Iodine 131 is a radioisotope with a very short half-life of 8.02 days, making it highly radioactive. Frequently used in small doses in thyroid cancers therapies, it is also one of the most feared fission products when accidentally released into the environment.
In medicine, iodine 131 is primarily used to study the functionning of the thyroid though it can also be employed in the treatment of hyperthyroidism as well as thyroid cancer. The first production of iodine 131 in France took place in 1949 at the Fort de Chatillon, the site of the first Zoe atomic reactor, before manufacture was transferred to the nuclear research centre at Saclay. The isotope had been used since 1942, however, in the treatment of thyroid cancer.
Though used in low doses for medical examinations, iodine 131 is an ideal tracer for use in humans. Only a few radioactive atoms need to be inserted into the bloodstream for the iodine path to be accurately monitored. The atoms integrate into molecules that eventually transform into thyroid hormones; this is particularly interesting, given that iodine attaches itself exclusively to the thyroid gland. Gamma ray scintigraphy scans can thus monitor the thyroid activity and flag up the appearance of any anomalies. In recent years, iodine 131 has been abandoned in favour of another isotope, iodine 132 – a gamma emitter with a half-life of only 13.2 hours.
Stronger doses of iodine 131 are also used in radioactive therapies aimed at dealing with thyroid cancers. Iodine is inserted into the bloodstream in the same manner, and the short trajectory of the emitted beta particles guarantees that the radiation only affects a comparatively small part of the body.
Iodine 131 is also a feared fission product, posing as it does the principal risk for short-term contamination in the event of accidental waste release. From a chemical point of view, iodine is a halogen (similar in structure to chlorine and fluorine) and its high volatility means that it easily transforms into a purple vapour.
Volatile and highly mobile in the environment as volatile, radioactive iodine isotopes follow the usual transfer processes to the food chain : dispersion, deposits, uptake by plant leaves, root absorption, ingestion by animals and humans. Ingested by animals during lactation, iodine deposited on the grass finds its way in milk a few hours after ingestion, the maximum appearing after three days.
After a nuclear or radioactivity accident, the iodine-131 should be monitored in the food chain forseveral weeks, until it disappears radionuclide, specially in milk and vegetables, especially and large leaves vegetables like spinach and lettuce. Water should also be monitored.
In any case, the high radioactivity of iodine 131 is somewhat offset by its high decay rate, with the level of activity dropping by a factor of 1000 every eighty days. There are also procedures for us to protect ourselves from it before it decays.
Other radioactive isotopes of iodine have very short lifetimes such as iodine-132 and iodine-133 whose periods are 20.8 and 2.3 hours. These isotopes deliver almost their radiatioactivity in the early days after a reactor is shutdown.