陕北黄土高原正负地形研究(英文)

被引:28
作者
周毅 [1 ]
汤国安 [1 ]
杨昕 [1 ]
肖晨超 [2 ]
张媛 [3 ]
罗明良 [4 ]
机构
[1] Key Laboratory of Virtual Geographic Environment of Ministry of Education,Nanjing Normal University
[2] Institute of RS and GIS,Peking University
[3] School of Foreign Languages,Central South University
[4] College of Land and Resources,China West Normal
关键词
Loess Plateau; positive and negative terrains; DEM; shoulder-lines; spatial differentiation;
D O I
暂无
中图分类号
P931.6 [黄土地貌学];
学科分类号
摘要
The Loess positive and negative terrains (P-N terrains),which are widely distrib-uted 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. Us-ing 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 de-picting 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 land-forms 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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