Research article

Formation and ecological response of sand patches in the protection system of Shapotou section of the Baotou-Lanzhou railway, China

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  • 1Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
    2University of Chinese Academy of Sciences, Beijing 100049, China
    3College of Urban and Environmental Sciences, Northwest University, Xi'an 710100, China
    4Zhongwei Works Section of China Railway Lanzhou Bureau Group Company Limited, Zhongwei 755000, China

Received date: 2023-08-31

  Revised date: 2024-01-12

  Accepted date: 2024-01-23

  Online published: 2024-02-29

Abstract

The development of bare patches typically signifies a process of ecosystem degradation. Within the protection system of Shapotou section of the Baotou-Lanzhou railway, the extensive emergence of bare sand patches poses a threat to both stability and sustainability. However, there is limited knowledge regarding the morphology, dynamic changes, and ecological responses associated with these sand patches. Therefore, we analyzed the formation and development process of sand patches within the protection system and its effects on herbaceous vegetation growth and soil nutrients through field observation, survey, and indoor analysis methods. The results showed that sand patch development can be divided into three stages, i.e., formation, expansion, and stabilization, which correspond to the initial, actively developing, and semi-fixed sand patches, respectively. The average dimensions of all sand patch erosional areas were found to be 7.72 m in length, 3.91 m in width, and 0.32 m in depth. The actively developing sand patches were the largest, and the initial sand patches were the smallest. Throughout the stage of formation and expansion, the herbaceous community composition changed, and the plant density decreased by more than 50.95%. Moreover, the coverage and height of herbaceous plants decreased in the erosional area and slightly increased in the depositional lobe; and the fine particles and nutrients of soils in the erosional area and depositional lobe showed a decreasing trend. In the stabilization phases of sand patches, the area from the inlet to the bottom of sand patches becomes initially covered with crusts. Vegetation and 0-2 cm surface soil condition improved in the erosional area, but this improvement was not yet evident in the depositional lobe. Factors such as disturbance, climate change, and surface resistance to erosion exert notable influences on the formation and dynamics of sand patches. The results can provide evidence for the future treatment of sand patches and the management of the protection system of Shapotou section of the Baotou-Lanzhou railway.

Cite this article

DUN Yaoquan, QU Jianjun, KANG Wenyan, LI Minlan, LIU Bin, WANG Tao, SHAO Mei . Formation and ecological response of sand patches in the protection system of Shapotou section of the Baotou-Lanzhou railway, China[J]. Journal of Arid Land, 2024 , 16(2) : 298 -313 . DOI: 10.1007/s40333-024-0006-2

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