Radioactivity


        radioactivity

Marie Curie's main field of study, radioactive decay or radioactivity, is when an unstable molecule emits radioactive particles in order to become more stable.
These radioactive particles include alpha, beta, and gamma particles but scientists have more recently discovered more kinds of particles that may be released through radioactive decay. Each particle consists of different materials from the parent molecule. Alpha particles are composed of two protons and two neutrons and beta decay has to do with electron and positron emmision. Gamma decay occurs when alpha or beta particles are released in order to release excess energy from the molecule.

When a molecule emits radioactive particles it becomes more stable and in some cases results in an entirely different element forming after the decay has occurred. In some cases this new element created may then be radioactive itself which can create a cascading set of radioactive elements. Uranium is an element that does this sometimes, as seen below, after each decay another radioactive element is formed all the way to lead.decay chain
image from New Mexico Bureau of  Geology and Mineral Resources

 Each particle has different effects on the parent molecule and different levels of penetrating power seen in the image to the left. (picture from Wikipedia)
radioactive penetrating power

As shown in the picture alpha particles have the lowest amount of penetrating power and can be stopped by something as thin as a sheet of paper while beta particles require something such as a sheet of aluminum to stop them. Gamma particles are the strongest of these three and requires several inches of lead in order to be stopped.