首页> 外文期刊>The Science of the Total Environment >The denitrification potential of eroding wetlands in Barataria Bay, LA, USA: Implications for river reconnection
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The denitrification potential of eroding wetlands in Barataria Bay, LA, USA: Implications for river reconnection

机译:美国路易斯安那州巴拉塔里亚湾湿地侵蚀的反硝化潜力:对河流重新连接的启示

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Expressions of eutrophication have led to increased stress on coastal ecosystems around the world. The nitrogen (N) removal potential of coastal wetland ecosystems is important due to increased loading of N to the coast. In Louisiana, there is rapid coastal wetland loss due primarily to the presence of river levees, which have isolated the coastal basins, and a high relative sea level rise. Ecosystem managers are planning to construct the Mid-Barataria sediment diversion which will reconnect the Mississippi River with Barataria Basin to build new wetlands and nourish existing marsh. The sediment diversion will deliver large amounts of nitrate into the surface waters of Barataria Bay. This research sought to quantify the nitrate removal potential of three bay zones: vegetated marsh, submerged peat fringe, and bay-bottom muddy estuarine sediment in intact soil cores incubated with a 2 mg L-1 N-NO3 water column. We noted: i) The areal nitrate reduction rates for the marsh, fringe, and estuary zones were 29.29 +/- 3.28, 18.83 +/- 1.31, and 10.83 +/- 0.62 mg N m(-2) day(-1), respectively; ii) the majority (similar to 93%) of NO3 was converted to N2O, indicating denitrification was the major NO3 reduction pathway; the submerged, eroded marsh soils (peat fringe zone) will play a large role in nitrate reduction due to increased contact time with the surface water. These findings can inform the predictive numerical models produced and utilized by ecosystem managers to better quantitatively understand how the coastal basin will respond to nutrient loading from river reconnection. In a broader context, the current relative sea level rise in coastal Louisiana is within the range of eustatic sea level rise that most stable coastlines will experience within the next 65-85 years. Therefore, these findings can serve as an example of potential future impacts to coastal wetland systems, globally, within the next century. (C) 2019 Elsevier B.V. All rights reserved.
机译:富营养化的表现导致世界各地沿海生态系统的压力增加。由于增加了对海岸的氮负荷,沿海湿地生态系统的除氮潜力非常重要。在路易斯安那州,沿海湿地的迅速丧失主要是由于河堤的存在,这些河堤隔离了沿海盆地,并且相对海平面上升很高。生态系统管理者正计划建造巴拉塔里亚中部的沉积物分流系统,这将使密西西比河与巴拉塔里亚盆地重新连接,以建造新的湿地并养护现有的沼泽。沉积物的转移会将大量硝酸盐输送到巴拉塔里亚湾的地表水中。这项研究试图量化三个海湾地区的硝酸盐去除潜力:植被沼泽,淹没的泥炭边缘和完整土壤芯中的海湾底泥质河口沉积物,并用2 mg L-1 N-NO3水柱孵育。我们注意到:i)沼泽,边缘和河口区的硝酸盐减少率分别为29.29 +/- 3.28、18.83 +/- 1.31和10.83 +/- 0.62 mg N m(-2)天(-1) , 分别; ii)大部分(约93%)的NO3转化为N2O,表明反硝化是主要的NO3还原途径;由于与地表水的接触时间增加,淹没的侵蚀性沼泽土壤(豌豆边缘带)将在减少硝酸盐方面发挥重要作用。这些发现可以为生态系统管理者产生和利用的预测性数值模型提供信息,以更好地定量了解沿海流域将如何响应河流重新汇聚的养分。在更广泛的背景下,路易斯安那州沿海地区当前的相对海平面上升幅度在接下来的65至85年内最稳定的海岸线将经历的向海平面上升的范围内。因此,这些发现可以作为未来一个世纪内全球对沿海湿地系统潜在影响的例子。 (C)2019 Elsevier B.V.保留所有权利。

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