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恢复前土地利用和干扰对盐沼恢复后沉积物结构、水文学和沉积物地球化学环境的影响。

The impact of pre-restoration land-use and disturbance on sediment structure, hydrology and the sediment geochemical environment in restored saltmarshes.

机构信息

School of Geography, Queen Mary University of London, Mile End Road, London E1 4NS, UK.

School of Geography, Queen Mary University of London, Mile End Road, London E1 4NS, UK.

出版信息

Sci Total Environ. 2017 Jun 1;587-588:47-58. doi: 10.1016/j.scitotenv.2016.11.032. Epub 2017 Feb 16.

Abstract

Saltmarshes are being lost or degraded as a result of human activity resulting in loss of critical ecosystem services including the provision of wild species diversity, water quality regulation and flood regulation. To compensate, saltmarshes are being restored or re-created, usually driven by legislative requirements for increased habitat diversity, flood regulation and sustainable coastal defense. Yet, there is increasing evidence that restoration may not deliver anticipated ecosystem services; this is frequently attributed to poor drainage and sediment anoxia. However, physical sediment characteristics, hydrology and the sediment geochemical environment are rarely examined in restoration schemes, despite such factors being critical for plant succession. This study presents the novel integration of 3D-computed X-ray microtomography to quantify sediment structure and porosity, with water level and geochemical data to understand the impact of pre-restoration land use and disturbance on the structure and functioning of restored saltmarshes. The study combines a broad-scale investigation of physical sediment characteristics in nine de-embanked saltmarshes across SE England, with an intensive study at one site examining water levels, sediment structure and the sediment geochemical environment. De-embankment does not restore the hydrological regime, or the physical/chemical framework in the saltmarshes and evidence of disturbance includes a reduction in microporosity, pore connectivity and water storage capacity, a lack of connectivity between the sub-surface environment and overlying floodwaters, and impeded sub-surface water flow and drainage. This has significant consequences for the sediment geochemical environment. This disturbance is evident for at least two decades following restoration and is likely to be irreversible. It has important implications for plant establishment in particular, ecosystem services including flood regulation, nutrient cycling and wild species diversity and for future restoration design.

摘要

由于人类活动导致盐沼丧失或退化,包括提供野生物种多样性、水质调节和洪水调节等关键生态系统服务都受到了影响。为了弥补这一损失,盐沼正在被恢复或重新创造,这通常是由立法要求增加栖息地多样性、洪水调节和可持续海岸防御驱动的。然而,越来越多的证据表明,恢复可能无法提供预期的生态系统服务;这通常归因于排水不良和沉积物缺氧。然而,在恢复方案中,很少检查物理沉积物特征、水文学和沉积物地球化学环境,尽管这些因素对植物演替至关重要。本研究提出了将三维计算机断层扫描技术用于量化沉积物结构和孔隙度的新方法,并结合水位和地球化学数据,以了解恢复前土地利用和干扰对恢复盐沼结构和功能的影响。该研究结合了对英格兰东南部九个去堤盐沼的物理沉积物特征的广泛调查,以及在一个地点对水位、沉积物结构和沉积物地球化学环境进行的深入研究。去堤并不能恢复水文状况或盐沼的物理/化学框架,证据表明存在干扰,包括微孔隙减少、孔隙连通性和储水能力降低、地下环境与上层洪水之间缺乏连通性,以及地下水流和排水受阻。这对沉积物地球化学环境有重大影响。这种干扰在恢复后至少持续二十年,并且可能是不可逆转的。这对植物的建立、特别是对生态系统服务(包括洪水调节、养分循环和野生物种多样性)以及未来的恢复设计都有重要影响。

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