Microbial transformations of fertilizers and pesticides in the surface
soil have a direct impact on the mass of the agrochemical that is sus
ceptible to leaching losses. Thus, our greatest potential for controll
ing leaching losses of agrochemicals is through the management of thes
e compounds in the surface soil. A variety of strategies have been emp
loyed to maximize the residence time of applied chemical in the surfac
e soil, including: timing of application, formulation (e.g., slow-rele
ase fertilizers and encapsulated pesticides), and the use of compounds
that modify microbial activity in soil (e.g., nitrification inhibitor
s). Although these strategies have met with some success, more precise
quantification of the microbial transformations of agrochemicals is r
equired to aid the development of improved management strategies. The
high spatial variability exhibited by many microbial processes, in man
y cases, precludes precise quantification. A greater understanding of
the factors contributing to the variability of microbial processes all
ows for improved estimation, as well as for the assessment of key driv
ing variables controlling microbial processes in soil. This article re
views several aspects of spatial variability associated with microbial
populations and processes. The discussion focuses on the scale at whi
ch variability is expressed, and the soil and environmental variables
that serve to control variability at each scale. implications for the
development of new management strategies are also discussed, and final
ly, some statistical considerations for characterizing variability are
presented.