, CH
4; is among the simplest organic compounds.]]
In
chemistry, organic compounds are generally any
chemical compounds that contain
carbon-
hydrogen bonds. Due to carbon's ability to
catenate (form chains with other carbon atoms), millions of organic compounds are known. The study of the properties, reactions, and syntheses of organic compounds comprises the discipline known as
organic chemistry. For historical reasons, a few classes of carbon-containing compounds (e.g.,
carbonate anion salts and
cyanide salts), along with a handful of other exceptions (e.g., carbon dioxide), are not classified as organic compounds and are considered inorganic. Other than those just named, little consensus exists among
chemists on precisely which carbon-containing compounds are excluded, making any rigorous definition of an organic compound elusive.
[Spencer L. Seager, Michael R. Slabaugh. ''Chemistry for Today: general, organic, and biochemistry''. Thomson Brooks/Cole, 2004, p. 342. ]
Although organic compounds make up only a small percentage of the Earth's crust, they are of central importance because all known life is based on organic compounds. Living things incorporate inorganic carbon compounds into organic compounds through a network of processes (
the carbon cycle) that begins with the conversion of
carbon dioxide and a hydrogen source like water into simple sugars and other organic molecules by
autotrophic organisms using light (
photosynthesis) or other sources of energy. Most synthetically produced organic compounds are ultimately derived from
petrochemicals consisting mainly of
hydrocarbons, which are themselves formed from the high pressure and temperature degradation of organic matter underground over geological timescales. This ultimate derivation notwithstanding, organic compounds are no longer defined as compounds originating in living things, as they were historically.
In chemical nomenclature, an
organyl group, frequently represented by the letter R, refers to any monovalent
substituent whose open valence is on a carbon atom.
Definitions of organic vs inorganic
For historical reasons discussed below, a few types of carbon-containing compounds, such as
carbides,
carbonates (excluding
carbonate esters), simple
oxides of carbon (for example, CO and CO
2), and
cyanides are considered
inorganic. Different forms (
allotropes) of pure carbon, such as
diamond,
graphite,
fullerenes, and
carbon nanotubes are also excluded because they are simple substances composed of only a single element and therefore are not generally considered to be chemical ''compounds''.
History
Vitalism
Vitalism was a widespread conception that substances found in organic nature are created from the chemical elements by the action of a "vital force" or "life-force" (''vis vitalis'') that only living organisms possess. Vitalism taught that these "organic" compounds were fundamentally different from the "inorganic" compounds that could be obtained from the elements by chemical manipulations.
Vitalism survived for a while even after the rise 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.
Modern classification and ambiguities
thumb|upright=0.8|The [[isoleucine|L-isoleucine molecule, C
6H
13NO
2, 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.
The organic compound
L-isoleucine molecule presents some features typical of organic compounds:
carbon–carbon bonds,
carbon–hydrogen bonds, as well as covalent bonds from carbon to oxygen and to nitrogen.
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 as 'inorganic'. However, 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, Fe
3C), as well as other metal and semimetal carbides (including "ionic" carbides, e.g,
Al4C3 and
CaC2 and "covalent" carbides, e.g.
B4C and
SiC, and graphite intercalation compounds, e.g.
KC8). Other compounds and materials that are considered 'inorganic' by most authorities include: metal
carbonates, simple
oxides (CO, CO
2, and arguably, C
3O
2), the
allotropes of carbon,
cyanide derivatives not containing an organic residue (e.g., KCN, (CN)
2, BrCN, CNO
−, etc.), and heavier analogs thereof (e.g., CP
− '
cyaphide anion', CSe
2, COS; although CS
2 '
carbon disulfide' is often classed as an ''organic'' solvent). Halides of carbon without hydrogen (e.g., CF
4 and CClF
3),
phosgene (COCl
2),
carboranes,
metal carbonyls (e.g., nickel carbonyl),
mellitic anhydride (C
12O
9), and other exotic
oxocarbons are also considered inorganic by some authorities.
Nickel carbonyl (Ni(CO)
4) and other metal carbonyls present an interesting case. They 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 carbonyl is frequently considered to be ''organometallic''. Although many organometallic chemists employ a broad definition, in which any compound containing a carbon-metal covalent bond is considered
organometallic, it is debatable whether organometallic compounds form a subset of organic compounds.
Metal complexes with organic ligands but no carbon-metal bonds (e.g., Cu(OAc)
2) are not considered organometallic; instead they are classed as ''metalorganic''. Likewise, it is also unclear whether metalorganic compounds should automatically 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 is organic by this definition, yet they were two key compounds in the vitalism debate. The
IUPAC Blue Book on organic nomenclature specifically mentions urea and oxalic acid. 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 substance in
Martian soil. Terrestrially, it, and its anhydride, mellitic anhydride, are associated with the mineral
mellite (Al
2C
6(COO)
6·16H
2O).
A slightly broader definition of 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,
CF4 and
CCl4 would be considered by this rule to be "inorganic", whereas
CF3H,
CHCl3, and
C2Cl6 would be organic, though these compounds share many physical and chemical properties.
Classification
Organic compounds may be classified in a variety of ways. One major distinction is between natural and synthetic compounds. Organic compounds can also be classified or subdivided by the presence of
heteroatoms, e.g.,
organometallic compounds, which feature bonds between carbon and a
metal, and
organophosphorus compounds, which feature bonds between carbon and a
phosphorus.
Another distinction, based on the size of organic compounds, distinguishes between
small molecules and
polymers.
Natural compounds
Natural compounds refer to those that are produced by plants or animals. Many of these are still extracted from natural sources because they would be more expensive to produce artificially. Examples include most
sugars, some
alkaloids and
terpenoids, certain nutrients such as
vitamin B12, and, in general, those natural products with large or
stereoisometrically complicated molecules present in reasonable concentrations in living organisms.
Further compounds of prime importance in
biochemistry are
antigens,
carbohydrates,
enzymes,
hormones,
lipids and
fatty acids,
neurotransmitters,
nucleic acids,
proteins,
peptides and
amino acids,
lectins,
vitamins, and
fats and oils.
Synthetic compounds
Compounds that are prepared by reaction of other compounds are known as "synthetic". They may be either compounds that already are found in plants or animals or those that do not occur naturally.
Most
polymers (a category that includes all
plastics and
rubbers) are organic synthetic or semi-synthetic compounds.
Biotechnology
Many organic compounds—two examples are
ethanol and
insulin—are manufactured industrially using organisms such as bacteria and yeast. Typically, the
DNA of an organism is altered to express compounds not ordinarily produced by the organism. Many such
biotechnology-engineered compounds did not previously exist in nature.
Databases
* The ''
CAS'' database is the most comprehensive repository for data on organic compounds. The search tool ''
SciFinder'' is offered.
* The ''
Beilstein database'' contains information on 9.8 million substances, covers the scientific literature from 1771 to the present, and is today accessible via
Reaxys. Structures and a large diversity of physical and chemical properties is available for each substance, with reference to original literature.
* ''
PubChem'' contains 18.4 million entries on compounds and especially covers the field of
medicinal chemistry.
A great number of more specialized databases exist for diverse branches of organic chemistry.
Structure determination
The main tools are
proton and
carbon-13 NMR spectroscopy,
IR Spectroscopy,
Mass spectrometry,
UV/Vis Spectroscopy and
X-ray crystallography.
[Ernö Pretsch, Philippe Bühlmann, Martin Badertscher (2009), ''Structure Determination of Organic Compounds'' (Fourth, Revised and Enlarged Edition). Springer-Verlag Berlin Heidelberg]
See also
*
Inorganic compounds
*
List of chemical compounds
*
List of organic compounds
*
Organometallic compounds
References
External links
Organic Compounds Database
{{DEFAULTSORT:Organic Compound
Category:Organic chemistry