Palaeochannels 是 unconsolidated 沉积或在古老的、当前不活跃的河和流隧道系统里扔的巩固半的沉积岩石的存款。它从当前活跃的河隧道的 overbank 存款是不同的,包括定期不流动的短暂的水功课。我们介绍了一光谱从有特殊时间阶段的 SPOT-5 形象的基于特征的 palaeochannel 信息抽取模型,它被遥感机制的分析的优点造了并且光谱 palaeochannel 的特征,从空间分发与它的区别结合了并且光谱当前活跃的河隧道的特征,另外,随遥感判定的建立,在遥感的 palaeochannel 的特征想象。这个模型跟随监督分类的进程[箭头权利] 掩盖的农田和主要部件分析[箭头权利] 地下的 palaeochannel 信息抽取[箭头权利] 信息联合[箭头权利] palaeochannel 系统图象。在乔胡·莱克的东方的 Zhegao 河山谷作为一个学习区域被选择,并且 SPOT-5 形象被用作数据的来源。当这个方法成功地被使用了提取 palaeochannel 信息时,结果是令人满意的,它能为地区性的遥感考古学和 neotectonic 研究提供好参考。然而,这个方法的适用性需要作为空间特征在另外的区域进一步被测试并且光谱 palaeochannel 的反应可能是不同的[出版摘要]
Palaeochannels are deposits of unconsolidated sediments or semi-consolidated sedimentary rocks depos- ited in ancient, currently inactive river and stream channel systems. It is distinct from the overbank deposits of currently active river channels, including ephemeral water courses which do not regularly flow. We have introduced a spectral characteristics-based palaeochannel information extraction model from SPOT-5 imagery with special time phase, which has been built by virtue of an analysis of remote sensing mechanism and spectral characteristics of the palaeochannel, combined with its distinction from the spatial distribution and spectral features of currently active river channels, also with the establishment of remote sensing judging features of the palaeochannel in remote sensing image. This model follows the process of supervised classification → farmland masking and primary component analysis→ underground palaeochan- nel information extraction → information combination→ palaeochannel system image. The Zhegao River Valley in the east of Chaohu Lake was selected as a study area, and SPOT-5 imagery was used as a source of data. The result was satisfactory when this method has been successfully applied to extract the palaeochannel informa- tion, which can provide good reference for regional remote sensing archeology and neotectonic research. However, the applicability of this method needs to be tested further in other areas as the spatial characteristics and spectral response of palaeochannel might be different.