This is a special kind of rock. It is found deep in the Earth. It stays warm inside our ground. It helps us know how old rocks are. It is very old! Can you find a rock?
This is a special kind of rock. It is found deep in the Earth. It stays warm inside our ground. It helps us know how old rocks are. It is very old! It can stay the same for a long time. It can even turn into other things. This helps make new fuel for power. It is a very useful part of our world.
Uranium-238 is a type of uranium found in nature. It is very common. Over 99% of all natural uranium is this kind. It is a radioactive material. This means it slowly breaks down over time. It has a half-life of 4.463 billion years. A half-life is the time it takes for half of a sample to decay.
Because it breaks down, it makes heat. This heat makes up about 40% of the heat inside Earth. As it breaks down, it turns into other things. This set of steps is called a decay chain. One end product of this chain is lead. Scientists use this to study old rocks. This is called radiometric dating. It can help find the age of rocks older than 1 million years.
Uranium-238 can also help make fuel. In some reactors, it turns into plutonium-239. This new material can provide power. Some special machines called breeder reactors make more fuel than they use. Uranium-238 is also good at blocking radiation. It can stop gamma rays and X-rays very well.
Uranium-238 is a very important part of our natural world. It is the most common type of uranium found on Earth. In fact, more than 99% of all natural uranium is this specific isotope.
While it is not used for most standard nuclear reactions, it plays a huge role in how our planet works. It is a radioactive material, which means its atoms slowly break down over time. This slow breakdown releases energy that stays inside our planet. Because of this, Uranium-238 is responsible for about 40% of the radioactive heat produced deep within the Earth.
This material works in many interesting ways through a process called decay. When a Uranium-238 atom breaks down, it follows a long path called a decay chain. It turns into many different things, such as thorium, protactinium, and radium.
Eventually, this long chain ends when it turns into stable lead. This process is very slow because the isotope has a half-life of 4.463 billion years. Scientists use this predictable change to perform radiometric dating. By looking at the amount of lead left in a rock, they can find the age of materials older than 1 million years. This method has even helped find rocks that are 4.4 billion years old.
Humans have also found ways to use this material for energy. In a nuclear reactor, Uranium-238 can be turned into a different material called plutonium-239. This happens through a process called transmutation, where the atom changes into a new element.
Some special machines called breeder reactors are designed to do this very well. A breeder reactor actually creates more fuel than it uses up during its work. For example, the BN-600 reactor in Russia was a power-producing breeder reactor. Another unit called the BN-800 became fully operational in November 2016. These machines help turn fertile material into useful fuel for power plants.
Uranium-238 is also very useful for safety and protection. It is an excellent radiation shield. Because it has a high atomic weight and many electrons, it is great at absorbing X-rays and gamma rays.
It is actually five times better at blocking gamma rays than lead is. This means a shield made of uranium can be much thinner than a lead shield. Scientists are even looking at a special type of concrete called DUCRETE. This material uses uranium dioxide instead of gravel to help store radioactive waste safely. It helps keep the dangerous energy tucked away inside strong containers.
Even space travelers use this material. The Voyager spacecraft carry small amounts of pure Uranium-238 on their covers.
This material is also used in special tools to help control nuclear reactions. In some designs, it can even help make nuclear weapons more powerful. For instance, the Ivy Mike test in 1952 used a uranium tamper to create a huge amount of energy. However, most of our focus is on using it for electricity and science. From the heat in our Earth to the power in our homes, this common atom is everywhere.
Uranium-238, often called U-238, is the most common isotope found in nature. It makes up more than 99% of all natural uranium. While it is not fissile in standard thermal-neutron reactors, it is highly significant in science and energy. A fissile material can sustain a chain reaction, but U-238 cannot. Instead, U-238 is considered fertile. This means it can be transmuted, or changed, into plutonium-239. Plutonium-239 is a fissile isotope that can be used as fuel for nuclear reactors or in weapons. This unique ability makes U-238 a vital resource for future energy production.
The way U-238 interacts with neutrons is quite complex. In a typical reactor, U-238 cannot sustain a chain reaction because of inelastic scattering. This process reduces the energy of neutrons to a level where they cannot cause fast fission in the next generation of nuclei. However, U-238 is fissionable by fast neutrons. These are neutrons with high kinetic energy, specifically more than 1 MeV. When these fast neutrons hit a U-238 nucleus, they can cause it to split. This process can contribute between one and ten percent of all fission reactions in certain reactor designs.
Uranium-238 also acts as a natural safety mechanism in nuclear reactors. It undergoes a process called Doppler broadening. As the temperature of the fuel increases, the neutron absorption resonances of U-238 also increase. This means the material absorbs more neutrons as it gets hotter. This creates a negative feedback mechanism that helps control the reactor. This process helps prevent the nuclear reaction from growing too fast or becoming unstable. It is an essential part of keeping nuclear power plants running safely.
One of the most important aspects of U-238 is its radioactive decay. It is an alpha emitter with a very long half-life of 4.463 billion years. This long half-life means it decays very slowly over vast amounts of time. The decay of U-238 follows a long path called a decay chain, also known as the uranium series. It transforms through several stages, including isotopes like thorium-234, protactinium-234, and uranium-234. Eventually, the chain ends when the material becomes stable lead-206. This predictable decay is used in radiometric dating to find the age of rocks older than 1 million years.
Because of its slow decay, U-238 is a major source of energy for our planet. It is responsible for approximately 40% of the radioactive heat produced within the Earth. This heat comes from the decay of the isotope and its daughter products. As U-238 decays, it also contributes to a geoneutrino signal. Specifically, the decay chain produces six electron anti-neutrinos per U-238 nucleus. These particles can be detected from deep within the Earth. This allows scientists to study the internal processes of our planet from the surface.
Engineers use different forms of uranium for various technological needs. Depleted uranium has a very high concentration of U-238. Low-enriched uranium (LEU) also contains mostly U-238, though it has more U-235 than depleted uranium. Reprocessed uranium is also mainly U-238, but it contains different amounts of other isotopes like U-236 and U-232. U-238 is also excellent for radiation shielding. It is about five times better at blocking gamma rays than lead. Because of its high atomic weight, it can be used in thinner layers to absorb X-rays and gamma rays. Scientists are even testing DUCRETE, a concrete made with uranium dioxide, for storing radioactive waste.
Specialized machines called breeder reactors are designed to make the most of U-238. A breeder reactor creates more fissile material, like plutonium-239, than it actually consumes. This process turns fertile U-238 into usable fuel. In Russia, the BN-600 reactor was a 600-megawatt breeder reactor that produced power. A newer unit, the BN-800, became fully operational in November 2016. While some reactors, like Japan's Monju, have faced safety and design challenges, other nations like China and India have plans for breeder technology. These reactors could potentially provide energy for 10,000 to five billion years.
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