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Geomorphologic study of Anhui section of Changjiang River using Landsat TM image

机译:基于Landsat TM影像的长江安徽段地貌研究。

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Fluvial landforms in the Anhui section of the Changjiang (Yangtze) River are often considered as the main factors for frequent floods. It is these special landforms that influence the channel changes of the Changjiang River. Using Landsat TM image of 2000, this paper conducted a series of image processing, including principal component analysis, multi-spectral composition, gray value statistics, and spectral analysis of ground objects. Then it got a new interpretation map of different kinds of fluvial landforms of the Changjiang River in the Anhui section. Based on the interpretation mentioned above, the paper analyzes the distribution and characteristics of such typical landforms as terraces, floodplains and battures, and their functions on the changes of river channel. The results show a consistence with the earlier conclusion that the Anhui section of the Changjiang River tends to deflect gradually toward south, which provides more implications for further study on the geomorphologic evolution of the river channel.
机译:长江(安徽)江安徽段的河流地貌通常被认为是频繁洪水的主要因素。正是这些特殊的地貌影响了长江的河道变化。本文使用2000年的Landsat TM图像进行了一系列图像处理,包括主成分分析,多光谱成分,灰度值统计和地面物体的光谱分析。然后在安徽断面得到了长江河流不同地貌的新解释图。在上述解释的基础上,分析了梯田,洪泛区,滩涂等典型地貌的分布特征,特征及其在河道变化中的作用。研究结果与早期的结论相一致,即长江的安徽段趋向于逐渐向南偏转,这为进一步研究河道的地貌演化提供了更多的启示。

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