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Spatiotemporal Distribution of Eutrophication in Lake Tai as Affected by Wind

机译:风对太湖富营养化时空分布的影响

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One common hypothesis is that wind can affect concentrations of nutrients (i.e., nitrogen and phosphorus) and chlorophyll-a (Chl-a) in shallow lakes. However, the tests of this hypothesis have yet to be conclusive in existing literature. The objective of this study was to use long-term data to examine how wind direction and wind speed affect the spatiotemporal variations of total nitrogen (TN), total phosphorus (TP) and Chl-a in Lake Tai, a typical shallow lake located in east China. The results indicated that the concentrations of nutrients and Chl-a tended to decrease from the northwest to the southeast of Lake Tai, with the highest concentrations in the two leeward bays (namely Meiliang Bay and Zhushan Bay) in the northwestern part of the lake. In addition to possible artificial reasons (e.g., wastewater discharge), the prevalent southeastward winds in warm seasons (i.e., spring and summer) and northwestward winds in cool seasons (i.e., fall and winter) might be the major natural factor for such a northwest-southeast decreasing spatial pattern. For the lake as a whole, the concentrations of TN, TP and Chl-a were highest for a wind speed between 2.1 and 3.2 m·s ?1 , which can be attributed to the idea that the wind-induced drifting and mixing effects might be dominant in the bays while the wind-induced drifting and resuspension effects could be more important in the other parts of the lake. Given that the water depth of the bays was relatively larger than that of the other parts, the drifting and mixing effects were likely dominant in the bays, as indicated by the negative relationships between the ratios of wind speed to lake depth, which can be a surrogate for the vertical distribution of wind-induced shear stress and the TN, TP and Chl-a concentration. Moreover, the decreasing temporal trend of wind speed in combination with the ongoing anthropogenic activities will likely increase the challenge for dealing with the eutrophication problem of Lake Tai.
机译:一种常见的假设是,风会影响浅湖中养分(即氮和磷)和叶绿素-a(Chl-a)的浓度。然而,对这一假设的检验在现有文献中尚无定论。这项研究的目的是使用长期数据来研究风向和风速如何影响太湖中的典型总浅湖太湖中总氮(TN),总磷(TP)和Chl-a的时空变化。中国东部。结果表明,养分和Chl-a的浓度从太湖的西北向东南呈下降趋势,在湖西北部的两个背风海湾(即梅良湾和竹山湾)浓度最高。除了可能的人为原因(例如废水排放)之外,暖季(即春季和夏季)中的东南风和凉爽季节(即秋季和冬季)中的西北风可能是造成此类西北风的主要自然因素。 -东南减少的空间格局。对于整个湖泊来说,TN,TP和Chl-a的浓度在风速为2.1至3.2 m·s?1时最高,这可以归因于风致漂移和混合效应可能在海湾中占主导地位,而风引起的漂流和再悬浮效应在湖的其他部分可能更为重要。鉴于海湾的水深比其他部分的水深大,在海湾中漂流和混合效应很可能占主导地位,这由风速与湖泊深度之比之间的负关系表明,这可能是替代风致切应力和TN,TP和Chl-a浓度的垂直分布。此外,风速的下降趋势与正在进行的人为活动相结合,可能会增加应对太湖富营养化问题的挑战。

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