基于GIS和ERS的Serligkhem河流域形态计量学分析

S. A. Chupikova, S. G. Prudnikov, A. F. Chuldum
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引用次数: 0

摘要

地理信息系统(GIS)是确定集水区结构、水资源管理和规划的有效工具。流域特征的一个重要方面是利用地理信息技术进行定量分析。利用地理信息系统(GIS)和分形几何(fractal geometry)方法,对梯瓦共和国serligi - khem河流域(Todzhinsky地区)进行了地貌特征识别和特征分析。形态计量参数的分析包括盆地的线形和面形两个方面。在GIS环境下确定的流域面积为3032.79 km2,主要为树状不对称型河网格局。平均分岔系数为3.13,表明盆地主要受构造控制。河网密度为0.34 km/km2,流域呈梨形。研究的地区主要是山区,在奥布鲁切夫院士山脊和子午线段的坡度高达40-30度。工作中进行的分形分析证实了分形维数指标值与河网线对集水区覆盖程度之间关系的假设。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Morphometric analysis of the watershed of the Serligkhem river (Tuva) using GIS ahd ERS
The Geographic Information System (GIS) serves as an effective tool for determining the structure of the catchment area, water resources management and planning. An important aspect of watershed characteristics is quantitative analysis performed using geoinformation technologies. In this study, GIS and fractal geometry methods were used to identify morphological features and analyze the properties of the Serlig-Khem River basin (Todzhinsky district), Republic of Tyva. The analysis of morphometric parameters includes both linear and areal aspects of the basin. The area of the studied catchment basin, determined in the GIS environment, is 3032.79 km2, mainly with a tree-like asymmetric type of river network pattern. The average bifurcation coefficient of 3.13 indicates that the basin is largely controlled by the structure. The density of the river network is 0.34 km/km2, the basin is pear-shaped. The territory under study has a predominantly mountainous character, with a slope of up to 40-30 degrees within the Academician Obruchev ridge and on the meridional segment. The fractal analysis carried out in the work confirms the assumption about the relationship between the value of the fractal dimension indicator and the degree of coverage of the catchment area by the lines of the river network.
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