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Waves-waves collide induced by different wind directions caused high exchanged in the water level at the open area Shallow Lake, China

机译:不同风向引起的波-波碰撞在中国浅湖的开放区域引起水位的高交换

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Wind from different directions induce waves-waves to collid at the central zone of Taihu Lake. It causes exchange in water bodies and release of internal nutrients which increases algal bloom. This study aims to analyz the impact of the interactions between waves-waves collision from different directions and different sources such as traveling ships and explored factors, causing sediment resuspension. The results were achieved to collect high-frequency data for measuring wind speeds, currents, waves, and suspended solid concentration (SSCs). The results indicate that the water exchange and the turbidity highly escalated when wind speeds reached 5 m/s. The surface flow velocities are very high, about 80 cm/s or more according to the raw data after calibrating the instruments. This finding is very important in the processes of sediments dynamic. Maybe in these wide area, high waves waves collide leading to constructive interference from different sources generate waves. Sediment processes were categorized into three period A, B, and C corresponding to three shear-stress thresholds. Period A: Sediment bottom particals was stable with 0.01 N/m2. It did not change through this period and the averaged suspended solid concentration (SSCs) was approximately 50 mg/L. Period B: Sediment resuspension was small with a range between 0.1 N/m2. It jumped up slowly and the averaged was in the range of 50 to 70 mg/L. Period C: Sediment resuspension was moderate with shear stress 0.1 0.8 N/m2. The form of the sediment bed was changed at the second period, this shows that increase of the shear stress activated the sediment in this period. The bottom SSCs increased quickly from 60 to 350 mg/L in average. Outcomes of this paper presents the main factor causing sediment resuspension, which may assist further studies and estimate the real reasons for internal nutrient release from different waves induced waves-waves to collide in Lake Taihu.
机译:来自不同方向的风在太湖中心带引起波波碰撞。它引起水体交换并释放内部营养,从而增加藻华。本研究旨在分析不同方向和不同来源(如游轮和探索的因素)引起的波-波碰撞之间相互作用的影响,从而引起沉积物重悬浮。获得了收集高频数据以测量风速,电流,波浪和悬浮固体浓度(SSC)的结果。结果表明,当风速达到5 m / s时,水交换和浊度高度升高。校准仪器后,根据原始数据,表面流速非常高,约为80 cm / s或更高。这一发现在沉积物动力学过程中非常重要。也许在这些广阔的区域中,高波相撞,导致来自不同来源的相长干涉产生波。泥沙过程分为三个时期A,B和C,分别对应三个切应力阈值。时期A:沉积物底部颗粒稳定在0.01 N / m2。在此期间它没有变化,平均悬浮固体浓度(SSCs)约为50 mg / L。时期B:沉积物的重悬很小,范围在0.1 N / m2之间。它缓慢跳升,平均值在50至70 mg / L的范围内。时期C:沉积物重度中等,剪切应力为0.1 0.8 N / m2。在第二阶段改变了沉积物床的形式,这表明在该时期剪切应力的增加激活了沉积物。底部SSCs从60 mg / L快速增加到平均350 mg / L。本文的结果提出了造成泥沙重新悬浮的主要因素,这可能有助于进一步的研究,并估计造成不同养分的内部养分释放的真正原因。

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