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April 19, 2026Plants0 citationsOpen Access

Morphological Characteristics, Sediment Grain Size, and Spatial Distribution Patterns of Caragana tibetica Nabkhas in Desert Steppe

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YHYanlong HanMHMin HanYGYong Gao

Key Points

  • The study aims to investigate the relationships between nabkhas' characteristics, sediment grain size, and vegetation cover types.
  • Field investigations conducted in desert steppe
  • UAV image identification for mapping nabkhas
  • Grain size analysis of sediment composition
  • Spatial point pattern analysis to assess distribution characteristics
  • Morphological parameters of nabkhas varied with vegetation coverage
  • Surface sediments shifted from predominantly silt to fine sand in shrub-covered plots
  • Fractal dimension showed significant correlations with mean grain size and sorting
  • Spatial distribution patterns differed, with smaller clusters in higher vegetation cover plots

Abstract

Nabkhas are a common type of biogenic aeolian landform in arid and semi-arid regions. Their morphological characteristics, surface sediment grain size composition, and spatial distribution patterns can, to some extent, be associated with the interactions between vegetation and the aeolian environment. In this study, nabkhas formed around Caragana tibetica shrubs in the desert steppe of Damao Banner, Inner Mongolia, were selected as the research object. Based on field investigations, UAV image identification, grain size analysis, and spatial point pattern analysis, the characteristics of nabkhas were comparatively analyzed among a control plot without shrubs (CK) and three shrub-covered plots: a low coverage plot (LCP), a medium coverage plot (MCP), and a high coverage plot (HCP). The results showed that (1) some morphological parameters of nabkhas varied among plots with different vegetation cover, but the responses of various indicators were not entirely consistent. The MCP exhibited relatively higher values in indicators such as shrub long axis (Lg), short axis (Wg), and windward slope length (Ly). (2) The surface sediments of nabkhas were mainly composed of silt and fine sand, followed by very fine sand. Compared with the CK, the silt content was generally lower in the shrub-covered plots, whereas the contents of fine sand and very fine sand were higher. The mean grain size (Mz, Φ value) tended to decrease, while the skewness (SKG) and kurtosis (KG) tended to increase, and the sorting coefficient (σG) showed relatively limited variation. (3) In the LCP, MCP, and HCP, the fractal dimension (D) was significantly positively correlated with the Mz and σG (p < 0.05), and significantly negatively correlated with the SKG and KG (p < 0.01), suggesting that the D may be associated with variations in sediment grain size structure. (4) Overall, the nabkhas around Caragana tibetica shrubs exhibited a spatial distribution pattern characterized by aggregation at small scales and randomness at large scales, with small-scale clustering being more evident in the MCP and HCP. In general, nabkhas around Caragana tibetica shrubs under different vegetation cover conditions showed observable differences in morphological characteristics, surface sediment grain size composition, and spatial distribution patterns, providing a comparative case reference for the study of nabkhas in desert steppe areas.

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Cite This Study

Han et al. (2026) studied this question.

synapsesocial.com/papers/69e471ef010ef96374d8e1e1https://doi.org/10.3390/plants15081235
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