Introduction to Soil Chemistry
Introduction to Soil Chemistry
Introduction to Soil Chemistry
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170 spectroscopy<br />
nitrogen containing material, enriched in 15 N, is applied <strong>to</strong> soil or a crop and<br />
samples taken after various periods of time. The samples are digested using<br />
kjeldahl methods as discussed earlier in Chapter 6, and ammonia is collected<br />
and then decomposed before being injected in<strong>to</strong> the mass spectrometer. A<br />
species enriched in 15 N is a measure of the partitioning of nitrogen and its<br />
movement in the environment. Other stable iso<strong>to</strong>pes can be used in a similar<br />
way <strong>to</strong> follow their movement through the environment in general and in soil<br />
in particular [9,10,31–33].<br />
8.14. CONCLUSION<br />
Matter interacts with all forms of electromagnetic radiation, and these interactions<br />
are used <strong>to</strong> gain information about the matter with which it interacts.<br />
Thus, X-ray, a<strong>to</strong>mic absorption, and many other spectroscopic methods are<br />
available for the investigation of soil. X rays are used <strong>to</strong> determine the structure<br />
of clays and identify the elements present in soil via X-ray fluorescence.<br />
A<strong>to</strong>mic emission, adsorption, and ICP are routinely used <strong>to</strong> determine metals<br />
extracted from soil. Ultraviolet and infrared spectroscopies along with<br />
mass spectrometry are used <strong>to</strong> unequivocally identify compounds. NMR is<br />
extremely powerful in determining the structure and species of various compounds<br />
and species. A common method of analysis is colorimetry, in which the<br />
component of interest is reacted with a reagent, which produces a colored<br />
compound. Using the visible region of the spectrum, the intensity of the color,<br />
as measured by a spectropho<strong>to</strong>meter, is directly related <strong>to</strong> the amount of component<br />
present in the sample using a calibration curve. The results are related<br />
back <strong>to</strong> the original sample.<br />
PROBLEMS<br />
8.1. Describe two ways <strong>to</strong> distinguish between an analytical signal and noise<br />
in the output of an instrument.<br />
8.2. Describe some major limitations of X-ray fluorescence as a method for<br />
determining metals in soil.<br />
8.3. What is spectral overlap, and how may it affect analysis of metals<br />
extracted from soil?<br />
8.4. List three common solvents useful in UV–Vis spectroscopy. Which of<br />
these might be more useful in analysis of soil extracts?<br />
8.5. Describe two ways in which spectra may be used <strong>to</strong> identify compounds.<br />
8.6. Explain how infrared and nuclear magnetic resonance spectra are<br />
different.