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首页> 外文期刊>Journal of Hydrology >Artificial water sediment regulation scheme influences morphology, hydrodynamics and nutrient behavior in the Yellow River estuary
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Artificial water sediment regulation scheme influences morphology, hydrodynamics and nutrient behavior in the Yellow River estuary

机译:人工水沙调节方案影响黄河口的形态,水动力和养分行为

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Anthropogenic controls on water and sediment may play important roles in river system transformations and morphological evolution, which could further affect coastal hydrodynamics and nutrient behavior. We used geochemical tracers to evaluate the influence of an intentional large release of water and sediment during the so-called "Water Sediment Regulation Scheme" (WSRS) on estuarine morphology, hydrodynamics and nutrients in the Yellow River estuary, China. We discovered that there was a newly formed small delta in the river mouth after the 2013 WSRS. This new morphologic feature altered terrestrial material distribution patterns from a single plume to a two-plume pattern within the estuary. Our results show that the WSRS significantly influenced the study area in the following ways: (1) Radium and nutrient concentrations were significantly elevated (two to four times), especially along the two river outlets. (2) Estuarine mixing was about two times stronger during WSRS than before. Average aerial mixing rates before and during WSRS were 50 +/- 26 km(2) d(-1) and 89 +/- 51 km(2) d(-1), respectively. (3) Our data is consistent with P limitation and suggest that stoichiometrically based P limitation was even more severe during WSRS. (4) All river-derived nutrients were thoroughly consumed within one to two weeks after entry to near-shore waters. (5) The extent of the area influenced by terrestrial nutrients was two to three times greater during WSRS. Human influence, such as triggered by WSRS regulations, should thus be considered when studying biogeochemical processes and nutrient budgets in situations like the Yellow River estuary. (C) 2016 Elsevier B.V. All rights reserved.
机译:水和沉积物的人为控制可能在河流系统的转变和形态演变中起重要作用,这可能进一步影响沿海的水动力和养分行为。我们使用地球化学示踪剂评估了所谓的“水沙调节方案”(WSRS)期间故意大量释放水和沉积物对黄河口河口形态,水动力和养分的影响。我们发现,2013年WSRS之后,河口有一个新形成的小三角洲。这种新的形态学特征将河口内的陆地物质分布模式从单羽模式改变为两羽模式。我们的结果表明,WSRS通过以下方式对研究区域产生了显着影响:(1)尤其是在两个河流出口处,镭和养分浓度显着升高(2至4倍)。 (2)在WSRS期间,河口混合作用比以前强大约两倍。 WSRS之前和期间的平均空中混合速率分别为50 +/- 26 km(2)d(-1)和89 +/- 51 km(2)d(-1)。 (3)我们的数据与P限制一致,并表明基于化学计量的P限制在WSRS期间更为严重。 (4)进入近岸水域后的一到两周内,所有源自河流的养分被彻底消耗。 (5)在WSRS期间,受地面养分影响的区域范围扩大了2至3倍。因此,在黄河河口等情况下研究生物地球化学过程和养分预算时,应考虑诸如WSRS法规引发的人为影响。 (C)2016 Elsevier B.V.保留所有权利。

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