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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Silting patterns in the reservoirs of small- and medium-sized earthen check dams in humid subtropical monsoon regions
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Silting patterns in the reservoirs of small- and medium-sized earthen check dams in humid subtropical monsoon regions

机译:潮湿亚热带季风区的小型和中型土丘脑水库中的淤泥图案

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摘要

Silting of reservoirs is a ubiquitous process whenever water is impounded. Despite substantial work on the rates of silting, the spatial pattern of silting in reservoirs is not clearly understood. While it is anticipated that the variability of silting increases with decreasing reservoir size, not much is known about siltation in subtropical humid regions affected by monsoon rainfall. This paper presents the initial results of geomorphic analysis of six earthen check dams in the Shiwalik foothills of the Himalayas (India) in areas that are inhabited by high proportions of disempowered populations. These check dams include three small-sized dams (Dhamala-II, Rel Majra and Sukhomajri-II) and three medium-sized dams (Bunga-I, Parachh-II and Siswan). Field data were collected from each reservoir. The methods used included spatial interpolations of bed depth and silt thickness in each reservoir, Structure from Motion photogrammetry to extract multiple channel cross-sections from photographic scans along tributary mouths, texture analysis of bed and bank materials, and visual observations of hill slopes around the check dams. Based on this study, silt tended to concentrate either in the middle portion of the reservoir or near the dam; however, silt accumulation did not always occur along the dam or in the deepest portion of the reservoirs. Areas located downstream from these check dams are heavily used for various human activities and the channel network has almost been eliminated. While these earthen check dams may be cost-effective tools for water conservation in economically marginalized areas, if abandoned, these structures may pose a physical hazard to downstream communities. (c) 2019 John Wiley & Sons, Ltd.
机译:每当水被扣押,水库的淤泥是一种普遍存在的过程。尽管对淤泥的速度进行了大量的工作,但淤泥在水库中的空间模式没有清楚地理解。虽然预计淤泥的淤泥量随储层尺寸的降低而增加,但对于受季风降雨影响的亚热带潮湿地区的淤积并不多。本文介绍了在喜马拉雅山(印度)的Shiwalik脚下六个土地尸体的几何分析的初步结果,在高比例的丢弃群体中居住。这些校验坝包括三个小型大型水坝(Dhamala-II,Rel Majra和Sukhomajri-II)和三个中型水坝(Bunga-I,Parachh-II和Siswan)。从每个油库收集现场数据。使用的方法包括每个储存器中的床深度和淤泥厚度的空间插值,从运动摄影测量中的结构沿着沿着支流的嘴,床和银行材料的纹理分析提取来自摄影扫描的多声道横截面,以及山坡的视觉观察检查水坝。基于这项研究,淤泥倾向于集中在水库的中间部分或坝附近;然而,淤泥积聚并不总是沿着大坝或储层的最深部分发生。这些检查坝下游的区域大量用于各种人类活动,渠道网络几乎已被消除。虽然这些土壤检查坝可能是经济边缘化区域的水系的经济高效工具,但是,如果放弃,这些结构可能对下游社区构成了物理危害。 (c)2019 John Wiley&Sons,Ltd。

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