay.
The length of time required for half of a sample of radioactive material to decay
The name for the emissions of rays and particles by a radioactive material are called radioactive decay. There are many different types of radioactive decay that emit different rays and particles.
We often use a Geiger counter to detect and count the decay of radioactive material.
Yes, alpha decay occurs naturally, that is why radioactive material is dangerous, because we can't simply "turn off" the radioactive decay.
The decay of radioactive isotopes.The decay of radioactive isotopes.The decay of radioactive isotopes.The decay of radioactive isotopes.
That depends on the radioactive material. But whether you use it or not, the radioactive material will decay into other elements over the course of time. The time it takes for half of the material to decay into something else is called the "half-life". The more radioactive the substance is, the faster it decays. The half-life of a radioactive element can be measured from fractions of a second to billions of years.
The decay of radioactive isotopes.The decay of radioactive isotopes.The decay of radioactive isotopes.The decay of radioactive isotopes.
It disintegrates into its daughter nuclei that are much more stabler than the radioactive nuclei. If a sample of radioacictive material is left it will decay into another element over a period of time. Note that complete decay is not possible. A fraction of the original radioactive material will always remain in the sample.
It indicates how long it takes for the material to decay.
It indicates how long it takes for the material to decay.
They experience radioactive decay. They emit radiation, changing the state of their nucleus, usually by the loss of protons and neutrons. However, this process is completely random; it can only be predicted as a half-life, or the amount of time it takes half of a certain material to decay. This does not predict when an individual atom will decay, it only predicts when approximately half of the material will have decayed.
When a radioactive material undergoes radioactive decay, except spontaneous fission, a daughter product is formed. The daughter may or may not be radioactive. If it is, this daughter product begins its own evolution according to its decay scheme and its own half-life. Any daughter products from that decay event will either be stable or will decay according to how (un)stable the daughter is and what its half-life happens to be. The original radionuclide continues to decay in its own way. You can see a "dynamic" developing here. The fact that a radioactive material has a half-life doesn't speak to what happens to the material or to its daughter products. It is only a measure of the rate of decay of a material. Radioactive materials decay according to what they are, and their daughter products will, if they are not stable, undergo decay as well, each according to its own decay scheme. The half-life only puts a timeline on things. And it (the half-life idea) must be applied to each unstable daughter. A consequence of radioactive decay and inspection of the daughter products allows us to use radioactive decay schemes to date materials. There are a number of radionuclides that are useful in doing this, and the decay schemes are well known. We understand the decay rates of the original material and also its daughters, and by counting all of them, we can "rewind time" to the period when they were isolated and state with good accuracy when the material was sequestered. Different methods of dating materials might be applied, depending on the material and its age.