Usually, 50%. That's what half-life means: the time required for 50% of the original radioisotope to undergo radioactive decay (or, alternatively, the time required for there to be a 50% chance that any given atom will have decayed). To be more specific: half of the original radioactive substance will have transformed into something else (it may still BE there, so in some sense it's "remaining", but it will be a different element or isotope). The reason for the "usually" is that it's a random process and for small numbers of atoms, the actual results may vary quite a bit from the statistically expected results. In particular, if there's only one atom, the amount remaining after one half-life period will be either 0% or 100% (50/50 chance of each).
After five half-lives, 3.125% of a radioisotope would be remaining in a sample.
The equation for half-life is ...
AT = A0 2(-T/H)
... where A0 is the initial activity, AT is the activity after some time T, and H is half-life in units of T.
AT = (1) 2(-5/1)
AT = 2-5
AT = 0.03125
Note: The question asked about percentage of daughter material, but that is not a valid concern because the daughter material can easily also decay and have its own half-life. It is more viable to ask how much of the parent remains, which is how I answered the question.
50 percent = half
(1/2)7 = 1/128 - less than 1%.
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 tells what fraction of a radioactive sample remains after a certain length of time.
The equation for half-life is AT = A0 2 (-T / H) where A0 is the starting activity, AT is the activity at some time T, and H is half-life in units of T. As a result, seven half-lives would be 2(-7) or 0.0078125 of the original activity.
The "radioactive" safety symbol warns you that radioactive material or a radiation producing machine is near the symbol and you should take precautions to ensure that you are not unnecessarily exposed to ionizing radiation.
Radioactive material is warmer than the surrounding material because radioactive material is constantly breaking down. When material breaks down, that means that energy is constantly getting released. When energy is released, it produces warmth.
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.
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.
Yes, this new daughter is a different chemical element and will react differently chemically than the precursor element.
Yes, there are a number of uses for radioactive material. It depends on the type of radioactive material.
We often use a Geiger counter to detect and count the decay of radioactive material.
All radioactive material has a characteristic half-life. This is a period during which half the matter from the original mass will have decayed into a daughter element. Either the daughter element is non-radioactive and therefore non-hazardous or it is radioactive and has its own half-life. The total radioactivity thus reduces over time and at some stage is deemed to reach a non-hazardous level.
3 half-lives
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.
As radium is radioactive, radium chloride would also be radioactive. Any compounds make with any radioactive material are radioactive, and they cannot be "not" radioactive. Radioactive material doesn't really care if it is "alone" or in compound; it will be radioactive in any case.
The core of the earth is radioactive, as is the sun. Granites, which crystallize from mantle material are commonly slightly radioactive.
Radioactive Contamination
400 yrs