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Introduction to Soil Chemistry

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ioorganic 57<br />

activity may be increased, decreased, unchanged, or completely destroyed<br />

[15,16].<br />

All biomolecules tend <strong>to</strong> be large polymer or polymerlike combinations of<br />

individual molecular units that can be isolated by either acidic or basic hydrolysis.<br />

Lipids and fats are found as integral parts of membranes and cell walls.<br />

Polysaccharides are used as structural units and as s<strong>to</strong>red energy sources. Proteins<br />

are used <strong>to</strong> construct muscle and enzymes that also contain metals such<br />

as zinc, manganese, and iron. There are many other important biomolecules<br />

present at lower concentrations, such as DNA and RNA, which are also<br />

released in<strong>to</strong> the soil solution. All can be the source of smaller molecules in<br />

the soil solution.<br />

The different groups of biomolecules, lipids, polysaccharides, and proteins,<br />

illustrated in Figure 3.9, decompose at different rates depending on their composition.<br />

Lipids and fats are slower <strong>to</strong> decompose in soil because of their insolubility<br />

in water. Large polysaccharides are also insoluble in water but are more<br />

quickly decomposed than are fats. Proteins and compounds such as DNA and<br />

RNA are more quickly decomposed in part because they contain nitrogen<br />

(fixed), which is often in short supply in the environment.<br />

Biochemicals will be present in soil during any analysis and can react with<br />

components of interest, either organic or inorganic, including sand, silt, and<br />

clay particles. Possible reactions include chelation, decomposition, precipitation,<br />

solubilization, or dissolving such as dissolving in soil organic matter<br />

(humus). Several of these reactions will take place simultaneously and can lead<br />

<strong>to</strong> nondetection of the component of interest or an analytical result that is<br />

much lower than the true value [15].<br />

3.5. BIOORGANIC<br />

Bioorganic components in soil include those organic molecules that participate<br />

in biochemical reactions; are responsible for the initiation of a reaction,<br />

eliciting the formation of a compound or an antibiotic; or are inhibi<strong>to</strong>rs. Bioorganic<br />

chemistry also uses synthesized models and molecules, <strong>to</strong> study biological<br />

processes such as enzymatic activity. Often these studies are<br />

undertaken <strong>to</strong> develop a mechanism for the reactions of interest. Bioorganic<br />

molecules will be present either as components of the synthesis chain or as<br />

part of the degradation products. Whenever cells lyse, these compounds will<br />

be released in<strong>to</strong> the soil solution. Their moderate size and complexity will<br />

allow them <strong>to</strong> be metabolized rapidly.<br />

Because of their moderate size and complexity, bioorganic molecules can be<br />

confused with analytes of interest. They can have the same or similar retentions<br />

times, during chroma<strong>to</strong>graphic procedures, as the analytes of interest and<br />

thus can indicate the presence of more molecules than are actually the case or<br />

even the presence of an analyte or contaminant when it is not or has not been<br />

added from an external source. It is also possible for gas chroma<strong>to</strong>graphic/mass

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