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Dissolved oxygen in contrasting estuaries of the Bay of Biscay: effects of temperature, river discharge and chlorophyll a

机译:比斯开湾相对河口中的溶解氧:温度,河流流量和叶绿素a的影响

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摘要

The effects of environmental factors on variations of dissolved oxygen (DO) saturation was assessed in 2 estuaries (Bilbao and Urdaibai) in the Bay of Biscay with contrasting hydrography and anthropogenic impact, for the period 1997 to 2006, using generalised additive models (GAMs) and generalised additive mixed models (GAMMs). Spatial and temporal variations in DO saturation and the current severity and extent of hypoxia were higher in the culturally eutrophicated and stratified Bilbao estuary. Seasonal patterns of DO saturation and the hierarchy of factors controlling them differed both between estuaries and between salinity zones. In the inner Bilbao estuary, the main factor explaining DO-saturation variations was temperature, with a dominant effect on oxygen consumption processes. In contrast, in the outer Bilbao estuary, the main factor explaining DO-saturation variations was chlorophyll a, suggesting that the effect of oxygen production through photosynthesis was stronger than that of oxygen consumption. In the inner Urdaibai estuary, both a negative relationship with temperature and a positive relationship with chlorophyll a were detected. The outer Urdaibai estuary showed strong water-column mixing and very high tidal flushing, and ventilation processes were more important than oxygen production or consumption processes. River discharge affected DO saturation only at the inner waters, but when the effects of several variables on DO-saturation variability were tested in an additive model, river discharge was excluded from the models. The effects of temperature-dependent processes on DO-saturation dynamics decreased from the inner to the outer zones of both estuaries.
机译:使用广义加性模型(GAM),在1997年至2006年期间,利用对比水文学和人为影响,在比斯开湾的两个河口(毕尔巴鄂和乌尔代拜)评估了环境因素对溶解氧(DO)饱和度变化的影响。以及广义加性混合模型(GAMM)。在富营养化和分层的毕尔巴鄂河口,DO饱和度的时空变化以及当前缺氧的严重程度和程度更高。在河口之间和盐度区之间,溶解氧饱和度的季节性模式和控制它们的因素的层次都不同。在毕尔巴鄂内河口,解释溶解氧饱和度变化的主要因素是温度,这对耗氧过程起主要作用。相反,在毕尔巴鄂外河口,解释DO饱和度变化的主要因素是叶绿素a,这表明通过光合作用产生氧气的作用比消耗氧气的作用强。在乌尔代拜河内河口,与温度呈负相关,与叶绿素a呈正相关。乌尔代拜河外河口显示出强烈的水柱混合和非常高的潮汐冲刷,通风过程比氧气生产或消耗过程更为重要。河流排放仅影响内部水域的DO饱和度,但是在加性模型中测试了几个变量对DO饱和度变异性的影响时,模型中排除了河流排放。温度依赖性过程对溶解氧饱和度动力学的影响从两个河口的内部到外部区域都减小了。

著录项

  • 来源
    《Marine ecology progress series》 |2010年第18期|p.57-71|共15页
  • 作者单位

    Laboratory of Ecology, Department of Plant Biology and Ecology, Faculty of Science and Technology, University of the Basque Country, PO Box 644, 48080 Bilbao, Spain;

    Laboratory of Ecology, Department of Plant Biology and Ecology, Faculty of Science and Technology, University of the Basque Country, PO Box 644, 48080 Bilbao, Spain;

    Laboratory of Ecology, Department of Plant Biology and Ecology, Faculty of Science and Technology, University of the Basque Country, PO Box 644, 48080 Bilbao, Spain;

    Laboratory of Ecology, Department of Plant Biology and Ecology, Faculty of Pharmacy, University of the Basque Country, Paseo de la Universidad 7, 01006 Gasteiz, Spain;

    Basque Foundation for Health Innovation and Research (BIOEF), 48015 Sondika, Bizkaia, Spain,Biomedical Research Center, 31008 Pamplona, Spain;

    Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biology, University of Oslo, PO Box 1066 Blindern, 0316 Oslo, Norway,Instituto Espanol de Oceanografia (IEO), Centro Oceanografico de Cadiz, Puerto Pesquero, Muelle de Levante s, PO Box 2609, 11006 Cadiz, Andalucia, Spain;

    Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biology, University of Oslo, PO Box 1066 Blindern, 0316 Oslo, Norway,Fl0devigen Marine Research Station, Institute of Marine Research, 4817 His, Norway;

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

    dissolved oxygen; chlorophyll; temperature; river discharge; estuary; generalised additive models; bay of biscay;

    机译:溶解氧叶绿素温度;河水排放河口;广义加性模型;比斯开湾;

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