Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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166 spectroscopy<br />
Table 8.1. Important Diagnostic Absorptions of Major Organic Functionalities in<br />
Mid-Infrared, 1 H NMR, and 13 C Spectra<br />
Functionality Mid-Infrared (cm -1 )<br />
CH3 CH2 H C C H<br />
C C H<br />
C OH<br />
C O<br />
C O<br />
H<br />
C O<br />
OH<br />
C NH<br />
H<br />
1 H ppm<br />
13 C ppm<br />
3000–2900 and 2925–2825 S–N 0–1 S 0–40 S<br />
2950–2850 and 2875–2800 S–N 1–2 S 10–50 S<br />
3100–3000 W–N 5–7 W–N 100–170 S<br />
2250–2100 W–N 2.5–3.1 W–N 60–90 S<br />
3500–3100 B–S 0.5–6.0 S 50–90 S<br />
2700–2900 (H) W–N 9–10 W 190–220 S<br />
1650–1750 (C=O) S–N<br />
1650–1750 (C=O) S–N NA* 190–220 S<br />
3300–2900 (—OH) B–N 10–13 W 160–185 S<br />
1675–1775 (C=O) S–N<br />
3500–3200 W–N 1.0–5.0 W–N 35–50 S<br />
3100–3000 W–N 6.5–8.5 S–N–SS 100–170 S<br />
* NA not applicable, S strong, N narrow, B broad, W weak, SS split.<br />
importance (see discussion of petroleum hydrocarbon analysis above). Neither<br />
carbon tetrachloride nor carbon disulfide is used <strong>to</strong>day because of <strong>to</strong>xicity,<br />
difficulty in handling, and detrimental environmental effects.<br />
Methods are available <strong>to</strong> remove the interferences due <strong>to</strong> solvents, such as<br />
subtraction and compensation. These may be accomplished manually or electronically<br />
depending on the instrumentation and how they are configured.<br />
However, the preference is always <strong>to</strong> obtain a spectrum without the interference<br />
of a solvent!<br />
Perhaps the most widely and commonly used method for liquid sampling,<br />
used with FT-IR spectropho<strong>to</strong>meters, is attenuated <strong>to</strong>tal reflection, the cell for<br />
which is shown in B in Figure 8.7. A liquid sample is placed in the trough, the<br />
bot<strong>to</strong>m of which is a crystal situated such that the incident IR beam is <strong>to</strong>tally<br />
reflected inside the crystal and exits in<strong>to</strong> the instrument. When reflected, the<br />
beam appears <strong>to</strong> slightly pass in<strong>to</strong> the sample in contact with the crystal, allowing<br />
the sample <strong>to</strong> absorb energy, producing a spectrum. Another common<br />
method is <strong>to</strong> place the pure liquid between two salt windows. A drop may be<br />
placed between two salt windows or in a sealed cell, where the space between<br />
the windows is predetermined and held constant. These types of cells can be<br />
used where quantitation of the component is desired or where a volatile<br />
solvent or solution of a compound is being analyzed.<br />
Solid samples or solid extracts can be mixed and ground with potassium<br />
bromide (KBr), pressed <strong>to</strong> form a transparent pellet and a spectrum obtained