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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Marsh accretion and sediment accumulation in a managed tidal wetland complex of Delaware Bay
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Marsh accretion and sediment accumulation in a managed tidal wetland complex of Delaware Bay

机译:特拉华湾受管理的潮汐湿地综合体的沼泽积聚和沉积物积累

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摘要

Wetland impoundments are created to provide ecological benefits such as water quality improvement, mosquito control, and migratory bird habitat. Prime Hook National Wildlife Refuge, located on the southwestern shore of the Delaware Bay, is composed of four interconnected wetland management units. Tidal inflow from Delaware Bay to Units I and IV occurs naturally, whereas flow to Units II and III has been restricted by tidal gates since the mid-1980s. To assess the accretionary status of Refuge marshes and inform an ongoing restoration, we investigated soil physical properties and developed Cs-137 and Pb-210 radiochronologies for cores collected at twelve sites. Results indicate that marsh accretion is driven by a combination of mineral sediment and organic matter accumulation, the relative proportions of which vary among and within the wetland units. Accretion rates (0.11-0.54 cm/y) were found to be significantly correlated with organic matter accumulation but not with mineral sediment accumulation. These relationships demonstrate that biotic contributions to marsh accretion, such as belowground biomass productivity, must be considered in marsh restoration strategies, in addition to the supply of mineral sediment. At eight of the sites, the contribution of mineral sediment to the total volume of the soils has decreased significantly since the early 1900s, predating the impoundment works, perhaps in association with closure of two tidal inlets by natural processes. By comparison, changes in organic soil volume were relatively small over the same time span. At seven of the sites the marsh is accreting at, to just below, the rate of local relative sea-level rise (0.34 +/- 0.03 cm/y) with potential for submergence on the long term. Additional research at the Refuge is needed to better align measurements of marsh accretion, relative sea-level from tide gauges, and wetland elevation change. (C) 2016 Elsevier B.V. All rights reserved.
机译:创建湿地蓄水池是为了提供生态效益,例如改善水质,控制蚊子和候鸟栖息地。总理钩国家野生动物保护区位于特拉华湾的西南海岸,由四个相互连接的湿地管理单位组成。从特拉华湾流向I和IV单元的潮汐自然发生,而自1980年代中期以来,流向门II和III的流量一直受到潮汐闸门的限制。为了评估避难所沼泽的增生状况并为正在进行的恢复提供信息,我们调查了土壤的物理特性,并针对在十二个地点收集的岩心开发了Cs-137和Pb-210放射性年代学。结果表明,沼泽沉积物是由矿物沉积物和有机质积累共同驱动的,其相对比例在湿地单元之间和内部不同。发现吸积率(0.11-0.54 cm / y)与有机物积累显着相关,但与矿物沉积物积累却无关。这些关系表明,除了提供矿质沉积物以外,还必须在沼泽恢复策略中考虑对沼气积聚的生物贡献,例如地下生物量生产力。自1900年代初以来,在八个地点中,矿物沉积物对土壤总体积的贡献已显着下降,这可能是在蓄水工程之前,可能是由于自然过程关闭了两个潮汐入口。相比之下,同一时间段内有机土壤体积的变化相对较小。在其中的七个地点,沼泽以当地相对海平面上升速度(0.34 +/- 0.03厘米/年)的速率增加至其正下方,并可能长期淹没。需要在避难所进行其他研究,以更好地调整沼泽积聚,潮汐仪相对海平面和湿地海拔变化的度量。 (C)2016 Elsevier B.V.保留所有权利。

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