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The daughter isotope is the result of the radioactive disintegration of the parent isotope. For example radium is a product of the uranium disintegration.

The two isotopes have different chemical (different atomic numbers, etc.), physical and nuclear properties.

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Is it true that a stable radioactive isotope called the parent will decay and form daughter products?

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.


What is meant by parent atom and daughter atom in terms of radioactive decay how are these atoms used to date rocks or organism?

In radioactive decay, a parent atom is an unstable isotope that undergoes transformation over time, emitting radiation and decaying into a more stable isotope known as the daughter atom. The ratio of parent to daughter atoms in a sample can be measured to determine the age of rocks or organic materials through radiometric dating methods, such as carbon dating for organic materials or uranium-lead dating for rocks. By knowing the half-life of the parent isotope, scientists can calculate how long it has taken for a certain amount of the parent to decay into the daughter, thus estimating the age of the sample.


What is important of decay chain in isotopes?

In nuclear science, the decay chain refers to the radioactive decay of different discrete radioactive decay products as a chained series of transformations. Most radioactive elements do not decay directly to a stable state, but rather undergo a series of decays until eventually a stable isotope is reached.Decay stages are referred to by their relationship to previous or subsequent stages. A parent isotope is one that undergoes decay to form a daughter isotope. The daughter isotope may be stable or it may decay to form a daughter isotope of its own. The daughter of a daughter isotope is sometimes called a granddaughter isotope.


Which of these is most likely a characteristic of a parent isotope before it releases radioactive particles?

Parent isotopes are typically unstable and have excess energy, making them more likely to undergo radioactive decay to achieve a more stable state. Additionally, parent isotopes often have a longer half-life compared to their daughter isotopes.


At what point do isotopes stop decaying?

Isotopes do not stop decaying. The process of radioactive decay continues until the isotope reaches a stable state, which could be a different isotope or a non-radioactive element. The rate of decay can vary depending on the specific isotope.

Related Questions

Is it true that a stable radioactive isotope called the parent will decay and form daughter products?

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.


What is important of decay chain in isotopes?

In nuclear science, the decay chain refers to the radioactive decay of different discrete radioactive decay products as a chained series of transformations. Most radioactive elements do not decay directly to a stable state, but rather undergo a series of decays until eventually a stable isotope is reached.Decay stages are referred to by their relationship to previous or subsequent stages. A parent isotope is one that undergoes decay to form a daughter isotope. The daughter isotope may be stable or it may decay to form a daughter isotope of its own. The daughter of a daughter isotope is sometimes called a granddaughter isotope.


Which of these is most likely a characteristic of a parent isotope before it releases radioactive particles?

Parent isotopes are typically unstable and have excess energy, making them more likely to undergo radioactive decay to achieve a more stable state. Additionally, parent isotopes often have a longer half-life compared to their daughter isotopes.


Isotope A has half-life of seconds and isotope B has a half-life of millions of years which isotope is more radioactive?

Isotope A is more radioactive because it has a shorter half-life, indicating a faster rate of decay. A shorter half-life means that more of the isotope will undergo radioactive decay in a given time period compared to an isotope with a longer half-life.


If a radioactive isotope in a rock has a half-life of 10000 years and the ratio of radioactive parent to stable daughter is 1 to 3 how old is the rock?

At the time the rock is created, the radioactive isotope is present in that rock in a ratio of 1 to zero with regard to the stable daughter. After one half-life, which is 10,000 years, the isotope to daughter ratio is 1 to 1. After another half-life, which is another 10,000 years, the ratio is 1 to 3. The rock is 20,000 years old.To see it another way, after the first half-life is complete, half the material is the original isotope, and half is the daughter. That's a 1 to 1 ratio. After another half-life (another 10,000 years) has passed, half the original isotope that was left has become the daughter. That's one quarter more of the daughter that will be added to the quantity of the daughter existing after the first half-life. That means that one quarter of the original isotope will be left after 2 half-lives, and the rest (the other 3/4ths of the material) will be the daughter. The ratio of the original isotope to the daughter after 2 half-lives (20,000 years) is 1 to 3.


When an isotope decays over time and becomes a different element what is it called?

It is called radioactive decay. During this process, an unstable isotope loses energy or particles to become a more stable element.


At what point do isotopes stop decaying?

Isotopes do not stop decaying. The process of radioactive decay continues until the isotope reaches a stable state, which could be a different isotope or a non-radioactive element. The rate of decay can vary depending on the specific isotope.


What is the process in which one isotope changes to another isotope?

The process in which one isotope changes to another isotope is called radioactive decay. During this process, the unstable nucleus of an isotope emits radiation in the form of alpha particles, beta particles, or gamma rays to transform into a more stable isotope. The rate at which radioactive decay occurs is measured by the isotope's half-life.


Why are igneous rocks the best type of rock sample for radiomertic dating?

Because when they form, minerals in igneous rocks often contain only a parent isotope and none of the daughter isotope. This makes the isotope percentage more accurate and easier to interpret.


Definition of elements that are stable?

This is an element (more exactly an isotope) which is not radioactive.


What is half of a radioactive isotope?

Half of a radioactive isotope is an atom that would have half of the atomic number of the radioactive isotope. In the case of radium-88 (88Ra), half of the radioactive isotope would be ruthenium-44 (44Ru). This assumes that the protons do not break down and that none are lost to additional reactions with other elements or compounds. Electrons can be lost along the radioactive chain, resulting in an ion of ruthenium rather than an electrically neutral atom.


Compared to nitrogen-14 the radioactive isotope nitrogen-16 has?

Two more neutrons