There is no one answer for an individual atom, but for a given radioisotope we usually quantify the rate of decay via the half-life, i.e. the average time it takes for half of the atoms of an isotope to decay. Realizing that some isotopes will decay to another radioisotope before eventually decaying to a stable product, this can get even more complicated. In mathematical terms the equation for concentration of the radioisotope approaches zero asymptotically. The math says that you will never get zero concentration - but of course atoms are discrete entities so that once the concentration predicted by the math drops below one atom, you have reached zero in the real world.
No. Often a decay product is itself unstable and will decay into something else until a stable isotope is reached. This is called a decay chain. For example, Uranium-238 will decay 15 times through various isotopes until it becomes lead-206 which is stable
No. Barium 137 is stable and is not a radioisotope.
The half-life of the radioisotope Ba-137 is approximately 11.23 minutes. This means that it takes 11.23 minutes for half of a sample of Ba-137 to decay into a more stable element.
Yes, that is correct. Radioactive decay involves the transformation of an unstable parent isotope into a more stable daughter product through the emission of particles or energy. This process continues until the parent isotope reaches a stable configuration.
Argon-40 Naturally occurring K-40 with a half-life of 1.25×109 years, decays to stable Ar-40 (11.2%) by electron capture or positron emission.
The isomer Ag-108m has a half life of 418(21) years.
No. Often a decay product is itself unstable and will decay into something else until a stable isotope is reached. This is called a decay chain. For example, Uranium-238 will decay 15 times through various isotopes until it becomes lead-206 which is stable
No. Barium 137 is stable and is not a radioisotope.
The stable isotope formed by the breakdown of a radioactive isotope is called a daughter isotope. This process is known as radioactive decay, where a radioactive isotope transforms into a stable daughter isotope through the emission of particles or energy.
One-half of the original amount. That's precisely the definition of "half-life".
The half-life of the radioisotope Ba-137 is approximately 11.23 minutes. This means that it takes 11.23 minutes for half of a sample of Ba-137 to decay into a more stable element.
When a radioisotope emits radiation, it undergoes radioactive decay, transforming into a more stable element. This process releases energy in the form of radiation, which can be in the form of alpha particles, beta particles, or gamma rays.
PGA is the first stable product of The Calvin Cycle of photosynthesis.
The daughter product of potassium-40 is argon-40, which is formed through the process of radioactive decay. Potassium-40 undergoes electron capture to become argon-40, releasing a neutrino and a positron in the process. Argon-40 is stable and does not undergo further decay.
It is important for a radioisotope to have a known rate of decay in order to provide accurate dating results. This allows scientists to calculate the age of a material based on the amount of remaining radioisotope present. Additionally, having a stable and predictable decay process is crucial for determining the timing of past events with precision.
Yes, that is correct. Radioactive decay involves the transformation of an unstable parent isotope into a more stable daughter product through the emission of particles or energy. This process continues until the parent isotope reaches a stable configuration.
No. Often a decay product is itself unstable and will decay into something else until a stable isotope is reached. This is called a decay chain. For example, Uranium-238 will decay 15 times through various isotopes until it becomes lead-206 which is stable