Fermium is a new kind of stuff. 

Fermium is a special kind of matter. 

Making it is very hard. It is made by hitting small pieces of matter with tiny bits called neutrons. This makes the matter grow much heavier. 
Some parts of it stay around for a little while. Other parts go away very fast. We use it to study how the world works.
Fermium is a man-made chemical element. 


Making fermium is a very difficult task. It is made by hitting lighter elements with neutrons. Neutrons are tiny parts of an atom. This process makes the atoms much heavier. Fermium is the heaviest element we can make this way. It is also the last one we can make in large amounts. Most of it is made in nuclear reactors. One big reactor in Tennessee helps make it.
There are 20 known versions of fermium. We call these versions isotopes. Some isotopes stay around for a long time. One version lasts for 100.5 days. Other versions disappear very fast. Some last for only a few minutes. Because it is hard to make and goes away quickly, we only use it for science research.
Fermium is a man-made chemical element with the symbol Fm. It has the atomic number 100. This element is part of a group called actinides. 
Making fermium is a step-by-step process involving tiny particles. Scientists use a method called neutron bombardment to create it. In this process, they hit lighter elements with neutrons. These neutrons are absorbed by the nucleus of an atom. This makes the atom much heavier. 
Fermium has a very interesting history of discovery. It was first seen in the debris from a hydrogen bomb test. This test was called Ivy Mike and happened on November 1, 1952. 
There are many different versions of this element. We call these versions isotopes. Scientists know of 20 different isotopes of fermium. 
Understanding fermium helps us learn about the building blocks of our world. It shows how atoms change when they catch neutrons. This is similar to how adding weight to a backpack changes how you move. The way fermium behaves helps scientists study the rules of physics. 
Fermium is a synthetic chemical element with the symbol Fm and the atomic number 100. It belongs to a group of heavy elements known as actinides. 
The production of fermium relies on a process called neutron bombardment. In this mechanism, a nucleus of a lighter element absorbs neutrons to increase its mass. This can occur within a nuclear reactor, such as the 85 MW High Flux Isotope Reactor (HFIR) in Tennessee. This reactor is specifically dedicated to producing transcurium elements, which are elements with an atomic number greater than 96. During a typical campaign at Oak Ridge, scientists irradiate tens of grams of curium. This process yields milligram quantities of einsteinium and tiny picogram quantities of fermium. 
Scientists have identified 20 different isotopes of fermium, which are versions of the element with different atomic weights. These weights range from 241 to 260. The isotopes vary greatly in their stability. The longest-lived isotope is fermium-257, which has a half-life of 100.5 days. Other isotopes decay much faster. For example, fermium-255 has a half-life of about 20 hours. Some isotopes are extremely unstable, lasting only a few milliseconds. This rapid decay creates what scientists call the "fermium gap." This gap exists because no accessible fermium isotopes undergo beta minus decay to become mendelevium. Instead, they undergo spontaneous fission, where the nucleus splits apart.
The discovery of fermium is tied to the history of nuclear physics. It was first observed in the debris of the "Ivy Mike" hydrogen bomb test on November 1, 1952. 

During the mid-1950s, researchers attempted to create heavier elements using nuclear explosions. They hoped the massive neutron flux of a thermonuclear explosion would allow nuclei to capture more neutrons than a reactor could. The flux in an explosion can reach 10 neutrons per square centimeter within a microsecond. In comparison, the HFIR reactor provides about 5 neutrons per square centimeter per second. Despite these powerful tests, such as the "Hutch" test in 1969, no elements heavier than fermium were discovered. 
Collecting the products of these explosions proved to be a massive technical challenge. In atmospheric tests, the debris was spread across wide areas. Scientists tried using airplanes with paper filters to catch fallout, but this only captured a small fraction of the material. In underground tests, the debris was buried under 300 to 600 meters of rock. Even when researchers drilled shafts to help expel material, the concentration of actinides was often lower than expected. In the Hutch test, only 4.0 picograms of fermium-257 were recovered from 10 kilograms of debris. This showed that collecting these rare elements from a blast site is highly inefficient.
Fermium's chemistry is typical for the late actinides in the periodic table. It mostly exists in a +3 oxidation state, which is a way of describing its electrical charge. However, it also has an accessible +2 oxidation state. To isolate the element from other materials, scientists use ion-exchange chromatography. This process uses a cation exchanger and a solution called ammonium alpha-hydroxyisobutyrate. The different elements move through the column at different speeds, allowing researchers to separate the fermium. This specialized chemistry allows scientists to study the fundamental properties of the heaviest reachable elements.
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