the type of isotope
The istopes and that's it.
For a given isotope of a given element, the half-life is generally considered to be a constant. But there is more.
Different isotopes of different elements have unique half-lives. The half-life for a given element is based on the constituent isotopes in a sample: different isotopes of the same element can vary greatly in their half-lives.
It is the configuration of the nucleus which means it is either stable or unstable, giving rise to radioactive decay. Essentially it is the balance of the forces within the nucleus, between the protons and neutrons in it, that determines this. Thus you can have a stable nucleus of an element but adding another neutron upsets this and produces instability.
There are so many different radioisotopes it would take an encyclopedia to describe them all. What can definitely be said is that once a radioisotope is formed, its activity will follow the half-life curve regardless of external conditions such as temperature. The only way to change it is to irradiate it again in a reactor (neutron flux) to access the nucleus itself.
The half-life of any particular radioactive substance (isotope) is constant. It does not change as it decays. However, when decay does occur, there is a tendency to form other radioactive isotopes, what we call daughter products, and those can and do have their own half-lives. This, of course, complicates the measure of half-life, and forces analysis of energy levels and other chemical properties, i.e. not just count rate, in order to assess activity and its related half-life.
"Time required to reach the initial concentration oe a reactant to it half value is called half life period."
What are "the following"? However half life is a property of a particular isotope and can't be changed for that one, so the only way to change it is to convert it to a different isotope by neutron irradiation.
the type of isotope
In general, and at temperatures one might commonly find on Earth, temperature has
no appreciable effect on half life. If the temperature of an atom is elevated sufficiently,
we can get effects in which the question of half life becomes moot, because the atom is
no longer able to hold together in atomic form, but I am supposing that is not what this
question is about. There are certain circumstances, under which the half life might be
affected by temperatures that a person might consider more ordinary. One such place is
in a neutron rich environment, such as in the core of a nuclear reactor. Neutrons colliding
with the nuclei of atoms can cause the atom to become a different isotope of the same
element, to decay, or to undergo fission. The probability of the neutron colliding with the
nucleus depends on what is called the "nuclear cross section" which is measured in a unit
called a "barn." The nuclear cross section generally increases with temperature, though as
the temperature increases, the actual value goes up and down, depending on the
temperature and the specific isotope involved. So, in a neutron rich environment,
increasing the temperature generally reduces the half life.
All very interesting, I'm sure. Now, let me attempt an answer to the question:
For a large enough sample with enough atoms in it, the half-life doesn't change
as time passes and the atoms in the sample decay. If the half-life depended on
how much of the original sample remains, then there wouldn't be any such thing
as the 'half life' of a radioactive substance at all. It would have to be "the half-life
of this substance after 30 percent of it has already decayed" or some such number.
But you never see that. You only see "the half-life of this substance", and it doesn't
matter how much of it you start with, or how much of the original sample has already
decayed.
For a nucleus stationary by your side, nothing whatsoever. However, if the nucleus is passing you near the speed of light, relativistic effects will make the halflife seem to increase.
Under normal circumstances, nothing can affect the half-life.
anything but the isotope
12.5%
No, the half-life of a radioactive isotope does not decrease as the isotope decays. That half-life remains constant. It's the amount of the substance that decreases as the isotope decays.
The half-life of a radioactive substance that decays from 2.4g to 1.8g in 66 hours is 159 hours. AT = A0 2(-T/H) 1.8 = (2.4) 2(-66/H) 0.75 = 2(-66/H) log2(0.75) = log2(2(-66/H)) -0.415 = -66/H H = 159
If I take a radioactive sample of 400 moles of an unknown substance and let it decay to the point of three half-lives I would have 50 moles left of the sample. 1/2 of what is left will decay in the next half-life. At the end of that half-life I will have 25 moles left of the unknown substance or 4/25.
Iodine-125 (53125I) decays by beta+ decay, with a half-life of 59.4 days, to tellurium-125 (52125Te), which is stable and non-radioactive.
12.5%
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.
No, the half-life of a radioactive isotope does not decrease as the isotope decays. That half-life remains constant. It's the amount of the substance that decreases as the isotope decays.
The half-life of a radioactive substance that decays from 2.4g to 1.8g in 66 hours is 159 hours. AT = A0 2(-T/H) 1.8 = (2.4) 2(-66/H) 0.75 = 2(-66/H) log2(0.75) = log2(2(-66/H)) -0.415 = -66/H H = 159
The half-life directly affects how quickly something decays. It is the amount of time for a substance to lose half of its material, so the lower the half-life time, the faster something decays.
Iodine-131 has a half-life of about 8 days.
If I take a radioactive sample of 400 moles of an unknown substance and let it decay to the point of three half-lives I would have 50 moles left of the sample. 1/2 of what is left will decay in the next half-life. At the end of that half-life I will have 25 moles left of the unknown substance or 4/25.
Iodine-125 (53125I) decays by beta+ decay, with a half-life of 59.4 days, to tellurium-125 (52125Te), which is stable and non-radioactive.
The time required for half of the atoms in a radioactive substance to disintegrate.
Half-life
Radioactive decay has a constant rate of change, therefore it con be used to somewhat accurately tell the age of an object if you work backwards through the use of half-lifes (half of the existing radioactive material decays, leaving half of the original in its original form)
That is the half-life - the 6 hours in this case.That is the half-life - the 6 hours in this case.That is the half-life - the 6 hours in this case.That is the half-life - the 6 hours in this case.