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陕北黄土高原正负地形研究
引用本文:周毅,汤国安,杨昕,肖晨超,张媛,罗明良. 陕北黄土高原正负地形研究[J]. 地理学报(英文版), 2010, 20(1): 64-76. DOI: 10.1007/s11442-010-0064-6
作者姓名:周毅  汤国安  杨昕  肖晨超  张媛  罗明良
作者单位: 
基金项目:国家自然科学基金重点项目,National Youth Science Foundation of China,安徽省自然科学基金
摘    要:

关 键 词:陕北黄土高原  地形地貌  空间分布规律  数字高程模型  陕西黄土高原  数字地形分析  提取方法  分类方法

Positive and negative terrains on northern Shaanxi Loess Plateau
Yi Zhou,Guo’an Tang,Xin Yang,Chenchao Xiao,Yuan Zhang,Mingliang Luo. Positive and negative terrains on northern Shaanxi Loess Plateau[J]. Journal of Geographical Sciences, 2010, 20(1): 64-76. DOI: 10.1007/s11442-010-0064-6
Authors:Yi Zhou  Guo’an Tang  Xin Yang  Chenchao Xiao  Yuan Zhang  Mingliang Luo
Affiliation:[1]Key Laboratory of Virtual Geographic Environment of Ministry of Education, Nanjing Normal University Nanjing 210046, China [2]Institute of RS and GIS, Peking University, Beijing 100871, China [3]School of Foreign Languages, Central South University, Changsha 410083, China [4]College of Land and Resources, China West Normal University, Nanchong 637002, Sichuan, China
Abstract:The Loess positive and negative terrains (P-N terrains), which are widely distributed on the Loess Plateau, are discussed for the first time by introducing its characteristic, demarcation as well as extraction method from high-resolution Digital Elevation Models. Using 5 m-resolution DEMs as original test data, P-N terrains of 48 geomorphological units in different parts of Shaanxi Loess Plateau are extracted accurately. Then six indicators for depicting the geomorphologic landscape and spatial configuration characteristic of P-N terrains are proposed. The spatial distribution rules of these indicators and the relationship between the P-N terrains and Loess relief are discussed for further understanding of Loess landforms. Finally, with the integration of P-N terrains and traditional terrain indices, a series of un-supervised classification methods are applied to make a proper landform classification in northern Shaanxi. Results show that P-N terrains are an effect clue to reveal energy and substance distribution rules on the Loess Plateau. A continuous change of P-N terrains from south to north in Shaanxi Loess Plateau shows an obvious spatial difference of Loess landforms and the positive terrain area only accounted for 60.5% in this region. The P-N terrains participant landform classification method increases validity of the result, especially in the Loess tableland, Loess tableland-ridge and the Loess low-hill area. This research is significant on the study of Loess landforms with the Digital Terrains Analysis methods.
Keywords:Loess Plateau  positive and negative terrains  DEM  shoulder-lines  spatial differentiation
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