TY - JOUR
T1 - Effects of riverbank restoration on the removal of dissolved organic carbon by soil passage during floods - A scenario analysis
AU - Derx, J.
AU - Farnleitner, A. H.
AU - Blöschl, G.
AU - Vierheilig, J.
AU - Blaschke, A. P.
N1 - Funding Information:
This paper was supported by the Austrian Science Fund (FWF) as part of the DKplus (Vienna Doctoral Program on Water Resource Systems, project number W1219-N22) and the GWRS-Vienna in cooperation with Vienna Water as part of the “(New)Danube – Untere Lobau Network Project” (Gewässervernetzung (Neue) Donau – Untere Lobau (Nationalpark Donau-Auen) funded by the Government of Austria (Federal Ministry of Agriculture, Forestry, Environment & Water Management), the Government of Vienna, and the European Agricultural Fund for Rural Development (project LE 07-13). This is a joint investigation of the Interuniversity Cooperation Centre for Water & Health ( www.waterandhealth.at ).
PY - 2014/5/6
Y1 - 2014/5/6
N2 - River restoration typically aims at improving and preserving the ecological integrity of rivers and their floodplains. Restoration projects may, however, decrease the ability of the riparian zone to remove contaminants as the river water moves into the aquifer, especially during high river discharges. The purpose of this paper is to analyze several factors involved during riverbank restoration (i.e. changes in riverbank topography and hydraulic conductivity of the upper sediments of the riverbank), with respect to their effect on enhancing dissolved organic carbon (DOC) transport from rivers into the groundwater. 3-D groundwater flow and transport with first-order decay was simulated for a typical setting of a porous groundwater aquifer near a large river. The simulations indicate that, during a 5. m flooding event, DOC concentrations in the groundwater can be 1.7-9 times higher at a restored riverbank (i.e. 250. m wide, no clogging within one meter of riverbank sediments) compared to a steep riverbank (i.e. 8. m wide, clogging within 1. m of sediments), in coarse to fine sandy gravel. 51-84% of this increase in DOC concentration levels in the groundwater were due to an increase in submerged area of the riverbank, depending on the type of soil of the aquifer. The remaining part was caused by a change in riverbank hydraulic conductivity. The simulations further showed that the arrival times of DOC concentration peaks at 400-500. m distance from the river axis can be 18-27. days shorter at restored than at steep riverbanks. 77-100% of the earlier arrival times of DOC concentration peaks at 400-500. m from the river axis were due to an increase in submerged area of the riverbank. The remaining part was due to a change in riverbank hydraulic conductivity. The effects of riverbank restoration on DOC concentrations and arrival times were bigger if river DOC concentrations increased than if they were assumed constant during the flood, the more the river water level increased and the closer the distance was to the river. The findings suggest that riverbank restoration projects as conducted as part of the implementation of the European Water Framework Directive, potentially, may have adverse effects on the groundwater quality near rivers. Additional monitoring strategies will therefore be needed in the future in such projects to protect alluvial ground water resources for public drinking water supply.
AB - River restoration typically aims at improving and preserving the ecological integrity of rivers and their floodplains. Restoration projects may, however, decrease the ability of the riparian zone to remove contaminants as the river water moves into the aquifer, especially during high river discharges. The purpose of this paper is to analyze several factors involved during riverbank restoration (i.e. changes in riverbank topography and hydraulic conductivity of the upper sediments of the riverbank), with respect to their effect on enhancing dissolved organic carbon (DOC) transport from rivers into the groundwater. 3-D groundwater flow and transport with first-order decay was simulated for a typical setting of a porous groundwater aquifer near a large river. The simulations indicate that, during a 5. m flooding event, DOC concentrations in the groundwater can be 1.7-9 times higher at a restored riverbank (i.e. 250. m wide, no clogging within one meter of riverbank sediments) compared to a steep riverbank (i.e. 8. m wide, clogging within 1. m of sediments), in coarse to fine sandy gravel. 51-84% of this increase in DOC concentration levels in the groundwater were due to an increase in submerged area of the riverbank, depending on the type of soil of the aquifer. The remaining part was caused by a change in riverbank hydraulic conductivity. The simulations further showed that the arrival times of DOC concentration peaks at 400-500. m distance from the river axis can be 18-27. days shorter at restored than at steep riverbanks. 77-100% of the earlier arrival times of DOC concentration peaks at 400-500. m from the river axis were due to an increase in submerged area of the riverbank. The remaining part was due to a change in riverbank hydraulic conductivity. The effects of riverbank restoration on DOC concentrations and arrival times were bigger if river DOC concentrations increased than if they were assumed constant during the flood, the more the river water level increased and the closer the distance was to the river. The findings suggest that riverbank restoration projects as conducted as part of the implementation of the European Water Framework Directive, potentially, may have adverse effects on the groundwater quality near rivers. Additional monitoring strategies will therefore be needed in the future in such projects to protect alluvial ground water resources for public drinking water supply.
KW - DOC transport
KW - Ecological integrity
KW - Riverbank filtration
KW - Water supply
UR - http://www.scopus.com/inward/record.url?scp=84896541477&partnerID=8YFLogxK
U2 - 10.1016/j.jhydrol.2014.02.061
DO - 10.1016/j.jhydrol.2014.02.061
M3 - Journal article
AN - SCOPUS:84896541477
SN - 0022-1694
VL - 512
SP - 195
EP - 205
JO - Journal of Hydrology
JF - Journal of Hydrology
ER -