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Sediment structure and physicochemical changes following tidal inundation at a large open coast managed realignment site

机译:大型开阔海岸调整区的潮汐淹没后沉积物结构和理化变化

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摘要

Managed realignment (MR) schemes are being implemented to compensate for the loss of intertidal saltmarsh habitats by breaching flood defences and inundating the formerly defended coastal hinterland. However, studies have shown that MR sites have lower biodiversity than anticipated, which has been linked with anoxia and poor drainage resulting from compaction and the collapse of sediment pore space caused by the site's former terrestrial land use. Despite this proposed link between biodiversity and soil structure, the evolution of the sediment sub-surface following site inundation has rarely been examined, particularly over the early stages of the terrestrial to marine or estuarine transition. This paper presents a novel combination of broad- and intensive-scale analysis of the sub-surface evolution of the Medmerry Managed Realignment Site (West Sussex, UK) in the three years following site inundation. Repeated broad-scale sediment physiochemical datasets are analysed to assess the early changes in the sediment subsurface and the preservation of the former terrestrial surface, comparing four locations of different former land uses. Additionally, for two of these locations, high-intensity 3D-computed X-ray microtomography and Itrax micro-X-ray fluorescence spectrometry analyses are presented. Results provide new data on differences in sediment properties and structure related to the former land use, indicating that increased agricultural activity leads to increased compaction and reduced porosity. The presence of anoxic conditions, indicative of poor hydrological connectivity between the terrestrial and post-inundation intertidal sediment facies, was only detected at one site. This site has experienced the highest rate of accretion over the terrestrial surface (ca. 7 cm over 36 months), suggesting that poor drainage is caused by the interaction (or lack of) between sediment facies rather than the former land use. This has significant implications for the design of future MR sites in terms of preparing sites, their anticipated evolution, and the delivery of ecosystem services. (C) 2019 Elsevier B.V. All rights reserved.
机译:正在实施管理调整计划(MR),以通过破坏防洪设施和淹没原本应保卫的沿海腹地来补偿潮间带盐沼栖息地的损失。但是,研究表明,MR地点的生物多样性低于预期,这与该地点以前的土地利用造成的压实和沉积物孔隙空间的塌陷导致缺氧和排水不良有关。尽管提出了生物多样性与土壤结构之间的这种联系,但很少研究过场地淹没后沉积物地下的演变,特别是在陆地向海洋或河口过渡的早期。本文提出了在现场淹没后的三年中,对梅德姆里管理重整场址(英国西萨塞克斯郡)的地下演化进行广泛和深入分析的新颖组合。分析了重复的大规模沉积物理化数据集,以评估沉积物地下的早期变化和前陆表的保存,并比较了不同前陆用途的四个位置。此外,针对这些位置中的两个位置,还提供了高强度3D计算X射线显微断层扫描和Itrax微型X射线荧光光谱分析。结果提供了与先前土地利用有关的沉积物特性和结构差异的新数据,表明增加的农业活动导致压实度增加和孔隙率降低。仅在一个地点发现了缺氧条件的存在,这表明陆地和淹没后潮间带沉积相之间的水文连通性较差。该地点在陆地表面的增生速率最高(在36个月内约7厘米),这表明排水不良是由于沉积物相之间的相互作用(或缺乏)而不是以前的土地利用引起的。从准备站点,它们的预期演变以及生态系统服务的交付方面,这对未来的MR站点的设计具有重要的意义。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第10期|1419-1432|共14页
  • 作者单位

    Coventry Univ, Sch Energy Construct & Environm, Coventry CV1 5FB, W Midlands, England;

    Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England;

    Queen Mary Univ London, Sch Geog, London E1 4NS, England;

    Queen Mary Univ London, Sch Geog, London E1 4NS, England|Univ Cumbria, Sci Nat Resources & Outdoor Studies, Rydal Rd, Ambleside LA22 9BB, Cumbria, England;

    Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England;

    Univ Brighton, Sch Environm & Technol, Ctr Aquat Environm, Brighton BN2 4GJ, E Sussex, England;

    Univ Brighton, Sch Environm & Technol, Ctr Aquat Environm, Brighton BN2 4GJ, E Sussex, England|Univ Witwatersrand, Sch Geog Archaeol & Environm Studies, Private Bag 3, ZA-2050 Johannesburg, South Africa;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Managed realignment; Microtomography; Sediment structure; Saltmarsh geochemistry; Itrax XRF;

    机译:管理重排;显微断层摄影术;沉积物结构;盐沼地球化学;Itrax XRF;

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