Heckmann, Tobias ; Haas, Florian ; Abel, Judith ; Rimböck, Andreas ; Becht, Michael:
Feeding the hungry river: Fluvial morphodynamics and the entrainment of artificially inserted sediment at the dammed river Isar, Eastern Alps, Germany.
In: Geomorphology. (2017).
ISSN 0169-555x ; 1872-695X
Link zum Volltext (externe URL): http://dx.doi.org/10.1016/j.geomorph.2017.01.025
Dams interrupt the sediment continuum in rivers by retaining the bedload; combined with flow diversion, bedload retention in tributaries and river engineering measures, this causes a bedload deficit leading to changes in river planform and morphodynamics, with potentially detrimental downstream effects. As part of the SedAlp joint project (Sediment management in Alpine basins: integrating sediment continuum, risk mitigation and hydropower), this study investigates changes within a section of the dammed river Isar between the Sylvenstein reservoir and the city of Bad Tölz.
We use a multi-method approach on a range of spatial and temporal scales. First, we analysed historical maps and aerial photos to analyse river planform and landcover changes within the river corridor of the whole study area on a temporal scale of over 100 years. Results show that major changes occurred before the construction of the Sylvenstein reservoir, suggesting that present morphodynamics represent the reaction to different disturbances on different time scales. Second, changes in mean bed elevation of cross profiles regularly surveyed by the water authorities are analysed in light of artificial sediment insertion and floods; they are also used to estimate the sediment budget of river reaches between consecutive cross profiles. Results suggest stability and a slight tendency towards incision, especially near the Sylvenstein reservoir; further downstream, the sediment balance was positive. Third, we acquired multitemporal aerial photos using an unmanned aerial vehicle and generated high-resolution digital elevation models to show how sediment artificially inserted in the river corridor is entrained. Depending on the position of the artificial deposits in relation to the channel, the deposits are entrained during floods of different return periods.
|Institutionen der Universität:||Mathematisch-Geographische Fakultät > Geographie > Lehrstuhl für Physische Geographie|
|Titel an der KU entstanden:||Ja|
|Eingestellt am:||23. Jan 2017 14:33|
|Letzte Änderung:||23. Jan 2017 14:33|
|URL zu dieser Anzeige:||http://edoc.ku-eichstaett.de/18811/|