结合遥感和GIS数据的scs - cn方法评价塔皮盆地下游支流洪水潜力

Sudhakar B. Sharma, Anupam K. Singh
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引用次数: 8

摘要

本文的研究目的是基于流域特征来识别具有高洪水潜力的流域,以形成地表径流。SCS-CN方法依靠遥感和GIS数据获取流域特征。利用3米精度的全球定位系统(GPS),结合印度测绘地形图,生成了一个30米栅格尺寸的数字高程模型(DEM),比例尺为1:5万,等高线间隔为10米。收集了现场未受干扰的土壤样品,并根据ASTM D1557和ASTM C136使用改进的普罗克特压实试验和筛分分析进行了实验室分析。这有助于建立水文土壤图,而土地利用图则是利用Landsat 7ETM+影像波段2、3、4 [30 m]与PAN波段8 [15 m]合并进行分类。利用最大似然分类器的监督分类方法编制了地理覆盖面积为442平方公里的Varekhadi集水区的土地利用图。2001年11月10日Landsat 7ETM+图像分类的主要土地利用类别为农业(32%)、森林(29%)、荒地(20%)、休耕地(14%)、建筑(4%)和水体(2%)。GIS环境下产生的水文土壤类群确定了研究区内存在的B类和C类土壤类群。Varekhadi集水区已划分为五个流域,即Amli, Zankhwaw, Visdaliya, Godsambha和Wareli,使用DEM和河流网络划定。采用SCS-CN模型估算各子流域日径流量。洪水潜力分析结果表明,瓦勒里流域洪水潜力最大,阿姆里流域洪水潜力最小。需要注意的是,洪水潜势值最高的区域位于流域最低处,人口密度较高。这一分析反映了瓦勒里流域遭受洪水和淹没的脆弱性和风险的增加。用2010年一个常见事件的流量测量数据对结果进行了验证,结果与模型拟合良好。塔皮流域下游支流的洪水潜力分析表明,利用遥感和GIS数据获得水文参数的SCS-CN方法可以应用于预测测量不足的流域的径流
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of the Flood Potential on a Lower Tapi Basin Tributary usingSCS-CN Method integrated with Remote Sensing & GIS data
The purpose of this research paper is to identify watersheds with high flood potential based on watershed characteristics for formation of surface runoff. The SCS-CN method relies on remote sensing and GIS data for obtaining watershed characteristics. A 30 m raster grid size digital elevation model (DEM) has been generated from field survey using Global Positioning System (GPS) of 3 m accuracy integrating with Survey of India topographical maps of 1: 50,000 scale having 10 m contour interval. The undisturbed soil samples from field have been collected and laboratory analysis was carried out using modified proctor compaction test as per ASTM D1557 and sieve analysis as per ASTM C136. This has helped in establishing hydrological soil map while land use map has been prepared using Landsat 7ETM+ image band 2, 3, 4 [30 m] merged with PAN band 8 [15 m] for classification. The supervised classification approach using maximum likelihood classifier has been employed for preparation of land use map for Varekhadi catchment having 442 km2 of geographical coverage. The major land use categories classified on 10 Nov 2001 Landsat 7ETM+ image have been agriculture (32%), forest (29%), wasteland (20%), fallow land (14%), built-up (4%) and water bodies (2%). The hydrological soil groups generated in GIS environment have identified two soil groups viz. group B and group C that exist under study area. The Varekhadi catchment has been delineated into five watersheds viz. Amli, Zankhwaw, Visdaliya, Godsambha and Wareli delineated using DEM and stream network. The SCS-CN model was applied for estimating of daily run-off for each sub-watershed. The results obtained on the flood potential analysis shows that Wareli watershed has highest flood potential while the Amli watershed lowest. It should be noted that highest value of flood potential belongs to lowest part of watershed, where high population density can be found. This analysis reflects an increased vulnerability and risks to floods and inundations for Wareli watershed. Stream gauge data has been used for result validation with a common event of 2010 and it shows good fit with the model. The flood potential analysis within the lower Tapi basin tributary suggests that the SCS-CN method with hydrological parameters derived using remote sensing and GIS data can be applied to predict run-off in poorly gauged watersheds
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