Vegetation and longitudinal coarse sediment connectivity affect the ability of ecosystem restoration to reduce riverbank erosion and turbidity in drinking water

被引:32
作者
McMahon, Joseph M. [1 ]
Olley, Jon M. [1 ]
Brooks, Andrew P. [2 ]
Smart, James C. R. [1 ]
Stewart-Koster, Ben [1 ]
Venables, William N. [3 ]
Curwen, Graeme [1 ]
Kemp, Justine [1 ]
Stewart, Morag [4 ]
Saxton, Nina [1 ]
Haddadchi, Arman [5 ]
Stout, Justin C. [1 ]
机构
[1] Griffith Univ, Australian Rivers Inst, Nathan, Qld, Australia
[2] Griffith Ctr Coastal Management, Gold Coast, Qld, Australia
[3] CSIRO, Dutton Pk, Qld, Australia
[4] Seqwater, Ipswich, Qld, Australia
[5] Natl Inst Water & Atmospher Res, Christchurch, New Zealand
关键词
Riverbank erosion; Riparian vegetation; Dams; Sediment mining; Subtropics; Light Detection and Ranging (LiDAR); NEW-SOUTH-WALES; RIPARIAN VEGETATION; CONCEPTUAL-FRAMEWORK; SPATIAL VARIABILITY; ALTERNATIVE METHOD; HUMID-TEMPERATE; LOCKYER VALLEY; SE QUEENSLAND; BANK EROSION; MORETON BAY;
D O I
10.1016/j.scitotenv.2019.135904
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
It is a substantial challenge to quantify the benefits which ecosystems provide to water supply at scales large enough to support policy making. This study tested the hypothesis that vegetation could reduce riverbank erosion, and therefore contribute to reducing turbidity and the cost of water supply, during a large magnitude flood along a 62 km riparian corridor where land cover differed substantially from natural conditions. Several lines of evidence were used to establish the benefits that vegetation provided to reducing eleven riverbank erosion processes over 1688 observations. The data and analyses confirmed that vegetation significantly reduced the magnitude of the riverbank erosion process which was the largest contributor to total erosion volume. For this process, a 1% increase in canopy cover of trees higher than five metres reduced erosion magnitude by between 2 and 3%. Results also indicate that riverbank erosion was likely to be affected by direct changes to the riparian corridor which influenced longitudinal coarse sediment connectivity. When comparing the impact of these direct changes on a relative basis, sand and gravel extraction was likely to be the dominant contributor to changed erosion rates. The locations where erosion rates had substantially increased were of limited spatial extent and in general substantial change in river form had not occurred. This suggests that the trajectory of river condition and increasing turbidity are potentially reversible if the drivers of river degradation are addressed through an ecosystem restoration policy. (C) 2019 Elsevier B.V. All rights reserved.
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页数:16
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