Radioactive isotopes emit radiation in the form of alpha, beta, positron or gamma rays to become a stable isotope of any given particular element. This is caused by the instability of the nucleus of the atom. The stabilising process in which unstable atoms undergo is known as radioactive decay.
Isotopes that are stable do not emit radiation. For example; Carbon-12 is stable and carbon-14 is radioactive.
Radioactive isotopes emit radiation in the form of alpha, beta, positron or gamma rays to become a stable isotope of any given particular element. This is caused by the instability of the nucleus of the atom. The stabilising process in which unstable atoms undergo is known as radioactive decay.
Isotopes that are stable do not emit radiation. For example; Carbon-12 is stable and carbon-14 is radioactive.
Unless you http://wiki.answers.com/wiki.phtml?title=Special:Userlogin&returnto=What_is_the_differents_between_radioactice_isotope_and_stable_isotope your contributions will be anonymous. However, your computer's internet address will be recorded so that contributors can trace http://wiki.answers.com/Q/WikiFAQs:Tips_for_Vandals and http://wiki.answers.com/Q/WikiFAQs:Tips_for_Spammers. "What is the differents between radioactice isotope and stable isotope?"
A stable isotope will not decay. A radioactive isotope is expected to decay over time and the term "half-life" describes the time period in which it will happen. Given a mole of radioactive atoms, half will have decayed in the half-life, then a half of the remaining will decay in the next half-life period, and so on. There is no predicting for any particular atom, we must simply treat it as a matter of probability.
The radioactive isotope is disintegrated in time and emit radiations.
Radioactive minerals are unstable and emit radiation at a constant rate. They also have half lives and lose energy overtime. Nonradioactive minerals are stable, and by there own are incapable of emitting energy.
it must eject the extra nucleons and should be conveted into a stable isotope.
The parent isotope is the original radioactive isotope that undergoes decay to form the daughter isotope. The daughter isotope is the stable isotope that is formed as a result of the radioactive decay of the parent isotope.
daughter isotope
The stable isotope produced by radioactive decay is called a daughter isotope.
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.
The radioactive isotope is disintegrated in time and emit radiations.
The radioactive isotope is disintegrated in time and emit radiations.
Radioactive minerals are unstable and emit radiation at a constant rate. They also have half lives and lose energy overtime. Nonradioactive minerals are stable, and by there own are incapable of emitting energy.
it must eject the extra nucleons and should be conveted into a stable isotope.
Radiogenic isotopes are formed through the radioactive decay of parent isotopes, while stable isotopes do not undergo radioactive decay. Radiogenic isotopes are used in geochronology to date rocks and minerals, while stable isotopes are used in various fields such as climate science and nutrition studies.
The parent isotope is the original radioactive isotope that undergoes decay to form the daughter isotope. The daughter isotope is the stable isotope that is formed as a result of the radioactive decay of the parent isotope.
daughter isotope
Phosphorus-31 (31P) is a stable isotope of phosphorus that is commonly used in nuclear magnetic resonance (NMR) spectroscopy, while phosphorus-32 (32P) is a radioactive isotope of phosphorus commonly used in biological research for labeling and tracking DNA and proteins. The main difference is the stability of the isotopes, with 31P being stable and 32P being radioactive.
When an isotope is stable, it does not undergo radioactive decay. Stable isotopes have a balanced number of protons and neutrons in the nucleus, which prevents them from spontaneously changing into another element over time.
The process where an unstable parent isotope becomes a stable daughter isotope is called radioactive decay. During this process, the parent isotope undergoes a series of transformations, such as alpha or beta decay, emitting particles or energy until it reaches a stable state as a daughter isotope.