uranium ore

Uranium ores were not mentioned; that would come later.

Uranium-236 is produced in uranium ores by neutrons from other radioactives.

It is formed from the oxidation and alteration of primary uranium ores.

In simple terms, uranium ores are found in sandstone deposits.

Its purpose was to produce high purity uranium from uranium ores.

The Subarnarekha passes through areas with extensive mining of copper and uranium ores.

For uranium ores, the leachate may be acid or sodium bicarbonate.

Radon is formed from the decay of radium contained in uranium ores.

Uranium ores from Ontario have occasionally yielded yttrium as a byproduct.

It has yellow crystals and usually mixed with curite in oxidized uranium ores.

They are fossil fuels: coal, oil and natural gas, nuclear fuels: uranium ores.

Before the advent of nuclear reactors, protactinium was separated for scientific experiments from uranium ores.

It is present in uranium ores in concentrations of 100 micrograms per metric ton.

On earth, technetium occurs naturally only in uranium ores as a product of spontaneous fission.

Neptunium is also found in trace amounts in uranium ores due to transmutation reactions.

Only minute traces occur naturally in the Earth's crust as a spontaneous fission product in uranium ores.

It is a breakdown product of uranium, and hence it is found in uranium ores.

As prices go up, production responds from existing mines, and production from newer, harder to develop or lower quality uranium ores begins.

However, trace amounts of the neptunium isotopes neptunium-237 through neptunium-240, are found naturally as decay products from transmutation reactions in uranium ores.

Hydrothermal uranium deposits encompass the vein-type uranium ores.

Because of its geologically short half-life and intense radioactivity, radium compounds are quite rare, occurring almost exclusively in uranium ores.

These included discoveries related to X-radiation and purification of uranium ores, which had been made by Bachelder during the course of the war effort.

The primary source of contamination at the locations stems from the processing of uranium ores and the disposal of the byproducts.

It can be found alongside other very rare selenium-bearing uranium ores, such as haynesite, guilleminite, marthozite and piretite.

In the early years of the SAG Wismut, it simply took over existing plants for processing its uranium ores.