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Introduction to Soil Chemistry

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% Transmittance<br />

% Transmittance<br />

120<br />

100<br />

80<br />

60<br />

40<br />

20<br />

infrared spectroscopy 165<br />

0<br />

4000 3500 3000 2500 2000 1500 1000<br />

Wavenumber cm –1<br />

120<br />

100<br />

80<br />

60<br />

40<br />

20<br />

Hexanoic acid<br />

C<br />

O<br />

OH<br />

Octene Octyne 1-Hexanol<br />

H<br />

C OH<br />

H<br />

C C<br />

0<br />

4000 3500 3000 2500 2000 1500 1000<br />

Wavenumber cm –1<br />

Figure 8.11. Infrared spectra showing common absorption. Both the OH of acids and alcohols<br />

are hydrogen-bonded, lending <strong>to</strong> broadening of the absorption. Note that the OH absorption of<br />

hexanol is unusually sharp for a hydrogen-bonded alcohol.<br />

8.11.1. Infrared Sample Preparation<br />

All compounds have absorptions in the midinfrared region of the spectrum.<br />

Most common solvents contain groups that absorb in this region of the spectrum,<br />

which are important for identification of unknowns and thus are not<br />

used. Carbon tetrachloride, carbon disulfide, and mineral oil (often called<br />

nujol) are exceptions, in spite of the fact that all three have significant infrared<br />

absorbences. Mineral oil, for example, has strong absorbences due <strong>to</strong> —CH 3,<br />

—CH2— in its molecules. This obscures regions that may be of analytical<br />

O<br />

C<br />

C C

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