Chloromethane production: Difference between revisions

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(Created page with "{{Mineral |name=Chert |freq=common |hardness=7 |density=approx. 2.6 |chemf=SiO2 | }} Chert is a naturally occurring mineral composed almost entirely of bonded granules of silicon dioxide. Quartz, Quartzite, Chert, and Flint are all various forms (and granularities) of silicon dioxide. ==See Also==")
 
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{{Mineral
The chloromethane production consumes [[methane]] and [[chlorine]] gas, and produces Compounds of the form CH<sub>x</sub>Cl<sub>y</sub> where x + y = 4.
|name=Chert
 
|freq=common
==Process==
|hardness=7
Generally, [[methane]] and [[chlorine]] gasses are mixed at atmospheric pressure, and catalyzed in some way that the chlorine gas disassociates into a Cl<sup>+</sup> and a Cl<sup>-</sup>. The negative chlorine combines with one of the hydrogens on the methane, producing [[hydrochloric acid]]. The (now slightly negative) methane remnant attracts the positive chlorine ion and bonds with it. This process can occur multiple times, producing variably chlorinated carbon atoms, resulting in [[chloromethane]], [[dichloromethane]], [[trichloromethane]], and [[carbon tetrachloride]].
|density=approx. 2.6
 
|chemf=SiO2
The process can be catalyzed by simple heat (at over 400&deg;C the reaction proceeeds at speed) or via exposure to ultraviolet light, which dissociates the chlorine by photonic cleavage.
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The products are separated by fractional distillation:
Chert is a naturally occurring mineral composed almost entirely of bonded granules of silicon dioxide. [[Quartz]], Quartzite, Chert, and [[Flint]] are all various forms (and granularities) of silicon dioxide.
{{Chloromethane Boiling Points}}
==See Also==
[[Category:Processes]]

Latest revision as of 20:36, 2 December 2024

The chloromethane production consumes methane and chlorine gas, and produces Compounds of the form CHxCly where x + y = 4.

Process

Generally, methane and chlorine gasses are mixed at atmospheric pressure, and catalyzed in some way that the chlorine gas disassociates into a Cl+ and a Cl-. The negative chlorine combines with one of the hydrogens on the methane, producing hydrochloric acid. The (now slightly negative) methane remnant attracts the positive chlorine ion and bonds with it. This process can occur multiple times, producing variably chlorinated carbon atoms, resulting in chloromethane, dichloromethane, trichloromethane, and carbon tetrachloride.

The process can be catalyzed by simple heat (at over 400°C the reaction proceeeds at speed) or via exposure to ultraviolet light, which dissociates the chlorine by photonic cleavage.

The products are separated by fractional distillation:

Chloromethane boiling points
Compound Boiling point (°C)
CH3Cl -23.8
CH2Cl2 39.6
CHCl3 61.15
CCl4 76.72