This report presents methodology for excavating one-meter cubic undist
urbed soil monoliths for detailed laboratory investigations of solute
transport through the soil profile. Eight soil monoliths were collecte
d in 1992 from three field areas that had been under consistent tillag
e systems since 1978. The soil was predominantly a Kenyon silt loam (T
ypic Hapludoll) with the water table maintained by subsurface drainage
. Each monolith was instrumented with time-domain reflectometer (TDR)
waveguides, and mini-tensiometers to monitor changes in soil water con
tent and soil matric potential on three sides. A rainfall simulator wa
s constructed to apply water at a rainfall intensity of 33 mm-h(-1) to
a 0.8 m x 0.8 m surface area of the monolith. A conservative tracer (
KBr) was applied to the soil surface and leachate samples were collect
ed from 36 locations at the bottom of each monolith using fiberglass w
ick extractors attached to 810 mm(2) areas in a 6 x 6 grid arrangement
. Water application, soil water content and leachate were monitored to
determine how surface tillage affected preferential flow. Results sug
gest that the soil monolith collection and transportation procedures m
aintained the integrity of the soil profile. Anion tracers provided an
inexpensive means of simulating different nitrogen application method
s. Grid cell samplers using fiberglass wicks allowed analysis of the s
patial variation in leaching losses Leachate samples provided informat
ion about the potential impact of nitrogen application method on leach
ing losses. When coupled with time domain reflectometry and mini-tensi
ometers, electronic data lagging equipment can be used to monitor chan
ges in soil volumetric water content and matric potential.