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陕北黄土高原正负地形研究(英文)
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(英文)[J].地理学报(英文版),2010,20(1):64-76.
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.
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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