Characterization of meter-scale spatial variability of riverbed hydraulic conductivity in a lowland river (Aa River, Belgium)
•Riverbed K has been measured in situ by 220 slug tests and 45 standpipe tests.•Riverbed K shows significant meter-scale spatial variability.•A clear directional anisotropy is observed in the riverbed K dataset.•Riverbed structures can be linked to depositional environment and flow regime. An improv...
Saved in:
| Published in: | Journal of hydrology (Amsterdam) Vol. 559; pp. 1013 - 1027 |
|---|---|
| Main Authors: | , , , , , , |
| Format: | Journal Article |
| Language: | English |
| Published: |
Elsevier B.V
01-04-2018
|
| Subjects: | |
| Online Access: | Get full text |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Summary: | •Riverbed K has been measured in situ by 220 slug tests and 45 standpipe tests.•Riverbed K shows significant meter-scale spatial variability.•A clear directional anisotropy is observed in the riverbed K dataset.•Riverbed structures can be linked to depositional environment and flow regime.
An improved general understanding of riverbed heterogeneity is of importance for all groundwater modeling studies that include river-aquifer interaction processes. Riverbed hydraulic conductivity (K) is one of the main factors controlling river-aquifer exchange fluxes. However, the meter-scale spatial variability of riverbed K has not been adequately mapped as of yet. This study aims to fill this void by combining an extensive field measurement campaign focusing on both horizontal and vertical riverbed K with a detailed geostatistical analysis of the meter-scale spatial variability of riverbed K. In total, 220 slug tests and 45 standpipe tests were performed at two test sites along the Belgian Aa River. Omnidirectional and directional variograms (along and across the river) were calculated. Both horizontal and vertical riverbed K vary over several orders of magnitude and show significant meter-scale spatial variation. Horizontal K shows a bimodal distribution. Elongated zones of high horizontal K along the river course are observed at both sections, indicating a link between riverbed structures, depositional environment and flow regime. Vertical K is lognormally distributed and its spatial variability is mainly governed by the presence and thickness of a low permeable organic layer at the top of the riverbed. The absence of this layer in the center of the river leads to high vertical K and is related to scouring of the riverbed by high discharge events. Variograms of both horizontal and vertical K show a clear directional anisotropy with ranges along the river being twice as large as those across the river. |
|---|---|
| ISSN: | 0022-1694 1879-2707 |
| DOI: | 10.1016/j.jhydrol.2018.03.002 |