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Principles of terrestrial ecosystem ecology.pdf

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214 9. Terrestrial Nutrient Cycling<br />

Solution Losses<br />

Nitrate and dissolved organic nitrogen account<br />

for most <strong>of</strong> the solution loss <strong>of</strong> nitrogen from<br />

<strong>ecosystem</strong>s. Undisturbed <strong>ecosystem</strong>s that<br />

receive low atmospheric inputs generally lose<br />

relatively little nitrogen, and these small losses<br />

occur primarily as dissolved organic nitrogen<br />

(Hedin et al. 1995). Although nitrate is also<br />

highly mobile, plants and microbes absorb most<br />

nitrate before it leaches below the rooting zone<br />

<strong>of</strong> intact <strong>ecosystem</strong>s. Disturbance, however,<br />

<strong>of</strong>ten improves the environment for mineralization<br />

by increasing soil moisture and temperature<br />

and reduces the biomass <strong>of</strong> vegetation<br />

available to absorb nutrients (see Chapter 12).<br />

At the Hubbard Brook Forest in the northeastern<br />

United States, for example, all vegetation<br />

was removed from an experimental<br />

watershed to examine the consequences <strong>of</strong><br />

devegetation.There were large losses <strong>of</strong> nitrate,<br />

calcium, and potassium to the groundwater and<br />

streams when vegetation regrowth was prevented<br />

(Bormann and Likens 1979) (Fig. 9.8).<br />

Nutrient loss (g m -2 )<br />

9<br />

6<br />

3<br />

0<br />

3<br />

2<br />

1<br />

0<br />

60<br />

40<br />

20<br />

0<br />

40<br />

30<br />

20<br />

10<br />

0<br />

60 yr old<br />

forest<br />

Reforestation<br />

prevented<br />

Deforested<br />

Control<br />

Recovery<br />

Calcium<br />

Potassium<br />

Nitrate<br />

Particulate matter<br />

1964 1966 1968 1970 1972 1974 1976<br />

Once vegetation began to regrow, however, the<br />

accumulating plant biomass absorbed most <strong>of</strong><br />

the mineralized nutrients, and stream nutrient<br />

concentrations returned to their preharvest<br />

levels. Additions <strong>of</strong> fertilizer nitrogen or nitrogen<br />

deposition that exceed plant and microbial<br />

nitrogen demands also increase nitrate leaching.<br />

Increased nitrate leaching is one <strong>of</strong> the<br />

characteristics <strong>of</strong> nitrogen saturation, the<br />

changes that occur in <strong>ecosystem</strong> functioning<br />

when anthropogenic nitrogen additions relieve<br />

nitrogen limitation to plants and microbes<br />

(Aber et al. 1998). Anthropogenic nitrogen<br />

inputs are generally correlated with nitrogen<br />

outputs via leaching (Tietema and Beier 1995,<br />

Fenn et al. 1998) (Fig. 9.9).<br />

Nitrate loss to groundwater can have important<br />

consequences for human health and for<br />

the ecological integrity <strong>of</strong> aquatic <strong>ecosystem</strong>s.<br />

Nitrite, which forms from nitrate under reducing<br />

conditions, can reduce the capacity <strong>of</strong><br />

hemoglobin in animals to transport oxygen,<br />

producing anemia, especially in infants.<br />

Groundwater in areas <strong>of</strong> intensive agriculture<br />

Figure 9.8. Losses <strong>of</strong> calcium, potassium,<br />

nitrate, and particulate organic matter in<br />

stream water before and after deforestation<br />

<strong>of</strong> an experimental watershed at Hubbard<br />

Brook Forest in the northeastern United<br />

States. The shaded area shows the time interval<br />

during which vegetation was absent due to<br />

cutting <strong>of</strong> trees and herbicide application.<br />

(Redrawn with permission from Springer-<br />

Verlag; Bormann and Likens 1979.)

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