首页> 外文期刊>Polish Journal of Environmental Studies >Determination of Temporal Changes in the Sinuosity and Braiding Characteristics of the Kizilirmak River, Turkey
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Determination of Temporal Changes in the Sinuosity and Braiding Characteristics of the Kizilirmak River, Turkey

机译:土耳其基济马马克河的弯曲度和编织特征的时间变化测定

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摘要

In this study, the pattern of the approximately 1,300-km-long Kizilirmak River was recreated in a geographic information system (GIS) environment using data obtained from Landsat TM/ETM+/OLI satellite images from 1987, 2000, and 2013. The temporal changes in the sinuosity and braiding characteristics of the river were determined for the periods 1987-2000 and 2000-13. The right and left shorelines of the Kizilirmak River and the shorelines of islands and bars within the river channel were extracted automatically from the satellite images by integrating the normalized difference water index (NDWI) and modified normalized difference water index (MNDWI). The data required for measuring the sinuosity and braiding characteristics were obtained by evaluating the shorelines in the GIS environment. The braiding index (BI), braid-channel ratio (B), and braiding ratio (BR) were used to determine the braiding of the river, and the sinuosity index was used to determine the sinuosity of the river. The Kizilirmak River was divided into 21 analyzed sections based on the locations of dams. The sinuosity decreased in 15 sections in 1987-2000 and 2000-13. The BI, B, and BR values decreased in 11 sections in 1987-2000 and in 9 sections in 2000-13. Sinuosity and braiding both decreased in most of the sections downstream of dams; these sections were often subject to uncontrolled sand and gravel extractions.
机译:在这项研究中,使用从1987、2000和2013年的Landsat TM / ETM + / OLI卫星图像获得的数据,在地理信息系统(GIS)环境中重建了约1,300公里长的Kizilirmak河的格局。时间变化在1987-2000年和2000-13年确定了河流的弯曲度和编织特征。通过对归一化差水指数(NDWI)和修正归一化差水指数(MNDWI)进行积分,可以从卫星图像中自动提取出基兹利尔马克河的左右海岸线以及河道内的岛屿和小岛的海岸线。测量弯曲度和编织特性所需的数据是通过评估GIS环境中的海岸线获得的。使用编织指数(BI),编织通道比(B)和编织比(BR)来确定河流的编织,使用弯曲度指数来确定河流的弯曲度。根据大坝的位置,基济马马克河被分为21个分析段。 1987-2000年和2000-13年的15个断面的弯曲度降低了。 1987-2000年的11个区域和2000-13年的9个区域的BI,B和BR值均下降。大坝下游大部分断面的弯曲度和编织度均降低。这些断面经常受到不受控制的砂石砾石开采。

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