Di. Olson et al., CONSTRUCTION AND TESTING OF A FACILITY FOR MEASURING WATER AND AGROCHEMICAL TRANSPORT THROUGH THE VADOSE ZONE, Transactions of the ASAE, 40(4), 1997, pp. 961-969
A large borehole cavity was constructed to study the transport of agri
cultural chemicals through the vadose zone and to the shallow groundwa
ter system. A metal culvert (3.05 m dia and 3.65 m long) was installed
vertically in the excavated cavity to provide a permanent structure.
Stainless steel suction lysimeters were installed radially from the ca
vity wall to collect water samples for chemical analysis from the vado
se zone and the shallow groundwater system at five depths in the soil
profile. A monitoring system consisting of electronic tensiometers and
a data logger were also installed to measure soil water pressure head
at three depths in the vadose zone. A rainfall simulation experiment
was conducted to rest the performance of this large field monitoring s
ystem. Field data on the water and chemical transport through the vado
se zone were collected during and after the rain simulation period. A
rainfall of 127 mm was applied during a 7.5 h period over the area whe
re suction lysimeters were installed at various depths. Chloride was a
pplied with the rain water while bromide was applied to the soil surfa
ce (prior to rainfall) at a rate of 175 kg/ha. Metolachlor and metribu
zin were applied at the experimental site three weeks prior to conduct
ing this rainfall simulation experiment. Increased chloride concentrat
ions were detected at 180 and 240 cm depths within three hours of init
iating rainfall. Bromide was detected at 240 cm depth within three hou
rs of initiating rainfall and increased from 0 to nearly 20 mg L-1 in
about seven hours. Herbicide was detected at 120 cm depth in about an
hour Breakthrough curves for chloride and bromide indicated that prefe
rential flow can cause rapid transport of agricultural chemicals to th
e shallow groundwater system. The results of this rainfall simulation
study indicated that this field monitoring facility works well and has
the potential for future field scale studies on chemical transport to
shallow groundwater systems.