|Table of Contents|

Geomorphic Development Characteristics andEvolution Process in Luo River Basin, Loess Plateau, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2024年第02期
Page:
154-168
Research Field:
环境与可持续发展
Publishing date:

Info

Title:
Geomorphic Development Characteristics andEvolution Process in Luo River Basin, Loess Plateau, China
Author(s):
ZHANG Tian-yu1; 2; 3;  LIU Fan2; 3;  HONG Zeng-lin1; 3;  DENG Ya-hong2; 3
(1. Shaanxi Institute of Geological Survey, Xi'an 710068, Shaanxi, China; 2. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Key Laboratory of Mine Geological Hazards Mechanism and Control of Ministry of Natural Resources, Xi'an 710054, Shaanxi, China)
Keywords:
loess landform;  geomorphic differentiation;  geomorphic evolution;  geomorphic pattern;  quantitative analysis;  geomorphic factor;  principal component analysis;  Luo River Basin
PACS:
P931.6
DOI:
10.19814/j.jese.2023.11006
Abstract:
The morphological characteristics, developmental mechanism and evolutionary process of loess landform always have been the focus and frontier of geoscience research. 14 geomorphic factors were selected from slope scale, basin scale and regional scale to construct a comprehensive quantitative parameter system for characterizing the landform development in Luo River Basin, and the factor values and interpolation maps were obtained from 646 small watershed units. Through principal component analysis(PCA), four mainfactors were obtained, and reflected four spatial patterns of geomorphic morphological, including south-north gradient type, single-center diffusion type, east-west transitional type, and multi-center diffusion type. Combined with geomorphic types and development degree, it is indicated that the characteristics of loess geomorphic relief and vertical erosion reflect the overall geomorphic spatial pattern in Luo River Basin.Under multi-factor influence, the loess geomorphology of Luo River Basin has been continuously headwarderoded and expanded downward with water system developed from downstream to upstream, and finally formed the present morphologicalspatialdifferentiation pattern.

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