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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

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