Faster access than browser!Similarities between Background radiation and Radionuclide
Background radiation and Radionuclide have 25 things in common (in Unionpedia): Acute radiation syndrome, Alpha particle, Beta particle, Carbon-14, Cosmic ray, Cosmogenic nuclide, Electron, Electronvolt, Environmental radioactivity, Half-life, Ionizing radiation, Isotopes of radon, Isotopes of thallium, Neutron, Nuclear fallout, Nuclear medicine, Nuclear transmutation, Potassium-40, Radioactive contamination, Radioactive decay, Radiocarbon dating, Radium, Thorium, Uranium, Uranium-238.
Acute radiation syndrome
Acute radiation syndrome (ARS) is a collection of health effects that are present within 24 hours of exposure to high doses of ionizing radiation.
Acute radiation syndrome and Background radiation · Acute radiation syndrome and Radionuclide ·
Alpha particle
Alpha particles consist of two protons and two neutrons bound together into a particle identical to a helium-4 nucleus.
Alpha particle and Background radiation · Alpha particle and Radionuclide ·
Beta particle
A beta particle, also called beta ray or beta radiation, (symbol β) is a high-energy, high-speed electron or positron emitted by the radioactive decay of an atomic nucleus during the process of beta decay.
Background radiation and Beta particle · Beta particle and Radionuclide ·
Carbon-14
Carbon-14, 14C, or radiocarbon, is a radioactive isotope of carbon with an atomic nucleus containing 6 protons and 8 neutrons.
Background radiation and Carbon-14 · Carbon-14 and Radionuclide ·
Cosmic ray
Cosmic rays are high-energy radiation, mainly originating outside the Solar System and even from distant galaxies.
Background radiation and Cosmic ray · Cosmic ray and Radionuclide ·
Cosmogenic nuclide
Cosmogenic nuclides (or cosmogenic isotopes) are rare nuclides (isotopes) created when a high-energy cosmic ray interacts with the nucleus of an in situ Solar System atom, causing nucleons (protons and neutrons) to be expelled from the atom (see cosmic ray spallation).
Background radiation and Cosmogenic nuclide · Cosmogenic nuclide and Radionuclide ·
Electron
The electron is a subatomic particle, symbol or, whose electric charge is negative one elementary charge.
Background radiation and Electron · Electron and Radionuclide ·
Electronvolt
In physics, the electronvolt (symbol eV, also written electron-volt and electron volt) is a unit of energy equal to approximately joules (symbol J).
Background radiation and Electronvolt · Electronvolt and Radionuclide ·
Environmental radioactivity
Environmental radioactivity is produced by radioactive materials in the human environment.
Background radiation and Environmental radioactivity · Environmental radioactivity and Radionuclide ·
Half-life
Half-life (symbol t1⁄2) is the time required for a quantity to reduce to half its initial value.
Background radiation and Half-life · Half-life and Radionuclide ·
Ionizing radiation
Ionizing radiation (ionising radiation) is radiation that carries enough energy to liberate electrons from atoms or molecules, thereby ionizing them.
Background radiation and Ionizing radiation · Ionizing radiation and Radionuclide ·
Isotopes of radon
There are 35 known isotopes of radon (86Rn) from 195Rn to 229Rn; all are radioactive.
Background radiation and Isotopes of radon · Isotopes of radon and Radionuclide ·
Isotopes of thallium
Thallium (81Tl) has 37 isotopes with atomic masses that range from 176 to 212.
Background radiation and Isotopes of thallium · Isotopes of thallium and Radionuclide ·
Neutron
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Background radiation and Neutron · Neutron and Radionuclide ·
Nuclear fallout
Nuclear fallout, or simply fallout, is the residual radioactive material propelled into the upper atmosphere following a nuclear blast, so called because it "falls out" of the sky after the explosion and the shock wave have passed.
Background radiation and Nuclear fallout · Nuclear fallout and Radionuclide ·
Nuclear medicine
Nuclear medicine is a medical specialty involving the application of radioactive substances in the diagnosis and treatment of disease.
Background radiation and Nuclear medicine · Nuclear medicine and Radionuclide ·
Nuclear transmutation
Nuclear transmutation is the conversion of one chemical element or an isotope into another chemical element.
Background radiation and Nuclear transmutation · Nuclear transmutation and Radionuclide ·
Potassium-40
Potassium-40 (40K) is a radioactive isotope of potassium which has a very long half-life of 1.251 years.
Background radiation and Potassium-40 · Potassium-40 and Radionuclide ·
Radioactive contamination
Radioactive contamination, also called radiological contamination, is the deposition of, or presence of radioactive substances on surfaces or within solids, liquids or gases (including the human body), where their presence is unintended or undesirable (from the International Atomic Energy Agency - IAEA - definition).
Background radiation and Radioactive contamination · Radioactive contamination and Radionuclide ·
Radioactive decay
Radioactive decay (also known as nuclear decay or radioactivity) is the process by which an unstable atomic nucleus loses energy (in terms of mass in its rest frame) by emitting radiation, such as an alpha particle, beta particle with neutrino or only a neutrino in the case of electron capture, gamma ray, or electron in the case of internal conversion.
Background radiation and Radioactive decay · Radioactive decay and Radionuclide ·
Radiocarbon dating
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon.
Background radiation and Radiocarbon dating · Radiocarbon dating and Radionuclide ·
Radium
Radium is a chemical element with symbol Ra and atomic number 88.
Background radiation and Radium · Radionuclide and Radium ·
Thorium
Thorium is a weakly radioactive metallic chemical element with symbol Th and atomic number 90.
Background radiation and Thorium · Radionuclide and Thorium ·
Uranium
Uranium is a chemical element with symbol U and atomic number 92.
Background radiation and Uranium · Radionuclide and Uranium ·
Uranium-238
Uranium-238 (238U or U-238) is the most common isotope of uranium found in nature, with a relative abundance of 99%.
Background radiation and Uranium-238 · Radionuclide and Uranium-238 ·
The list above answers the following questions
- What Background radiation and Radionuclide have in common
- What are the similarities between Background radiation and Radionuclide
Background radiation and Radionuclide Comparison
Background radiation has 116 relations, while Radionuclide has 149. As they have in common 25, the Jaccard index is 9.43% = 25 / (116 + 149).
References
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