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首页> 外文期刊>Journal of Hydrology >Characteristics of sediment resuspension in Lake Taihu, China: A wave flume study
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Characteristics of sediment resuspension in Lake Taihu, China: A wave flume study

机译:太湖泥沙沉积物重新悬浮的特征:一种波浪水槽研究

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摘要

Lake Taihu is a typical shallow lake which frequently happens sediment resuspension induced by wind-induced waves. The experiments are carried on to simulate the wave disturbance processes in wave flume by setting a series of wave periods (1.2 s, 1.5 s, 1.8 s) and wave heights (2 cm, 10 cm). It aims to analyze the characteristics of sediment resuspension and the mechanisms of nutrients release and to evaluate the effects of sediment dredging on sediment resuspension and nutrients release in Lake Taihu. The results show that wave shear stress during 2 cm and 10 cm wave height processes ranges 0.018-0.023 N/m(2) and 0.221-0.307 N/m(2), respectively. Wave shear stress has no significant differences between wave periods. Wave height has much more effects on sediment resuspension. Wave height of 2 cm could induce total suspended solids (TSS) reaching up to 5.21 g/m(2) and resuspension flux of sediment (M) up to 1.74 g/m(2). TSS sharply increases to 30.33-52.41 g/m(2) and M reached up to 48.94 g/m(2) when wave height reaches to 10 cm. The disturbance depth under different sediment bulk weights ranges from 0.089 to 0.161 mm. Variation of suspended solids in 3 layers (1 cm, 5 cm, 20 cm above sediment interface) has no significant differences. Organic matter, TN and TP have positive relationship with SS. Organic matter is only accounted for 5.7%-7.3% of SS. The experiments under different sediment bulk densities (1.34 g/cm(3), 1.47 g/cm(3) and 1.59 g/cm(3)) find that TSS and M fall by 44.2% and 39.8% with sediment bulk density increasing, respectively. Total TN, DTN, TP and DTP decrease by 24.3%-33.6%. It indicates that sediment dredging could effectively reduce SS concentration and nutrient levels in water column. The researches provide a theoretical basis for sediment dredging to control the shore zone of Lake Taihu for lake management.
机译:太湖湖是一个典型的浅湖,经常发生被风引起的波浪引起的沉积物重悬浮。通过设定一系列波段(1.2秒,1.5秒,1.8秒)和波浪高(2cm,10cm),继续进行实验以模拟波浪管中的波扰动过程。它旨在分析​​沉积物重新悬浮的特征及营养素释放机制,并评价沉积物疏浚对太湖湖沉积物重悬的影响及营养释放。结果表明,在2cm和10cm波高程期间的波剪应力分别为0.018-0.023 n / m(2)和0.2221-0.307 n / m(2)。波剪应力在波时段之间没有显着差异。波浪高度对沉积物重新悬浮的影响更大。波高2cm的波形可以诱导总悬浮的固体(TSS)达到高达5.21g / m(2)的沉积物(M),沉积物(m)的重生通量高达1.74g / m(2)。 TSS急剧增加至30.33-52.41g / m(2),当波浪高达10厘米时,m达到高达48.94g / m(2)。不同沉积物散装重量下的扰动深度为0.089至0.161mm。 3层(1cm,5cm,沉积物界面上方1cm,5cm,20cm)中悬浮固体的变化没有显着差异。有机物,TN和TP与SS具有正相关关系。有机物仅占SS的5.7%-7.3%。在不同沉积物堆积密度下的实验(1.34g / cm(3),1.47g / cm(3)和1.59g / cm(3))发现TSS和M跌破44.2%和39.8%,沉积物堆积密度增加,分别。总TN,DTN,TP和DTP降低24.3%-33.6%。这表明沉积物疏浚可以有效地降低水柱中的SS浓度和营养水平。该研究为沉积物疏浚提供了理论依据,以控制太湖湖泊管理湖泊管理。

著录项

  • 来源
    《Journal of Hydrology》 |2018年第2018期|共9页
  • 作者单位

    China Univ Min &

    Technol Sch Resource &

    Geosci Xuzhou 221116 Jiangsu Peoples R China;

    China Univ Min &

    Technol Sch Resource &

    Geosci Xuzhou 221116 Jiangsu Peoples R China;

    Chinese Acad Sci State Key Lab Lake Sci &

    Environm Taihu Lab Lake Ecosyst Res Nanjing Inst Geog &

    Limnol Nanjing 210008 Jiangsu Peoples R China;

    Chinese Acad Sci State Key Lab Lake Sci &

    Environm Taihu Lab Lake Ecosyst Res Nanjing Inst Geog &

    Limnol Nanjing 210008 Jiangsu Peoples R China;

    Nanjing Hydraul Res Inst State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing 210029 Jiangsu Peoples R China;

    Nanjing Hydraul Res Inst State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing 210029 Jiangsu Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 水文科学(水界物理学);
  • 关键词

    Wave flume; Shear stress; Sediment resuspension; Sediment dredge; Nitrogen; Phosphorus;

    机译:波蝇;剪切应力;沉积物重新悬浮;沉积物疏通;氮;磷;

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