Increased inputs of phosphorus (P) in agricultural runoff can accelera
te freshwater eutrophication. This is of particular concern in areas o
f intensive crop and livestock farming, where soil P has increased to
levels that are of environmental rather than agronomic concern. Thus,
many states have been forced to consider the development of recommenda
tions for manure applications based on the potential for P loss in run
off, thereby creating an urgent need to assess the validity of the we
of soil test P as an indicator of P loss in runoff. Several field stud
ies have shown the dissolved P (DP) concentration of runoff is related
to soil test P (r(2) of 0.58-0.98) of surface soil (0 to 5 cm). There
relationships can identify critical levels which can support a DP con
centration of runoff: In this regard critical soil test. P levels esta
blished by several states, ranging from 75 to 200 mg kg(-1), appear to
be realistic However, amounts of P lost in runoff are not related sol
ely to soil test P, due to variable site runoff and erosion potentials
. Thus, an approach which integrates sail test P with estimates of pot
ential runoff and erosion losses and local climatic, topographic, and
agronomic factors is being developed for reliable, yet flexible recomm
endations of fertilizer and manure P management in environmentally sou
nd production agriculture.