罗玉沟流域侵蚀沟视觉解译及空间分布格局研究

Wenyin Zhang, Yinfeng Liu
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引用次数: 4

摘要

黄土高原沟壑纵横,侵蚀沟壑生长较好。黄土材料疏松,具有垂直节理,易受侵蚀;该地区的侵蚀类型主要有重力侵蚀和海沟侵蚀。天水北郊罗玉沟流域位于陇西黄土高原丘陵沟壑区与陇南山区的相互作用区域,存在典型的鸥蚀现象。在2008年SPOT卫星照片和野外调查的支持下,建立侵蚀沟的视觉判读特征,提取侵蚀沟信息,并运用景观格局分析方法,研究流域侵蚀沟的空间分布格局。结果表明:1)侵蚀沟槽形态呈条状或乔木状,在黑白图像中,稳定侵蚀沟槽呈现深深色,活跃侵蚀沟槽呈现亮色,半活跃侵蚀沟槽呈现浅深色;而在彩色合成图像中,稳定侵蚀沟的颜色混合石榴红色,其他侵蚀沟的颜色为亮绿色。2)研究区人类活动频繁发生的侵蚀沟较多,如梯田两侧、道路两侧和河流沼泽地,梯田两侧均有侵蚀沟。3)研究流域侵蚀沟以稳定侵蚀沟为主,占侵蚀沟总面积的51.3%,半活跃侵蚀沟占18.3%。这一现象标志着该盆地冲蚀沟的治理取得了进展。4)研究流域从上游到下游,侵蚀沟的平均形状指数有逐渐减小的趋势,说明越靠近下游,侵蚀沟的坡度越平缓。数据结果与实际地形特征吻合较好。
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Research on Visual Interpretation and Spatial Distribution Pattern of the Erosion Gully in Luoyugou Watershed of China
There are criss-cross Ravines and gullies in the Loess Plateau, where the erosion gullies grows better. The loess material, which is loose and has the vertical jointing, is easy to suffer from the erosion; the types of erosion in this area mainly include gravitational erosion and the trench erosion. There are typical gulling erosion in Luoyugou watershed of Tianshui northern suburb, located in the interactive region of Longxi Loess plateau hill-gully area and the Longnan mountainous area. Under the support of the SPOT satellite photos in 2008 and field survey, the paper establishes the visual interpretation features of erosion gully, extracting the information of erosion gully, and uses the landscape pattern analytical method, studying the spatial distribution pattern of the erosion gully in the watershed. Finally, the paper draws the following conclusions: 1) The shapes of erosion gullies are strip or arborization, and in the black-white image, the stable erosion gullies appear deep dark color, active erosion gullies present the bright color, and half-active erosion gullies are the shallow dark color; while in color synthesis image, the color of stable erosion gullies mixes garnet, and other erosion gullies are bright green. 2) There are more erosion gullies in the study area where human activities occur frequently, such as the both sides of terraced field, the side of road and the river marshland, the both sides of terraced field have. 3) The erosion gullies in the study watershed are primarily stable ones, whose area accounts for 51.3% of the total erosion gullies, and half-active ones accounts for 18.3%. This phenomenon indicates the progress in the control of the erosion gullies in this basin. 4) From the upstream to the downstream in the research basin, the erosion gully's average shape index has the tendency to reduce gradually, illustrating that the more getting nearly to the downstream, the more the slope of erosion gully to be gentler. The data results match well with the actual terrain feature.
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