以Sulejów湖为例,说明了水库形成后山谷底部形态的变化

M. Jaskulski, A. Szmidt
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引用次数: 4

摘要

本文根据目前Sulejów湖区域非人工水库时期的档案资料,进行了DEM的开发。资料来源为1961年1:25 000比例尺的《行政区域图》和《苏列约夫斯基水库研究-沉积研究与深度更新》附的1:10 000文献图。这项工作的效果是创建了该地区目前不存在的数字地貌模型。在第二阶段的工作中,根据气象与水管理研究所2008年进行的回声测深研究收集的数据,建立了Sulejów湖的底部模型,包括36个剖面。然后用ESRI将这两个模型与ArcGis程序中可用的工具进行比较。分析揭示了水库建设过程和40年存在过程造成的差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Transformations in morphometry of valley bottom as a result of the creation of a reservoir illustrated with the example of Sulejów Lake
The authors have undertaken the development of DEM based on the archived materials from the time when the area of present Sulejów Lake was not an artificial water reservoir. The source materials used were Area Map of Administrative Districts in the scale of 1:25,000 from 1961 and a 1:1,000 documental map attached to the study Sulejowski Reservoir – study of sedimentation and updating of depth. The effect of this work was the creation of a Digital Geomorphological Model of the area that presently does not exist. In the second stage of works a bottom model of Sulejów Lake was made based on data gathered during echo sounding research conducted in 2008 by the Institute of Meteorology and Water Management, which comprises 36 profiles. Both models were then compared with tools available in the ArcGis program by ESRI. The analysis revealed differences resulting from processes that occurred during the construction and 40 years of existence of the reservoir.
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