|
Reactive nitrogen does not cascade
at the same rate through all sectors of the environment. Some systems
(most notably forest and grassland soils) are able to slow down the
continuation of the cascade by accumulating reactive nitrogen and therefore
acting as reservoirs. However, most systems have a finite capacity to
accumulate reactive nitrogen. As a system becomes saturated, more and
more reactive nitrogen moves from these storage reservoirs to systems
downwind or downstream. Table 1 shows those systems that have large
accumulation potential and those from which reactive nitrogen is most
readily transferred. It also shows where reactive nitrogen is likely
to move to, and some potential effects of excess nitrogen within each
system.
Table
1. Characteristics of different systems in relation to the nitrogen
cascade |
|
Accumulation
potential |
Transfer
potential |
Links
to other systems |
Effects
potential |
| Atmosphere |
Low |
Very high |
All but groundwater |
Human and
ecosystem health, climate change |
| Agroecosystems |
Low to moderate |
Very high |
All |
Human and
ecosystem health, climate change |
| Forests |
High |
Moderate,
high in places |
All |
Biodiversity,
net primary productivity, plant mortality, groundwater |
| Grasslands |
High |
Moderate,
high in places |
All |
Biodiversity,
net primary productivity, groundwater |
| Groundwater |
Moderate |
Moderate |
Surface water,
atmosphere |
Human and
ecosystem health, climate change |
| Wetlands,
streams, lakes, rivers |
Low to moderate |
Very high |
Atmosphere,
marine coastal systems |
Biodiversity,
ecological structure, eutrophication, harmful algal blooms |
| Marine
coastal regions |
Low to moderate |
Moderate |
Atmosphere |
Biodiversity,
ecological structure, fish, eutrophication, harmful algal blooms,
hypoxia |
| Source: Galloway and others 2003 |
With more anthropogenic reactive nitrogen
present in the environment, it is likely to be increasingly mobilized
from storage reservoirs, compounding the consequences on people and
ecosystems. However, just as anthropogenic activities have substantially
increased the rate of reactive nitrogen formation, so is it possible
to intervene at critical points along the nitrogen cascade and make
reactive nitrogen less abundant. This can be done in two ways –
decreasing the rate of reactive nitrogen creation during energy and
food production, or converting reactive nitrogen back to N2 after it
has been created and used. |