悬载流作用下平面床的线性稳定性分析

IF 2.8 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Dynamics Pub Date : 2023-10-06 DOI:10.5194/esurf-11-961-2023
Koji Ohata, Hajime Naruse, Norihiro Izumi
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引用次数: 0

摘要

摘要在河流和海洋环境中,平面河床在水流下发育;它们在砂岩层中被记录为平行层状,例如在浊积岩中发现的那些。然而,浊积岩通常表现为平行层叠,很少表现为沙丘尺度的交叉层叠。虽然浊积岩中缺乏沙丘尺度交叉层叠的原因仍有争议,但沙丘的形成可能受到悬浮载荷的抑制。在这里,我们首次进行了线性稳定性分析,表明具有悬浮载荷的流动促进了平面床的形成。对于细粒床层,悬浮荷载可以促进平面床层的形成,抑制沙丘的形成。这些理论分析结果与明渠水流作用下平面河床的观测资料进行了验证。我们的理论分析发现,悬浮荷载促进了平面床的形成,这表明在浊流条件下,悬浮荷载的存在抑制了沙丘的发育。
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Linear-stability analysis of plane beds under flows with suspended loads
Abstract. Plane beds develop under flows in fluvial and marine environments; they are recorded as parallel lamination in sandstone beds, such as those found in turbidites. However, whereas turbidites typically exhibit parallel lamination, they rarely feature dune-scale cross-lamination. Although the reason for the scarcity of dune-scale cross-lamination in turbidites is still debated, the formation of dunes may be dampened by suspended loads. Here, we perform, for the first time, linear-stability analysis to show that flows with suspended loads facilitate the formation of plane beds. For a fine-grained bed, a suspended load can promote the formation of plane beds and dampen the formation of dunes. These results of theoretical analysis were verified with observational data of plane beds under open-channel flows. Our theoretical analysis found that suspended loads promote the formation of plane beds, which suggests that the development of dunes under turbidity currents is suppressed by the presence of suspended loads.
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来源期刊
Earth Surface Dynamics
Earth Surface Dynamics GEOGRAPHY, PHYSICALGEOSCIENCES, MULTIDISCI-GEOSCIENCES, MULTIDISCIPLINARY
CiteScore
5.40
自引率
5.90%
发文量
56
审稿时长
20 weeks
期刊介绍: Earth Surface Dynamics (ESurf) is an international scientific journal dedicated to the publication and discussion of high-quality research on the physical, chemical, and biological processes shaping Earth''s surface and their interactions on all scales.
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