Fine-grained bed sediment storage within the main channel systems of the Frome and Piddle catchments, Dorset, UK

✍ Scribed by A. L. Collins; D. E. Walling

• Publisher: John Wiley and Sons
• Year: 2007
• Tongue: English
• Weight: 265 KB
• Volume: 21
• Category: Article
• ISSN: 0885-6087
• DOI: 10.1002/hyp.6269

✦ Synopsis

Abstract

Lowland permeable catchments in the UK are particularly prone to sedimentation problems, on account of the increased fine sediment loadings generated by recent land‐use change and their stable seasonal hydrological regimes, which are frequently depleted by groundwater abstraction. Fine‐grained sediment storage on the bed of the main channel systems of the Frome (437 km^2^) and Piddle (183 km^2^) catchments, Dorset, UK, has been examined at 29 sites using a sediment remobilization technique. Measurements encompassed the period February 2003–July 2004. At individual sites in the Frome, average values ranged between 410 and 2630 g m^−2^, with an overall mean of 918 g m^−2^. In the Piddle, the average values for individual sites varied between 260 and 4340 g m^−2^, with an overall mean of 1580 g m^−2^. Temporal variations in fine bed sediment storage at each site were appreciable, with the coefficients of variation ranging between 43 and 155% in the Frome and between 33 and 160% in the Piddle. Average reach‐scale specific bed sediment storage increased markedly downstream along each main stem from 2 to 29 t km^−1^ (Frome) and from 4 to 19 t km^−1^ (Piddle). Total fine sediment storage on the channel bed of the Frome varied between 479 t (5 t km^−1^) and 1694 t (17 t km^−1^), with a mean of 795 t (7 t km^−1^), compared with between 371 t (5 t km^−1^) and 1238 t (14 t km^−1^) with a mean of 730 t (9 t km^−1^) in the Piddle. During the study period, fine bed sediment storage was typically equivalent to 18% (Frome) and 57% (Piddle) of the mean annual suspended sediment flux at the study catchment outlets. Copyright © 2006 John Wiley & Sons, Ltd.