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首页> 外文期刊>Journal of Hydrology >Measuring groundwater-surface water interaction and its effect on wetland stream benthic productivity, Trout Lake watershed, northern Wisconsin, USA
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Measuring groundwater-surface water interaction and its effect on wetland stream benthic productivity, Trout Lake watershed, northern Wisconsin, USA

机译:在美国威斯康星州北部的鳟鱼湖流域,测量地下水与地表水的相互作用及其对湿地底栖生产力的影响

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摘要

Measurements of groundwater-surface water exchange at three wetland stream sites were related to patterns in benthic productivity as part of the US Geological Survey's Northern Temperate Lakes-Water, Energy and Biogeochemical Budgets (NTL-WEBB) project. The three sites included one high groundwater discharge (HGD) site, one weak groundwater discharge (WGD) site, and one groundwater recharge (GR) site. Large upward vertical gradients at the HGD site were associated with smallest variation in head below the stream and fewest gradient reversals between the stream and the groundwater beneath the stream, and the stream and the adjacent streambank. The WGD site had the highest number of gradient reversals reflecting the average condition being closest to zero vertical gradient. The duration of groundwater discharge events was related to the amount of discharge, where the HGD site had the longest strong-gradient durations for both horizontal and vertical groundwater flow. Strong groundwater discharge also controlled transient temperature and chemical hyporheic conditions by limiting the infiltration of surface water. Groundwater-surface water interactions were related to highly significant patterns in benthic invertebrate abundance, taxonomic richness, and periphyton respiration. The HGD site abundance was 35% greater than in the WGD site and 53% greater than the GR site; richness and periphyton respiration were also significantly greater (P <= 0.001, 31 and 44%, respectively) in the HGD site than in the GR site. The WGD site had greater abundance (27%), richness (19%) and periphyton respiration (39%) than the GR site. This work suggests groundwater-surface water interactions can strongly influence benthic productivity, thus emphasizing the importance of quantitative hydrology for management of wetland-stream ecosystems in the northern temperate regions. (C) 2005 Elsevier B.V. All rights reserved.
机译:作为美国地质调查局北温带湖泊-水,能源和生物地球化学预算(NTL-WEBB)项目的一部分,对三个湿地河流站点的地下水-地表水交换的测量与底栖生产力的模式有关。这三个地点包括一个高地下水排放(HGD)站点,一个弱地下水排放(WGD)站点和一个地下水补给(GR)站点。 HGD站点上的较大的向上垂直梯度与溪流下方水头的最小变化和溪流与溪流下方的地下水以及溪流和相邻溪流之间最小的梯度反转相关。 WGD站点的梯度反转次数最多,反映了平均条件最接近零垂直梯度。地下水排放事件的持续时间与排放量有关,其中HGD站点在水平和垂直地下水流中具有最长的强梯度持续时间。强大的地下水排放还通过限制地表水的渗透来控制瞬态温度和化学流变条件。地下水与地表水的相互作用与底栖无脊椎动物的丰度,生物分类学丰富度和水生植物呼吸作用的高度重要模式有关。 HGD站点的丰度比WGD站点高35%,比GR站点高53%; HGD位点的丰富度和浮游植物呼吸也显着大于GR位点(分别为P <= 0.001、31%和44%)。 WGD站点比GR站点具有更高的丰度(27%),丰富度(19%)和浮游植物呼吸(39%)。这项工作表明,地下水与地表水的相互作用会极大地影响底栖生产力,从而强调定量水文学对于北部温带地区湿地河流生态系统管理的重要性。 (C)2005 Elsevier B.V.保留所有权利。

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