Spatial distribution of gully head activity and sediment supply along an ephemeral channel in a Mediterranean environment

Citation
Djo. Wijdenes et al., Spatial distribution of gully head activity and sediment supply along an ephemeral channel in a Mediterranean environment, CATENA, 39(3), 2000, pp. 147-167
Citations number
20
Categorie Soggetti
Environment/Ecology
Journal title
CATENA
ISSN journal
03418162 → ACNP
Volume
39
Issue
3
Year of publication
2000
Pages
147 - 167
Database
ISI
SICI code
0341-8162(200004)39:3<147:SDOGHA>2.0.ZU;2-M
Abstract
In this study, we examined the factors that control the spatial distributio n of bank gully heads along a reach of an ephemeral river (Rambla Salada) i n an area threatened by desertification in Southeast Spain. The activity of 458 gully heads was assessed in the field by pre-defined criteria such as sharp edges, presence of a plunge pool, tension cracks, recent deposited se diments, flow marks, and vegetation re-growth. The results showed that land use has a significant impact on bank gully head activity. Recent land-use changes involving the extension of almond cultivation appears to intensify bank gully head activity. Also, lithology has a clear impact on the bank gu lly extension. It was further investigated whether the gully heads were imp ortant sediment sources that contributed to reservoir sedimentation. The de nsity of (very) active bank gully heads along the study reach was one per 1 7 m of channel length. Average annual retreat volumes were derived from mea surements at 46 active gully heads (4.0 m(3) y(-1)). By selecting all the c hannel sections in the catchment of the Puentes Reservoir with a similar pa ttern of bank gullies using aerial photographs, an estimate of basin-wide s ediment production of bank gully heads was established. It was estimated th at the retreat of active bank gully heads alone in the 12,760 ha study area (representing 12% of the total catchment area of the Puentes Reservoir) pr oduced 6% of the sediment filling up the reservoir. Considering that the se diment is also derived from other sources such as channel walls, channel be ds, and hillslopes, the overall conclusion is that bank gully expansion in Southeast Spain is a major point source of sediment and therefore, a major process of land degradation. (C) 2000 Elsevier Science B.V. All rights rese rved.