Half the original amount.
Radio active parent elements decay to stable daughter elements i.e. the radio active parent Potassium 40 decays to Argon 40 Each radioactive isotope has it's own half life A half life is the time it takes for the parent radioactive element to decay to a daughter product, Potassium 40 decays to Argon 40 with a half life of 1 1/4 billion years. Therin lies the problem of storing nuclear waste
Isotopes are atoms of a particular element with different numbers of neutrons. A radio isotope is an isotope that is radioactive because the nucleus is unstable.
to study the biochemical reaction, radio active isotopes aids as a labelling agent! it is widely used to study the metabolism.
A radio-isotope.
Radiochemicals are chemical compounds containing a radioactive isotope.
One eighth remains.
Radio active parent elements decay to stable daughter elements i.e. the radio active parent Potassium 40 decays to Argon 40 Each radioactive isotope has it's own half life A half life is the time it takes for the parent radioactive element to decay to a daughter product, Potassium 40 decays to Argon 40 with a half life of 1 1/4 billion years. Therin lies the problem of storing nuclear waste
Isotopes are atoms of a particular element with different numbers of neutrons. A radio isotope is an isotope that is radioactive because the nucleus is unstable.
to study the biochemical reaction, radio active isotopes aids as a labelling agent! it is widely used to study the metabolism.
an isotope that is radioactive
A radio-isotope.
Carbon 14 - it's the element used as a standard in radio-carbon dating.
radio-isotopes
a radio active substance has half life of 5 days initial mass of 12kg.how much the original isotope will remain after 10 days?
Radiochemicals are chemical compounds containing a radioactive isotope.
A nuclear equation describes nuclear decay.
Radiometric or Radio-active decay dating involves looking at certain radio-active isotopes in the rocks of the earth, such as potassium and argon. Certain Isotopes have a half life and decay into another isotope after a certain amount of years. Geochemists use these types of dating to determine the age of rocks and how long the crust has been forming and moving.