Channel and vegetation recovery from dredging of a large river in the Gulf coastal plain, USA

被引:17
作者
Mossa, Joann [1 ]
Chen, Yin-Hsuen [1 ]
Kondolf, G. Mathias [2 ]
Walls, Scott Porter [3 ]
机构
[1] Univ Florida, Dept Geog, POB 117315,3141 Turlington Hall, Gainesville, FL 32611 USA
[2] Univ Calif Berkeley, Dept Landscape Architecture & Environm Planning, Berkeley, CA 94720 USA
[3] Walls Land Water LLC, Watershed Sci, 320 Alamo Ave, Santa Cruz, CA 95060 USA
关键词
biogeomorphology; fluvial geomorphology; vegetative recovery; dredging impacts; passive restoration; floodplains; RIPARIAN VEGETATION; APALACHICOLA RIVER; PRIMARY SUCCESSION; DYNAMICS; RESTORATION; WILLOW; ADJUSTMENTS; FEEDBACKS; GROWTH; SALICACEAE;
D O I
10.1002/esp.4856
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Anthropogenic impacts in large rivers are widely studied, but studies of recovery once a disturbance has stopped are uncommon. This study examines the biogeomorphic recovery of a 40-km river corridor on the mid-Apalachicola River, Florida following the cessation of dredging, disposal, and snag removal in 2002. This failed navigation project resulted in vegetation losses (166 ha between 1941 and 2004), river widening, and increased point bar areas. We used paired sets of imagery for a 10-year period during the recovery process at two different flow levels to assess sand bar change, land cover change, and their spatial variations. Most large sand bars decreased significantly in area due to growth of pioneer species, typically from the bankside of the bar. Mean bar area shrank 0.17 and 0.20 ha for the 30th and 1st percentile flows, respectively. For the entire study area, both water-level comparisons showed gains in vegetation (23.36 and 15.83 ha), compensated by losses in the extent of water (16.83 and 8.55 ha) and sand bar losses (6.53 and 7.28 ha). Overall, these gains during the 10-year passive recovery period are equivalent to 15% of the vegetation losses that resulted from the navigational dredging. As found in other studies, most of the pioneer vegetation grew approximately 2 m relative elevation above the low-water surface. The initial length of the tree line and the area of herbaceous growth both had a significant and positive relationship with the area of new vegetation growth over the study interval. As parts of the river are healing, reduced channel capacity from narrowing and tree growth will benefit the floodplain. As elsewhere, understanding of a river's biogeomorphology, hydrology, and disturbance history can help in selecting appropriate recovery metrics to further advance the understanding and management of disturbed floodplains. (c) 2020 John Wiley & Sons, Ltd.
引用
收藏
页码:1926 / 1944
页数:19
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