Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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60 soil basics iii<br />
Table 3.2 (Continued)<br />
Family Structure and<br />
Name Composition IUPAC a Name<br />
Ethers Carbon, hydrogen, single<br />
H H H<br />
bonds with at least one<br />
—C—O—C— in the molecule<br />
H C C O C<br />
(may include double and triple<br />
H H H<br />
bonds and other structures) Diethl ether<br />
Aldehydes Carbon, hydrogen, single<br />
H H<br />
bonds with at least one<br />
—CHO in the molecule<br />
(may include double and triple<br />
H C<br />
H<br />
C<br />
H<br />
C<br />
bonds and other structures) Propanal<br />
Ke<strong>to</strong>nes Carbon, hydrogen, single<br />
H O H<br />
bonds with at least one<br />
O<br />
C in in the molecule<br />
H C<br />
H<br />
C C<br />
H<br />
H<br />
(may include double and triple<br />
bonds and other structures)<br />
Propanone (ace<strong>to</strong>ne)<br />
Acids Carbon, hydrogen, single<br />
bonds with at least one<br />
O<br />
C<br />
OH in the molecule<br />
(may include double and triple<br />
bonds and other structures)<br />
H H<br />
O<br />
C C C<br />
H H<br />
OH<br />
Propanoic acid<br />
Amines Carbon, hydrogen, single<br />
bonds with at least one<br />
in the molecule<br />
H<br />
H<br />
C<br />
H<br />
N<br />
(may include double and triple<br />
bonds and other structures);<br />
R groups may be carbon or hydrogen<br />
Methyl amine<br />
H<br />
C N<br />
H<br />
R<br />
R<br />
R<br />
R R<br />
a IUPAC is the International Union of Pure and Applied <strong>Chemistry</strong>, which determines nomenclature<br />
for organic compounds.<br />
Any of these compounds can be found and even synthesized in soil. The<br />
simplest example methane (CH 4), is commonly found in the soil atmosphere.<br />
It is produced during the decomposition of organic matter under anaerobic<br />
conditions, which can occur even in aerobic soils. It is interesting <strong>to</strong> note that<br />
methane can not only be produced in aerobic soils but can also be oxidized<br />
by soil bacteria in the same soil.<br />
H<br />
O<br />
H<br />
H<br />
C<br />
H<br />
H