Nitrogen Saturation
Introduction

Sources of N

Biogeochemical effects

Physiological responses

Community responses

Case studies

Future study

References

Links

Nitrogen Cycle

Introduction

Photo of a nitrogen fertilization plot at harvard forest.

The productivity of most temperate forest ecosystems is limited by the availability of nitrogen.  Some regions have seen dramatic increases in rates of nitrogen deposition as a result of human activities.  As nitrogen deposition increases, it may act as a fertilizer to increase the productivity of forests.  However, if the supply of nitrogen continues to increase, a complex series of alterations to soil and plant biogeochemistry may affect productivity, competition, and microbial community structure.  As water and other nutrients become more limiting relative to nitrogen, these ecosystems may approach "nitrogen saturation" (Ågren and Bosatta, 1988; Aber et al., 1989; Aber, 1992; Aber et al., 1998). The nitrogen saturation model hypothesizes that a complex suite of changes occurs as nitrogen deposition increases, ultimately leading to forest decline and soil acidification (figure 1). 
 
 

Figure 1.  Hypothesized response of temperate forest ecosystems to long-term nitrogen additions.  In Stage 1, N-mineralization increases, which results in increased NPP.  In stage 2, NPP and N-mineralization decline due to decreasing Ca:Al and Mg:N ratios, and soil acidification.  Nitrification also increases as excess ammonium is available.  Finally, in Stage 3, nitrate leaching increases dramatically (modified from Aber et al 1998). 
 

As plant-microbial competition for nitrogen decreases, a greater proportion of labile ammonium will be nitrified to nitrate (figure 2-the nitrogen cycle). Greater rates of nitrification may result in an increased flux of nitrogen gas to the atmosphere and in increased leaching of nitrate to ground- and stream-water, which may lead to contaminated drinking water and eutrophication of aquatic ecosystems. 

The effects of nitrogen saturation have been studied using natural gradients in nitrogen deposition (Friedland et al., 1991; McNulty et al., 1991; McNulty et al., 1996) and controlled nitrogen-fertilization experiments (Gundersen, 1991; Magill et al., 1997; Boxman et al., 1998). This overview of nitrogen saturation is divided into the following sections:
 

  • Sources of anthropogenic nitrogen and patterns of deposition
  • Changes in Soil Chemistry and Microbial Processes
  • Plant Physiological Responses to Nitrogen Saturation
  • Community Responses to Nitrogen Saturation
  • Case Studies
  • Need for Further Study
  • Last modified 12/6/99
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