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A numerical study of surface‐subsurface exchange processes at a riffle‐pool pair in the Lahn River, Germany
Author(s) -
Saenger Nicole,
Kitanidis Peter K.,
Street Robert L.
Publication year - 2005
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2004wr003875
Subject(s) - riffle , subsurface flow , hydrology (agriculture) , environmental science , infiltration (hvac) , surface water , water quality , residence time (fluid dynamics) , hyporheic zone , hydraulic conductivity , water flow , geology , soil science , groundwater , streams , geotechnical engineering , environmental engineering , soil water , materials science , computer network , ecology , computer science , composite material , biology
Hyporheic exchange is an ecologically important process, controlling the nutrient supply in the upper sediments and thus benthic habitat quality. Hydraulic exchange at a riffle‐pool sequence in the Lahn River, Germany, was analyzed using HEC‐RAS to simulate the surface water flow as a boundary for the subsurface flow and MODFLOW, MODPATH, and MT3DMS to reproduce the transport in the subsurface. Solute transport and residence times of surface water in the subsurface were simulated after calibrating sediment properties to fit simulated hydraulic head to measured subsurface head from the riffle‐pool pair. Three surface water flow rates were considered. Results indicated that exchange increases with increasing surface water flow. However, the hydraulic conductivity of the riverbed sediments influences the mass transfer more than the surface water flow. The ratio of the infiltration rate to the surface water flow is of the same order of magnitude for all the considered flow conditions. Residence times of surface water in the subsurface varied inversely with the flow rates in the river.