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Effect of tidal flooding on metal distribution in pore waters of marsh sediments and its transport to water column (Tagus estuary, Portugal)

机译:潮汐洪水对沼泽沉积物孔隙水中金属分布的影响及其向水柱的迁移(葡萄牙塔古斯河口)

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摘要

Sediment cores and flooding water were collected at 0, 5,10 and 50 min of tidal inundation in two sites of the Rosario salt marsh located in the proximity of a heavy industrialised zone of Tagus estuary colonised by pure stands of Spartina maritima (low marsh) and Sarcocornia fruticosa (high marsh). The cores were sliced in 5 cm layers and sediment solids, pore water, and belowground biomass were separated in order to measure Fe, Mn, Zn, Cu, Pb and Cd. The pore waters and sediments colonised by S. fruticosa, as well as belowground biomass presented high concentrations of Zn, Cu, Pb and Cd. Below-ground biomass exceeded in one order of magnitude the metal levels in sediments. Abundant belowground biomass and small dimension of S. fruticosa roots facilitates the root-sediment interactions and presumably the metal retention in the higher marsh. The novelty of this work is the result of tidal inundation on pore water concentrations of metals in salt marsh sediments and their exportation to the water column. Concentrations in pore waters varied at minute scales, but 50 min after inundation levels were comparable to the initial values. The metal levels in flooding water increased abruptly during the first 10-20 min of inundation. The concentration peaks (Fe = 60 μM, Mn = 7.5 μM, Zn = 1.7 uM, Cu = 550 nM, Pb = 100 nM, Cd = 1.7 nM) reached one to two orders of magnitude above the values found in subsequent periods of inundation. The advective transports during the 50 min inundation during two daily pulses of inundation were: Fe (9520 and 1640), Mn (24), Zn (220 and 82), Cu (74 and 16), Pb (13 and 15) and Cd (0.3 and 0.08) for S. maritima and S. fruticosa, respectively. These quantities exceeded three to four orders of magnitude of the corresponding predicted diffusive fluxes (Fick 1st law) on a daily basis. This work emphasizes the importance of tidal flooding over salt marsh sediments to the metal exportation to the water column.
机译:在潮汐淹没的第0、5、10和50分钟时,在罗萨里奥盐沼的两个地点收集了沉积物核心和洪水,该地点位于塔霍斯河口重工业区附近,被纯净的Spartina maritima林分定殖(低沼泽)和Sarcocornia fruticosa(高沼地)。将岩心切成5厘米厚的层,并分离出沉积物固体,孔隙水和地下生物量,以测量铁,锰,锌,铜,铅和镉。金黄色葡萄球菌定居的孔隙水和沉积物,以及地下生物量呈现出高浓度的Zn,Cu,Pb和Cd。地下生物量超过沉积物中金属含量的一个数量级。丰富的地下生物量和金黄色葡萄球菌根的小尺寸促进了根-沉积物的相互作用,并促进了高沼泽地中的金属保留。这项工作的新颖性是潮汐淹没了盐沼沉积物中金属孔隙水浓度并将其排入水柱的结果。孔隙水中的浓度以分钟为单位变化,但淹没后50分钟的水平与初始值相当。在淹没的前10到20分钟内,洪水中的金属含量突然增加。浓度峰值(Fe = 60μM,Mn = 7.5μM,Zn = 1.7 uM,Cu = 550 nM,Pb = 100 nM,Cd = 1.7 nM)比随后的淹没期高出一到两个数量级。在每天两次浸水脉冲期间,浸水50分钟期间的对流输运为:Fe(9520和1640),Mn(24),Zn(220和82),Cu(74和16),Pb(13和15)和Cd maritima和f.ticutosa分别为(0.3和0.08)。这些量每天超过相应的预测扩散通量(菲克斯第一定律)的三到四个数量级。这项工作强调了盐沼沉积物上的潮汐泛滥对金属向水柱输出的重要性。

著录项

  • 来源
    《Marine Environmental Research》 |2010年第5期|p.358-367|共10页
  • 作者单位

    Marine Research Institute (CSIC), Department of Oceanography, Eduardo Cabello 6, 36208 Vigo, Spain,INRB/IPIMAR, National Institute of Biological Resources, Avenida Brasilia, 1446-006 Lisboa, Portugal;

    INRB/IPIMAR, National Institute of Biological Resources, Avenida Brasilia, 1446-006 Lisboa, Portugal;

    INRB/IPIMAR, National Institute of Biological Resources, Avenida Brasilia, 1446-006 Lisboa, Portugal;

    INRB/IPIMAR, National Institute of Biological Resources, Avenida Brasilia, 1446-006 Lisboa, Portugal;

    Marine Research Institute (CSIC), Department of Oceanography, Eduardo Cabello 6, 36208 Vigo, Spain;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    salt marsh; metals; pore waters; tagus estuary; advective; diffusive; fluxes; tidal flooding;

    机译:盐沼金属;毛孔水塔霍河口;平流扩散助焊剂潮水;

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