Positive and negative terrains on northern Shaanxi Loess Plateau

被引:85
作者
Zhou Yi [1 ]
Tang Guo'an [1 ]
Yang Xin [1 ]
Xiao Chenchao [2 ]
Zhang Yuan [3 ]
Luo Mingliang [4 ]
机构
[1] Nanjing Normal Univ, Minist Educ, Key Lab Virtual Geog Environm, Nanjing 210046, Peoples R China
[2] Peking Univ, Inst RS & GIS, Beijing 100871, Peoples R China
[3] Cent S Univ, Sch Foreign Languages, Changsha 410083, Peoples R China
[4] China W Normal Univ, Coll Land & Resources, Nanchong 637002, Sichuan, Peoples R China
基金
中国国家自然科学基金;
关键词
Loess Plateau; positive and negative terrains; DEM; shoulder-lines; spatial differentiation; SOIL;
D O I
10.1007/s11442-010-0064-6
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
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.
引用
收藏
页码:64 / 76
页数:13
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