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Em4885 irrigation management practices to protect ground water

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3 CHAPTER<br />

Nitrogen as a Potential Pollutant<br />

Nitrogen is the most critical of the essential elements for plant growth. The addition of nitrogen<br />

fertilizer <strong>to</strong> enhance crop growth is basic <strong>to</strong> modern irrigated agriculture. The ultimate source of this<br />

nitrogen is the inert gas N which makes up about 78% of the atmosphere. However, except for<br />

2<br />

legumes, plants cannot use nitrogen in this form. Most plants use nitrogen in either the ammonium<br />

+ - - (NH ) form or the nitrate (NO3 ) form. Both occur in solution. However, the nitrate (NO3 ) form is<br />

4<br />

+ much more leachable than the ammonium (NH ) form.<br />

4<br />

Nitrogen is added <strong>to</strong> the soil in a number of ways:<br />

- 1. Lightning may cause the formation of the nitrate (NO ) form which falls <strong>to</strong> earth<br />

3<br />

with rainfall.<br />

2. Legumes such as alfalfa, soybeans, and clover can convert atmospheric N 2 in<strong>to</strong> usable<br />

form through “rhizobia” bacteria. Rhizobia exist in a symbiotic (mutually beneficial)<br />

relationship with the crop. They form and inhabit nodules (abnormal growths) on the<br />

root systems of legumes. This process is termed “symbiotic fixation.”<br />

3. “Non-symbiotic fixation” occurs through some types of blue-green algae and what are<br />

known as “free-living” bacteria. These require no other plants for existence. The amount<br />

of nitrogen fixed by non-symbiotic fixation is relatively small, with estimates in the range<br />

of ten pounds/acre annually.<br />

4. By far, the most important sources of plant-available nitrogen are through addition of<br />

commercial fertilizer and manure.<br />

The disposition of nitrogen that enters the soil is a complex process with many possible avenues<br />

as indicated in Figure 3-1.<br />

AMMONIUM FERTILIZERS<br />

RAINFALL<br />

CROPPED OR GRAZED<br />

+ _<br />

NH + NO<br />

4 AMMONIUM VOLATILIZATION 3<br />

+ _<br />

(NH 4 3 NO in alkaline soils)<br />

MINERALIZATION<br />

LEACHING<br />

(Decomposition of organic<br />

TO IMMOBILIZATION<br />

matter <strong>to</strong> 4 NH )<br />

+<br />

DENITRIFICATION<br />

(Bacterial change of<br />

-<br />

NO 3 <strong>to</strong> 2<br />

N )<br />

IMMOBILIZATION<br />

(Used by microbes)<br />

NITRIFICATION<br />

(Bacterial oxidation<br />

<strong>to</strong> NO ) 3<br />

CLAY COLLOIDS<br />

-<br />

(Some NH 4 fixation)<br />

+<br />

HUMUS<br />

(Organic colloids)<br />

LEACHING<br />

FIGURE 3-1. The nitrogen cycle, showing the different ways that nitrogen enters and leaves the soil.<br />

4<br />

N OF AIR<br />

2<br />

FERTILIZER<br />

NITROGEN FIXATION<br />

(N used by bacteria)<br />

2

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