Radioactive decay is a function of quantum mechanical probability. When will something happen? It might happen now, it might happen next week, and it might not happen for a thousand years. Let's do a practical example with a deck of cards. A randomly arranged deck of cards is face down on the table and we're turning up cards. When will the next red card appear? The next club? The next face card? The next queen? Same with radioactive decay. You might see two in a second, and wait an hour for another decay. It's a "crap shoot" in that respect. Odd, huh? But that's the way it is. Note that radioactice decay is a statistically derived characteristic. But we've counted carefully and over a long enough period in each case we've investigated to get a "good" number for the half life of a given radionuclide. Certainly in the case of the exotic elements beyond plutonium we've had to work harder and our numbers are a bit less precise because of the small quantities and short half lives. And there are some "kinks" with measuring the half life of something like bismuth-209. Other than that, we're down with making the measurements and doing so with "good" accuracy. A link is provided.
The term for the element that a radioactive isotope decays into is called the "daughter product". During radioactive decay, the original isotope transforms into a different element or isotope through a series of decay reactions.
In chemistry, a parent element is a radioactive element that undergoes decay to form a different element known as the daughter element. The parent element gives rise to the daughter element as a result of radioactive decay processes such as alpha decay, beta decay, or electron capture. The daughter element has a different number of protons and atomic number compared to the parent element.
Radioactive decay occurs when the nucleus of an unstable element transforms into a more stable configuration by emitting particles or energy. During this process, the number of protons and neutrons in the nucleus may change, leading to the formation of a different element. This transformation follows specific decay pathways that are governed by the elements' atomic structures and decay modes.
The time it takes for half the atoms in a sample of a radioactive element to decay is called the half life.
To calculate the amount of a radioactive element compared to its original amount, you need to use the radioactive decay equation: A = A₀ * e^(-λt), where A is the final amount, A₀ is the initial amount, λ is the decay constant, and t is the time elapsed. By plugging in the values for A₀, t, and λ, you can determine the final amount of the radioactive element.
radioactive decay
A radioactive element (atom) can decay up to a stable isotope.
The lightest "element" that can undergo radioactive decay is the isotope hydrogen-3, which undergoes beta decay. The lightest element with no radioactively stable isotopes is technetium, and its isotopes have different modes of decay.
That would be radioactive decay.
A radioactive element is characterized by having unstable atomic nuclei that decay and emit radiation in the form of alpha particles, beta particles, or gamma rays. This decay process results in the transformation of the element into a different element or isotope.
To fully explain radioactive decay you need quantum mechanics.
i got no idea
When a radioactive element slowly turns into another element/s when it emits various particles.
Yes, but only if it is radioactive. Radioactive elements change into different elements through radioactive decay.
The name for the time required for half of a radioactive element to decay into a stable element is called the half-life. It is a constant value unique to each radioactive isotope, and it is used to measure the rate of radioactive decay.
The term for the element that a radioactive isotope decays into is called the "daughter product". During radioactive decay, the original isotope transforms into a different element or isotope through a series of decay reactions.
The half-life