Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China

• Published in: Chinese geographical science Vol. 28; no. 4; pp. 624 - 635
• Main Authors: Du, Huishi, Wang, Zongming, Mao, Dehua
• Format: Journal Article
• Language: English
• Published: Heidelberg Science Press 01.08.2018; Springer Nature B.V; College of Tourism and Geographical Science, Jilin Normal University, Siping 136000, China; Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China%Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China
• Subjects: Dunes; Earth and Environmental Science; Fluvial morphology; Geography; Geomorphology; Morphology; Rivers; China; fluvial-aeolian interaction; sand dune pattern; Horqin Sandy Land; landscape evolution; riverine dune
• ISSN: 1002-0063; 1993-064X
• DOI: 10.1007/s11769-018-0951-9

The interaction between fluvial and aeolian processes can significantly change surface morphology of the Earth. Taking the Horqin Sandy Land as the research area and using Landsat series satellite remote sensing images, this study utilizes geomorphology and landscape ecology to monitor and analyze the aeolian geomorphology characteristics of the Horqin Sandy Land. Results show that the sand dunes of the Horqin Sandy Land are mainly distributed on alluvial plains along the banks of the mainstream and tributaries of the Western Liao River, and the sand dune types tend to simplify from west to east and from south to north. The aeolian geomorphology coverage tend to be decreasing in the past 40 years, with an average annual change rate of 0.31%. While the area of traveling dunes decreased, the area of fixed and semi-fixed dunes increased. The fractal dimensions of various types of sand dune have all remained relatively constant between 1.07 and 1.10, suggesting that they are experiencing a relatively stable evolutionary process. There is a complex interaction between fluvial and aeolian processes of the Horqin Sandy Land, which plays a central role in surface landscape molding. Sand dunes on both sides of different rivers on the Horqin Sandy Land present certain regularity and different characteristics in terms of morphology, developmental scale, and spatial pattern. There are six fluvial-aeolian interaction modes in this area: supply of sand sources by rivers for sand dune development, complete obstruction of dune migration by rivers, partial obstruction of dune migration by rivers, influence of river valleys on dune developmental types on both sides, influence of river valleys on dune developmental scale on both sides, and river diversion due to obstruction and forcing by sand dunes. This study deepens our understanding of the surface process mechanism of the interaction between fluvial and aeolian processes in semi-arid regions, and provides a basis for researches on regional landscape responses in the context of global environmental change.