Agriculture and urban activities are major sources of phosphorus and n
itrogen to aquatic ecosystems. Atmospheric deposition further contribu
tes as a source of N. These nonpoint inputs of nutrients are difficult
to measure and regulate because they derive from activities dispersed
over wide areas of land and are variable in time due to effects of we
ather. In aquatic ecosystems, these nutrients cause diverse problems s
uch as toxic algal blooms, loss of oxygen, fish kills, loss of biodive
rsity (including species important for commerce and recreation), loss
of aquatic plant beds and coral reefs, and other problems. Nutrient en
richment seriously degrades aquatic ecosystems and impairs the use of
water for drinking, industry, agriculture, recreation, and other purpo
ses. Based on our review of the scientific literature, we are certain
that (1) eutrophication is a widespread problem in rivers, lakes, estu
aries, and coastal oceans, caused by over-enrichment with P and N; (2)
nonpoint pollution, a major source of P and N to surface waters of th
e United States, results primarily from agriculture and urban activity
, including industry; (3) inputs of P and N to agriculture in the form
of fertilizers exceed outputs in produce in the United States and man
y other nations; (4) nutrient flows to aquatic ecosystems are directly
related to animal stocking densities, and under high livestock densit
ies, manure production exceeds the needs of crops to which the manure
is applied; (5) excess fertilization and manure production cause a P s
urplus to accumulate in soil, some of which is transported to aquatic
ecosystems; and (6) excess fertilization and manure production on agri
cultural lands create surplus N, which is mobile in many soils and oft
en leaches to downstream aquatic ecosystems, and which can also volati
lize to the atmosphere, redepositing elsewhere and eventually reaching
aquatic ecosystems. If current practices continue, nonpoint pollution
of surface waters is virtually certain to increase in the future. Suc
h an outcome is not inevitable, however, because a number of technolog
ies, land use practices, and conservation measures are capable of decr
easing the flow of nonpoint P and N into surface waters. From our revi
ew of the available scientific information, we are confident that: (1)
nonpoint pollution of surface waters with P and N could be reduced by
reducing surplus nutrient flows in agricultural systems and processes
, reducing agricultural and urban runoff by diverse methods, and reduc
ing N emissions from fossil fuel burning; and (2) eutrophication can b
e reversed by decreasing input rates of P and N to aquatic ecosystems,
but rates of recovery are highly variable among water bodies. Often,
the eutrophic state is persistent, and recovery is slow.