Department of Ocean Sciences, Inha University, Incheon 22212, Republic of Korea.
Department of Ocean Sciences, Inha University, Incheon 22212, Republic of Korea.
Sci Total Environ. 2021 Apr 20;766:144493. doi: 10.1016/j.scitotenv.2020.144493. Epub 2020 Dec 26.
In-situ erodibility experiments were conducted to reveal the effects of vegetation on sediment stability in an intertidal flat. Spartina alterniflora (Spartina), one of the most widespread types of vegetation, led to complexity in sediment erodibility. The long stems and leaves of Spartina, which grew to approximately 156 cm from May to November 2019, were effective in trapping suspended sediments in the water columns, eventually promoting the deposition of approximately 2.3 cm within its communities. Sediments eroded by increasing bed shear stress (τ) mainly originated from sediments that were adhered to the stems and leaves of Spartina (May: 76%; November: 54%). They protected subsequent bed erosion against τ. However, this was only an apparent effect because the Spartina caused the erosion rate (E) to stagnate by suppressing the outflow of eroded mass from the bed. As the protective effect of the stems was removed, the uppermost sediment layers in the Spartina communities became more vulnerable to erosion by τ, with the initial erosion thresholds lowered to 0.1 Pa (May) and 0.05 Pa (November). Despite continuous sedimentation by sediment trapping, the sediment bed in Spartina communities had not been consolidated under repeated tidal inundation, showing no distinct development of the critical shear stress for erosion. Thus, the differences in E between cases with or without Spartina's stems reached approximately 1.22 × 10 (May) and 1.83 × 10 kg m s (November) at τ = 0.6 Pa. Results suggest that the increase in thickness of erodible layers mainly contributed more than sediment volume fraction to the enhancement of erosion potential with τ. This study highlights the necessity to assess both positive and negative effects of Spartina on the stability of sediment beds in intertidal flats.
进行了原地侵蚀实验,以揭示植被对潮滩沉积物稳定性的影响。盐地碱蓬(Spartina)是分布最广泛的植被类型之一,它使沉积物的可侵蚀性变得复杂。盐地碱蓬的长茎和叶在 2019 年 5 月至 11 月期间长到约 156 厘米,有效地捕获了水柱中的悬浮泥沙,最终促进了其群落内约 2.3 厘米的沉积。由于床面剪切应力(τ)增加而侵蚀的泥沙主要来源于附着在盐地碱蓬茎和叶上的泥沙(5 月:76%;11 月:54%)。它们保护了随后的床面侵蚀免受 τ 的影响。然而,这只是一种表面效应,因为盐地碱蓬通过抑制泥沙从床面流出,使侵蚀率(E)停滞不前。随着茎的保护作用的消除,盐地碱蓬群落中最上层的泥沙层更容易受到 τ 的侵蚀,初始侵蚀阈值降低到 0.1 Pa(5 月)和 0.05 Pa(11 月)。尽管由于泥沙捕获而持续沉积,但在潮汐反复淹没下,盐地碱蓬群落中的泥沙床并没有得到固结,没有明显发展出侵蚀的临界剪切应力。因此,有盐地碱蓬茎和没有盐地碱蓬茎的情况下 E 的差异在 τ=0.6 Pa 时分别约为 1.22×10(5 月)和 1.83×10kgm s(11 月)。结果表明,在 τ 增加的情况下,可侵蚀层厚度的增加对增强侵蚀潜力的贡献大于泥沙体积分数。本研究强调了在评估潮汐滩涂中盐地碱蓬对泥沙床稳定性的影响时,需要同时考虑积极和消极两方面的影响。