Francois Tissot works hard to measure and understand
Uranium isotopes in rocks and meteorites to learn about the early Solar System and early Earth.
1942 Sept 13The S - 1 Executive Committee recommends building a pilot plant based on Ernest O. Lawrence's cyclotrons to separate
uranium isotopes in Tennessee.
Not exact matches
Radioactive
isotopes of elements such as
uranium, potassium, and thorium are found
in a class of rocky meteorites known as chondrites.
The water contains a smattering of
uranium atoms that decay into a distinctive
isotope of thorium, which accumulates
in the calcite over millennia.
Knowing that
uranium and thorium decay into two lead «
isotopes» — which can be distinguished by their different physical properties — Soddy later measured the atomic weights of this stable element
in ores rich
in uranium and thorium, and found that they were 206.08 and 207.69, respectively.
Those segments with potentially hazardous amounts of
uranium - 235, the fissile
isotope of
uranium used
in nuclear reactors and weapons, will be removed and decontaminated.
Most nuclear reactors use
uranium fuel that has been «enriched»
in uranium 235, an
isotope of
uranium that fissions readily.
Uranium - 235 (U-235) is an isotope of uranium widely used for nuclear power generation and, like all other radioactive isotopes used in medicine, it has been also employed for diagnosis and treatment of diseased organs and
Uranium - 235 (U-235) is an
isotope of
uranium widely used for nuclear power generation and, like all other radioactive isotopes used in medicine, it has been also employed for diagnosis and treatment of diseased organs and
uranium widely used for nuclear power generation and, like all other radioactive
isotopes used
in medicine, it has been also employed for diagnosis and treatment of diseased organs and tumors.
In nature,
uranium occurs as a mixture of two
isotopes, the easily fissionable
uranium 235 (which is said to be «fissile») and the much more stable
uranium 238.
Overall, the tanks hold every element
in the periodic table, including half a ton of plutonium, various
uranium isotopes and at least 44 other radionuclides — containing a total of about 176 million curies of radioactivity.
In the 1980s the antineutrino spectra of three main fuel
isotopes,
uranium 235, plutonium 239 and plutonium 241, were determined.
A few studies have found naturally occurring radioactive materials
in the solid waste, but the research only focused on several long - lived radioactive
isotopes including
uranium - 238 and radium - 226.
The concentration of this
isotope must therefore be boosted
in natural
uranium before it can function as nuclear power plant fuel.
By applying
uranium - thorium dating to the corals and measuring ratios of oxygen
isotopes in their skeletons, her lab reconstructed ocean temperatures for much of the last 7000 years.
By studying the variations of
uranium isotopes recorded
in carbonates, the team was able to infer global anoxia occurring throughout the ocean using samples from a single outcrop.
The identified
uranium isotope signatures could
in future be used commercially to detect unknown
uranium deposits and help understand processes of
uranium mobility.
A new study of the global cycle of these
uranium isotopes brings additional perspectives to the debate on how Earth has changed over billions of years as revealed
in a recently published study
in the journal Nature.
Uranium isotopes leave a distinct «fingerprint»
in the sources of volcanic rocks, making it possible to gauge their age and origin.
In particular, the researchers found that a higher ratio of uranium - 238 to uranium - 235 is incorporated into the modern oceanic crust, when compared to the uranium isotope signature found in meteorite
In particular, the researchers found that a higher ratio of
uranium - 238 to
uranium - 235 is incorporated into the modern oceanic crust, when compared to the
uranium isotope signature found
in meteorite
in meteorites.
The study by Andersen and his colleagues is the first to use the
uranium isotope ratio for the examination of igneous rock and apply it to the recycling process
in deep Earth.
For this work, conducted at the University of Bristol including Morten Andersen (now Earth Science, ETH Zurich) along with researchers from the Durham (UK), Wyoming and Rhode Island (US), used the «fingerprint» carried
in the ratio of the two
uranium isotopes.
The fuel starts out as a mixture of
uranium isotopes, and the plutonium
isotopes are «bred»
in place.
Using techniques including
uranium - thorium dating
in UQ's Radiogenic
Isotope Laboratory researchers were able to determine when the corals had died with a precision of up to one to two years.
The researchers determined the depositional age of the two stalagmites, collected
in Qal» e Kord Cave
in central northern Iran, using a technique called
uranium - thorium geochronometry conducted
in the UM Rosenstiel School's Neptune
Isotope Lab.
Radioactive dating of the
uranium and lead found
in the minerals (and organic carbon and light
isotope carbon (C13)
in bulk - rock carbonates) within the trace fossils that bacteria etched into the glass around 3.342 + / - 0.068 billion years ago (Jonathan Amos, BBC News, October 12, 2010; Fliegel et al, 2010; Grosch et al, 2009; and Furnes et al, 2004).)
The thorium mined at Baley is likely to have a different set of decay products than the
uranium minerals (which typically contain a mix of
uranium isotopes called «natural
uranium» - or «u-nat» - a mixture of the
isotopes uranium - 235,
uranium - 234 and
uranium - 238 commonly found
in nature) mined at US, German and South Africa sites.
Uranium series is also known as uranium thorium (UT) dating and relies upon various frabctiond of the isotope U230 in the
Uranium series is also known as
uranium thorium (UT) dating and relies upon various frabctiond of the isotope U230 in the
uranium thorium (UT) dating and relies upon various frabctiond of the
isotope U230
in the sample.
«Highly enriched
uranium» (HEU) is made for use
in nuclear weapons and is created when the content of
uranium - 235 (U-235), the
isotope of
uranium that is fissionable and therefore necessary to make nuclear weapons and nuclear reactor fuel, is enriched.
Fast neutrons can unlock the energy
in the dominant
isotope of
uranium (U238) and thus extend known fuel resources by around 200x.
Uranium - series uses the decay of uranium and thorium isotopes (238U, 235U and 232Th) in calcites in particular, such as stalactites and stalagmites in
Uranium - series uses the decay of
uranium and thorium isotopes (238U, 235U and 232Th) in calcites in particular, such as stalactites and stalagmites in
uranium and thorium
isotopes (238U, 235U and 232Th)
in calcites
in particular, such as stalactites and stalagmites
in caves.
Uranium - 235 is the only fissile radioactive
isotope which is a primordial nuclide existing
in the nature
in its present form since before the creation of Earth.
Uranium dating is one of the ways of determining the age of ancient objects, even one million years old, by measuring how much of the following are present in them: the amount of radioactive isotopes of uranium, and the amount of other materials into which the radioactive isotopes would dec
Uranium dating is one of the ways of determining the age of ancient objects, even one million years old, by measuring how much of the following are present
in them: the amount of radioactive
isotopes of
uranium, and the amount of other materials into which the radioactive isotopes would dec
uranium, and the amount of other materials into which the radioactive
isotopes would decompose.
Precisely the situation you outline is present
in all of the world's high - speed centrifuges containing
uranium hexafluoride (UF6) for
isotope separation.
Just to reiterate, this experiment is being conducted, tens of thousands of times every day,
in the gas centrifuges used for
uranium isotope separation, which generate g - forces sufficiently large that the on - axis pressure is a near - vacuum, which the outer - rim pressure is many atomospheres — precisely the conditions of interest.
By comparing the ratio of protactinium - 231 to thorium - 230, two daughter
isotopes of
uranium decay that remain
in seawater for relatively short but consistently different periods of time before drifting into the seafloor, they could determine when circulation was strongest.
Specifically, the team analyzed the variations of the
uranium isotopes found
in these sedimentary deposits.
«Iodine - 129 (129I; half - life 15.7 million years) is a product of cosmic ray spallation on various
isotopes of xenon
in the atmosphere,
in cosmic ray muon interaction with tellurium - 130, and also
uranium and plutonium fission, both
in subsurface rocks and nuclear reactors.
Thorium is better because it has to absorb five neutrons before it will turn into a transuranic
isotope, whereas common
uranium only has to absorb one - a built
in buffer.