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Type: | Resource | |
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Created: | Feb 08, 2023 at 2:44 a.m. | |
Last updated: | Feb 08, 2023 at 2:44 a.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 560 |
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Abstract
Ecosystems in river valleys are affected mainly by the hydraulic conditions in wetlands including groundwater dynamics. The quantitative prediction of changes in groundwater dynamics caused by river embankment relocation requires numerical modelling using a physically-based approach. Groundwater recharge from the intermittently flooded river plains was determined by a leakage approach considering soil hydraulic properties. For the study area in the Elbe river valley north of Magdeburg, Germany, a calibrated groundwater flow model was established and the groundwater dynamics for the present situation as well as for the case of embankment relocation were simulated over a 14-year time period. Changes in groundwater depth derived from simulated groundwater levels occurred only during flood periods. By analysing the spatial distributions of changes in statistical parameters, those areas with significant impact on the ecosystems by embankment relocation can be determined.
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Coverage
Spatial
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Additional Metadata
Name | Value |
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DOI | 10.5194/hess-7-67-2003 |
Depth | 40 |
Scale | 11 - 101 km² |
Layers | 1 layer |
Purpose | Decision support |
GroMoPo_ID | 136 |
IsVerified | True |
Model Code | HFLOW_HT |
Model Link | https://doi.org/10.5194/hess-7-67-2003 |
Model Time | 14 |
Model Year | 2003 |
Model Authors | U. Mohrlock |
Model Country | Germany |
Data Available | Report/paper only |
Developer Email | mohrlok@ifh.uka.de |
Dominant Geology | Unconsolidated sediments |
Developer Country | Germany |
Publication Title | Prediction of changes in groundwater dynamics caused by relocation of river embankments |
Original Developer | No |
Additional Information | |
Integration or Coupling | None of the above |
Evaluation or Calibration | Dynamic water levels |
Geologic Data Availability |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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