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dichlorine trioxide, Cl 2 O 3 as possible isomer Cl−O−ClO 2, chlorine (I,V) oxide; dichlorine trioxide, Cl 2 O 3 as hypothetical isomer O−Cl−O−Cl−O, chlorine (III) oxide; dichlorine tetroxide, also known as chlorine perchlorate, Cl 2 O 4 or ClOClO 3, chlorine (I,VII) oxide; dichlorine pentoxide, Cl 2 O 5 or ClOOClO 3, is ...
In chemistry, hypochlorite, or chloroxide is an anion with the chemical formula ClO −. It combines with a number of cations to form hypochlorite salts. Common examples include sodium hypochlorite (household bleach) and calcium hypochlorite (a component of bleaching powder, swimming pool "chlorine"). [1] The Cl-O distance in ClO − is 1.69 Å ...
Ethylene [2] 4.612 0.0582 Fluorine [2] 1.171 0.0290 Fluorobenzene: 20.19 0.1286 Fluoromethane: 4.692 0.05264 Freon: 10.78 0.0998 Furan [2] 12.74 0.0926 Germanium tetrachloride: 22.90 0.1485 Helium: 0.0346 0.0238 Heptane [2] 31.06 0.2049 1-Heptanol [2] 38.17 0.2150 Hexane: 24.71 0.1735 1-Hexanol [2] 31.79 0.1856 Hydrazine [2] 8.46 0.0462 ...
Chlorine monoxide is a chemical radical with the chemical formula ClO •. It plays an important role in the process of ozone depletion. In the stratosphere, chlorine atoms react with ozone molecules to form chlorine monoxide and oxygen. Cl • + O 3 → ClO • + O 2. This reaction causes the depletion of the ozone layer. [1]
The earliest method of synthesis was to treat mercury(II) oxide with chlorine gas. [3] However, this method is expensive, as well as highly dangerous due to the risk of mercury poisoning. 2 Cl 2 + HgO → HgCl 2 + Cl 2 O. A safer and more convenient method of production is the reaction of chlorine gas with hydrated sodium carbonate at 20–30 ...
In chemistry, oxychlorination is a process for generating the equivalent of chlorine gas (Cl 2) from hydrogen chloride and oxygen. [1] This process is attractive industrially because hydrogen chloride is less expensive than chlorine. [2]
Oxygen is present as compounds in the atmosphere in trace quantities in the form of carbon dioxide (CO 2) and oxides of nitrogen (NO x). The Earth's crustal rock is composed in large part of oxides of silicon (silica SiO 2, found in granite and sand), aluminium (aluminium oxide Al 2 O 3, in bauxite and corundum), iron (iron (III) oxide Fe 2 O
However, in liquid or solid form, this chlorine oxide ionizes into the dark red ionic compound chloryl perchlorate [ClO 2] + [ClO 4] −, which may be thought of as the mixed anhydride of chloric and perchloric acids. This compound is a notable perchlorating agent. [1] It is produced by reaction between chlorine dioxide and excess ozone: 2 ClO ...