![]() ![]() ![]() Abiotic processes are also believed to contribute to natural chloroform productions in soils, although the mechanism is still unclear. Many kinds of seaweed produce chloroform, and fungi are believed to produce chloroform in soil. The total global flux of chloroform through the environment is approximately 660 000 tonnes per year, and about 90% of emissions are natural in origin. The chloroform molecule can be viewed as a methane molecule with three hydrogen atoms replaced with three chlorine atoms, leaving a single hydrogen atom. The molecule adopts a tetrahedral molecular geometry with C 3v symmetry. Chloroform was frequently used as an anaesthetic between 1847 and the first half of the 20th century. Ĭhloroform is miscible with many solvents but it is only very slightly soluble in water (only 8 g/L at 20 ☌). It is also part of a wider class of substances known as volatile organic compounds. It is a very volatile, colorless, strong-smelling, dense liquid produced on a large scale as a precursor to PTFE and refrigerants and is a trihalomethane that serves as a powerful anesthetic, euphoriant, anxiolytic, and sedative when inhaled or ingested. Chloroform, or trichloromethane, is an organic compound with the formula C H Cl 3 and a common organic solvent. ![]()
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |