Production : chromatographic separation of Fm(100), Es(99), Cf, Bk, Cm and Am Fermium is produced by the bombardment of lighter
actinides with
neutrons in a nuclear reactor. Fermium-257 is the heaviest isotope that is obtained via neutron capture, and can only be produced in picogram quantities. The major source is the 85 MW
High Flux Isotope Reactor (HFIR) at the
Oak Ridge National Laboratory in
Tennessee, USA, which is dedicated to the production of transcurium (
Z > 96) elements. Lower mass fermium isotopes are available in greater quantities, though these isotopes (254Fm and 255Fm) are comparatively short-lived. In a "typical processing campaign" at Oak Ridge, tens of grams of
curium are irradiated to produce decigram quantities of
californium, milligram quantities of
berkelium and
einsteinium, and picogram quantities of fermium. However, nanogram Smaller cations form more stable complexes with the α-hydroxyisobutyrate anion, and so are preferentially eluted from the column. Although the most stable isotope of fermium is 257Fm, with a
half-life of 100.5 days, most studies are conducted on 255Fm (
t1/2 = 20.07(7) hours), since this isotope can be easily isolated as required as the decay product of 255Es (
t1/2 = 39.8(12) days). , 1962), Kennebec (<5 kilotons, 1963), Par (38 kilotons, 1964), Barbel (<20 kilotons, 1964), Tweed (<20 kilotons, 1965), Cyclamen (13 kilotons, 1966), Kankakee (20–200 kilotons, 1966), Vulcan (25 kilotons, 1966) and Hutch (20–200 kilotons, 1969), the last one was most powerful and had the highest yield of transuranium elements. In the dependence on the atomic mass number, the yield showed a saw-tooth behavior with the lower values for odd isotopes, due to their higher fission rates. In order to accelerate sample collection after the explosion, shafts were drilled at the site not after but before the test, so that the explosion would expel radioactive material from the epicenter, through the shafts, to collecting volumes near the surface. This method was tried in the Anacostia and Kennebec tests and instantly provided hundreds of kilograms of material, but with actinide concentrations 3 times lower than in samples obtained after drilling; whereas such a method could have been efficient in scientific studies of short-lived isotopes, it could not improve the overall collection efficiency of the produced actinides. Though no new elements (apart from einsteinium and fermium) could be detected in the nuclear test debris, and the total yields of transuranium elements were disappointingly low, these tests did provide significantly higher amounts of rare heavy isotopes than previously available in laboratories. For example, 6 atoms of Fm could be recovered after the Hutch detonation. They were then used in the studies of thermal-neutron induced fission of Fm and in discovery of a new fermium isotope Fm. Also, the rare isotope Cm was synthesized in large quantities, which is very difficult to produce in nuclear reactors from its progenitor Cm; the half-life of Cm (64 minutes) is much too short for months-long reactor irradiations, but is very "long" on the explosion timescale.
Natural occurrence Because of the short half-life of all known isotopes of fermium, any
primordial fermium, that is fermium present on Earth during its formation, has decayed by now. Synthesis of fermium from naturally occurring uranium and thorium in the Earth's crust requires multiple neutron captures, which is extremely unlikely. Therefore, most fermium is produced on Earth in laboratories, high-power nuclear reactors, or in
nuclear tests, and is present for only a few months afterward. The transuranic elements up to fermium should have been present in the
natural nuclear fission reactor at
Oklo, but any quantities produced then would have long since decayed away. ==Chemistry==