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Journal of Desert Research ›› 2026, Vol. 46 ›› Issue (2): 53-62.DOI: 10.7522/j.issn.1000-694X.2025.00128

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Formation and evolution of granule ripples on an artificial flattening surface

Yuxuan Meng1,2(), Guangqiang Qian1, Zhuanling Yang3, Xuegang Xing3, Kaijia Pan1,2, Youyuan Guo1   

  1. 1.State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
    2.University of Chinese Academy of Sciences,Beijing 100049,China
    3.School of Geography and Resources,Guizhou Education University,Guiyang 550018,China
  • Received:2025-05-29 Revised:2025-07-23 Online:2026-03-20 Published:2026-04-13

Abstract:

Granule ripples are aeolian landforms composed of bimodal grain-sized sediments and are widely distributed on Earth and Mars. Since previous studies have not correlated the evolution process of granule ripples with dynamic forces, in order to explore the relationship between morphological evolution and dynamics, this study flattened a typical granule ripple area in the Sanlongsha region. Through in-situ field observation of its evolution process, three-dimensional topographic data were obtained, and the relationships among morphological changes, movement patterns, and wind conditions were analyzed. The results show that 91 granule ripples were formed in the early stage of evolution, with an average length of 1.09 m and an average height of 0.06 m. After the fusion of granule ripples with different movement speeds, the number decreased, the length increased, the overall movement speed slowed down, and the spacing increased. They returned to a mature state in about nine months. Subsequently, gale weather caused the granule ripples to decompose. The number increased to four times the original, the length shrank to 1/4 of the original, the number of ridge lines further increased, and the granule ripples underwent processes of fracture, re-formation, and then re-merging. Through in-situ observation, this study makes up for the deficiencies of previous studies due to equipment and technical limitations. It reveals the formation and evolution process of granule ripples on flat surfaces, which is of great significance for in-depth understanding of their dynamic processes. At the same time, it also provides important references for understanding aeolian landforms such as giant ripples and transverse sand ridges on Mars.

Key words: granule ripple, formation and evolution, morphological parameters, movement velocity, wind conditions

CLC Number: