 |
| Titel |
Variability of hyporheic exchange in an experimental gravel bed |
| VerfasserIn |
Marcel van der Perk, Ellen L. Petticrew, Philip N. Owens |
| Konferenz |
EGU General Assembly 2011
|
| Medientyp |
Artikel
|
| Sprache |
Englisch
|
| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 13 (2011) |
| Datensatznummer |
250054250
|
|
|
|
|
|
| Zusammenfassung |
| A series of tracer experiments in a large outdoor flume were conducted to examine the
variability of hyporheic exchange in gravel bed sediments. An 18 m long section of a 2 m
wide flume was filled with a 30 cm thick gravel layer with a porosity of 0.39. The gravel of
the 17 cm top layer was well-sorted and had a d50of 37 mm, whereas the deeper layer
consisted of finer gravel with a d50 of 11 mm. The flumes were filled with water, so that a
standing water layer of 20 cm depth over the gravel bed was established. The experiments
included flush-out experiments and instantaneous injection experiments using a salt
tracer at various water discharge rates. During the experiments, the breakthrough
curves of local groundwater was monitored in the water layer and at three gravel
depths (-5 cm, -10 cm, and -20 cm) at four locations downstream of the flume inlet.
In addition, dye tracer experiments were performed to investigate the patterns of
exfiltration relative to the point of infiltration by injecting uranine dye tracer in
a pore at the sediment-water interface. The results of the salt tracer experiments
demonstrate that the time to breakthrough in the water layer and the top 10 cm
layer of the gravel bed is consistent and increases with distance from the flume
inlet and with depth below the sediment-water interface. However, in the deeper
layers of the gravel bed (-10 cm and -20 cm), the time to breakthrough exhibits
considerable variability at short distances with differences up to 30%. This suggests that,
despite that the gravel was relatively homogeneous, the hyporheic exchange rate and
waiting time distribution vary considerably locally depending on local pore space
configurations and accompanying hyporheic flow patterns. The results of the dye
tracer experiments show that the locations of exfiltration were temporally stable and
occurred mostly within 1 m downstream from the point of infiltration. On a few rare
occasions the water exfiltrated within 10 cm upstream from the point of infiltration. |
|
|
|
|
|
|