Toward flow forces acting on a step-pool unit

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Chendi Zhang , Marwan A. Hassan , Yuncheng Xu
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引用次数: 0

Abstract

The flow forces on step-pool units are important to understand the physical processes and flow resistance partitioning in step-pool channels, and build the basis for better prediction of channel evolution and more advanced design of artificial step-pool system. However, the flow forces acting on step-pool units are understudied and poorly understood. To fill this knowledge gap, we applied the approach combining physical experiment and computational fluid dynamics simulation to a step-pool unit made of natural grains at six flow conditions. The topography of the step-pool unit was split into topography components (TCs) covering the entire unit length with the same width. The flow forces from both pressure and shear stress in XYZ directions were examined for the TCs. The results illustrate significant transverse variability of the flow forces from both the shear stress and pressure at all the three directions. The flow forces in both X and Y directions are closely related to the flow structures and morphology in the unit. The ratios between skin and form drag have large variations at low flows while show a relatively limited range of 0.05–0.1 at high flows, suggesting a small proportion occupied by the skin resistance in the total flow resistance in the step-pool channel. The drag and lift coefficient generally increase with discharge and the drag coefficient of the unit is around 0.3 at high flows, which can be used in evaluating the stability of the step-pool units in a sequence.
作用在阶梯池单元上的流向力
台阶水池单元上的流动力对于了解台阶水池渠道的物理过程和流动阻力分区非常重要,可为更好地预测渠道演变和更先进的人工台阶水池系统设计奠定基础。然而,人们对作用于台阶池单元的流力研究不足,了解甚少。为了填补这一知识空白,我们采用物理实验和计算流体动力学模拟相结合的方法,在六种流动条件下对天然谷物制成的阶梯池单元进行了研究。阶梯池单元的地形被分割成覆盖整个单元长度且宽度相同的地形组件(TC)。研究了这些 TC 在 XYZ 方向上的压力和剪应力流动力。结果表明,在所有三个方向上,来自剪应力和压力的流动力都存在明显的横向变化。X 和 Y 方向的流力与单元内的流动结构和形态密切相关。在低流量时,表皮阻力和形态阻力的比值变化很大,而在高流量时,比值范围相对有限,仅为 0.05-0.1,这表明表皮阻力在阶梯池水道的总流阻中所占比例很小。阻力系数和升力系数一般随排水量的增加而增大,大流量时单元的阻力系数约为 0.3,可用于评价梯级水池单元的稳定性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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