Vitalism Vitalism was a widespread conception that substances found in organic nature are formed from the chemical elements by the action of a "vital force" or "life-force" (
vis vitalis) that only living organisms possess. In the 1810s,
Jöns Jacob Berzelius argued that a regulative force must exist within living bodies. Berzelius also contended that compounds could be distinguished by whether they required any organisms in their
synthesis (organic compounds) or whether they did not (
inorganic compounds). Vitalism taught that formation of these "organic" compounds were fundamentally different from the "inorganic" compounds that could be obtained from the elements by chemical manipulations in laboratories. Vitalism survived for a short period after the formulation of modern ideas about the
atomic theory and
chemical elements. It first came under question in 1824, when
Friedrich Wöhler synthesized
oxalic acid, a compound known to occur only in living organisms, from
cyanogen. A further experiment was
Wöhler's 1828 synthesis of
urea from the inorganic
salts potassium cyanate and
ammonium sulfate. Urea had long been considered an "organic" compound, as it was known to occur only in the urine of living organisms. Wöhler's experiments were followed by many others, in which increasingly complex "organic" substances were produced from "inorganic" ones without the involvement of any living organism, thus disproving vitalism.
Modern classification and ambiguities molecule, , showing features typical of organic compounds. Carbon atoms are in black, hydrogens gray, oxygens red, and nitrogen blue. Although vitalism has been discredited, scientific nomenclature retains the distinction between
organic and
inorganic compounds. The modern meaning of
organic compound is any compound that contains a significant amount of carbon—even though many of the organic compounds known today have no connection to any substance found in living organisms. The term
carbogenic has been proposed by
E. J. Corey as a modern alternative to
organic, but this neologism remains relatively obscure. As described in detail below, any definition of organic compound that uses simple, broadly-applicable criteria turns out to be unsatisfactory, to varying degrees. The modern, commonly accepted definition of organic compound essentially amounts to any carbon-containing compound, excluding several classes of substances traditionally considered "
inorganic". The list of substances so excluded varies from author to author. Still, it is generally agreed upon that there are (at least) a few carbon-containing compounds that should not be considered organic. For instance, almost all authorities would require the exclusion of
alloys that contain carbon, including
steel (which contains
cementite, ), as well as other metal and semimetal carbides (including "ionic" carbides, e.g., Al4C3| and Calcium carbide| and "covalent" carbides, e.g. Boron carbide| and
SiC, and graphite intercalation compounds, e.g. Graphite intercalation compound|). Other compounds and materials that are considered 'inorganic' by most authorities include: metal
carbonates, simple
oxides of carbon (
CO, Carbon dioxide|, and arguably, carbon suboxide|), the
allotropes of carbon,
cyanide derivatives not containing an organic residue (e.g.,
KCN, Cyanogen|,
BrCN,
cyanate anion , etc.), and heavier analogs thereof (e.g.,
cyaphide anion , Carbon diselenide|,
COS; although
carbon disulfide is often classed as an
organic solvent). Halides of carbon without hydrogen (e.g., Carbon tetrafluoride| and Chlorotrifluoromethane|),
phosgene (),
carboranes,
metal carbonyls (e.g.,
nickel tetracarbonyl),
mellitic anhydride (), and other exotic
oxocarbons are also considered inorganic by some authorities.
Nickel tetracarbonyl () and other metal carbonyls are often volatile liquids, like many organic compounds, yet they contain only carbon bonded to a transition metal and to oxygen, and are often prepared directly from metal and
carbon monoxide. Nickel tetracarbonyl is typically classified as an
organometallic compound as it satisfies the broad definition that
organometallic chemistry covers all compounds that contain at least one carbon to metal covalent bond; it is unknown whether organometallic compounds form a subset of organic compounds. For example, the evidence of covalent Fe-C bonding in
cementite, a major component of steel, places it within this broad definition of organometallic, yet steel and other carbon-containing alloys are seldom regarded as organic compounds. Thus, it is unclear whether the definition of organometallic should be narrowed, whether these considerations imply that organometallic compounds are not necessarily organic, or both. Metal complexes with organic ligands but no carbon-metal bonds (e.g., Copper(II) acetate|) are not considered organometallic; instead, they are called
metal-organic compounds (and might be considered organic). The relatively narrow definition of organic compounds as those containing C–H bonds excludes compounds that are (historically and practically) considered organic. Neither
urea nor
oxalic acid are organic by this definition, yet they were two key compounds in the vitalism debate. However, the
IUPAC Blue Book on organic nomenclature specifically mentions urea and oxalic acid as organic compounds. Other compounds lacking C–H bonds but traditionally considered organic include
benzenehexol,
mesoxalic acid, and
carbon tetrachloride.
Mellitic acid, which contains no C–H bonds, is considered a possible organic compound in
Martian soil. Terrestrially, it, and its anhydride,
mellitic anhydride, are associated with the mineral
mellite (). A slightly broader definition of the organic compound includes all compounds bearing C–H or C–C bonds. This would still exclude urea. Moreover, this definition still leads to somewhat arbitrary divisions in sets of carbon-halogen compounds. For example, tetrafluoromethane| and Carbon tetrachloride| would be considered by this rule to be "inorganic", whereas fluoroform|, Chloroform|, and Hexachloroethane| would be organic, though these compounds share many physical and chemical properties. ==Classification==