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Calcium fluoride is a classic example of a crystal with a fluorite structure. Crystallographic information can be collected via x-ray diffraction, providing information on the locations of electron density within a crystal structure. Using modern software such as Olex2, [4] one can solve a crystal structure from crystallographic output files.
Fluoride is classified as a weak base since it only partially associates in solution, but concentrated fluoride is corrosive and can attack the skin. Fluoride is the simplest fluorine anion. In terms of charge and size, the fluoride ion resembles the hydroxide ion. Fluoride ions occur on Earth in several minerals, particularly fluorite, but are ...
Fluorite and various combinations of fluoride compounds can be made into synthetic crystals which have applications in lasers and special optics for UV and infrared. [38] Exposure tools for the semiconductor industry make use of fluorite optical elements for ultraviolet light at wavelengths of about 157 nanometers. Fluorite has a uniquely high ...
What is fluoride? Fluoride is a natural mineral. It is found in soil, air, food and water sources across the planet, although in different amounts depending on the place, according to the National ...
Fluorine absorption dating is based on the fact that groundwater contains fluoride ions. Items such as bone that are buried in soil will absorb fluoride from the groundwater over time. From the amount of absorbed fluoride in the item, the amount of time that the item has been buried can be estimated.
Phosphate minerals are minerals that contain the tetrahedrally coordinated phosphate (PO 3− 4) anion, sometimes with arsenate (AsO 3− 4) and vanadate (VO 3− 4) substitutions, along with chloride (Cl −), fluoride (F −), and hydroxide (OH −) anions, that also fit into the crystal structure.
A category for compounds with the same crystal structure as calcium fluoride (fluorite), or the structure of magnesium silicide (anti-fluorite). This category is also known by the Strukturbericht designation C1, and falls under the space group Fm 3 m (No. 225).
Fluorine can dissolve into waters as the anion fluoride, where is abundance depends on local abundance within the surrounding rocks. This is in contrast to other halogen abundances, which tend to reflect the abundance of other local halogens, rather than the local rock composition. [ 4 ]