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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