Suspended sediment load in the tidal zone of an Indonesian river

• Published in: Hydrology and earth system sciences 2012-11, Vol.16 (11), p.4191-4204
• Main Authors: Buschman, F. A, Hoitink, A. J. F, de Jong, S. M, Hoekstra, P, Hidayat, H, Sassi, M. G
• Format: Article
• Language: English
• Subjects: catchment; Coral reefs; east kalimantan; erosion; flux; Freshwater; hbv model; Hydraulic flow; impacts; Marine ecosystems; r-factor; Rivers; Runoff; Sediment transport; soil; Suspended sediment; Timber
• ISSN: 1607-7938; 1027-5606; 1607-7938
• DOI: 10.5194/hess-16-4191-2012

Forest clearing for reasons of timber production, open pit mining and the establishment of oil palm plantations generally results in excessively high sediment loads in tropical rivers. The increasing sediment loads pose a threat to coastal marine ecosystems, such as coral reefs. This study presents observations of suspended sediment loads in the Berau River (Kalimantan, Indonesia), which debouches into a coastal ocean that is a preeminent center of coral diversity. The Berau River is relatively small and drains a mountainous, still relatively pristine basin that receives abundant rainfall. In the tidal zone of the Berau River, flow velocity was measured over a large part of the river width using a horizontal acoustic Doppler current profiler (HADCP). Surrogate measurements of suspended sediment concentration were taken with an optical backscatter sensor (OBS). Averaged over the 6.5 weeks covered by the benchmark survey period, the suspended sediment load was estimated at 2 Mt yr−1. Based on rainfall-runoff modeling though, the river discharge peak during the survey was supposed to be moderate and the yearly averaged suspended sediment load is most likely somewhat higher than 2 Mt yr−1. The consequences of ongoing clearing of rainforest were explored using a plot-scale erosion model. When rainforest, which still covered 50–60% of the basin in 2007, is converted to production land, soil loss is expected to increase with a factor between 10 and 100. If this soil loss is transported seaward as suspended sediment, the increase in suspended sediment load in the Berau River would impose a severe stress on this global hotspot of coral reef diversity.