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 Roy Haggerty and
his students currently work on exchange of water between streams and the
shallow subsurface (the hyporheic zone), on nitrate transport through
sediments below agricultural lands in Oregon, groundwater flow modeling,
and on the physics of solute transport in highly heterogeneous
materials. Students have worked on the role of groundwater in
geologic processes, nuclear waste disposal, mathematical modeling of solute
transport, and stream turbidity. Recent funding for research has come
from the Dept. of Energy, National Science Foundation, Sandia National
Laboratories, and state agencies in Oregon.
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