Advances in Earth Science ›› 2025, Vol. 40 ›› Issue (8): 821-830. doi: 10.11867/j.issn.1001-8166.2025.054

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Optimization Sampling Schemes for Monitoring Land Gravelization in Desert Areas of Inner Mongolia

Hao PEI1(), Hu YE2(), Yanfeng JIANG3, Chengzhen JIA3, Lei FAN4, Kun ZHANG4, Lina XU2, Bailing MIAO3   

  1. 1. Inner Mongolia Meteorological Service, Hohhot 010051, China
    2. Inner Mongolia Meteorological Service Center, Hohhot 010051, China
    3. Institute of Meteorological Science of Inner Mongolia, Hohhot 010051, China
    4. College of Ecology and Environment, Inner Mongolia University, Hohhot 010030, China
  • Received:2025-07-17 Revised:2025-07-31 Online:2025-08-10 Published:2025-10-20
  • Contact: Hu YE
  • Supported by:
    the National Natural Science Foundation of China(32271656); The Central Guidance for Local Scientific and Technological Development Funding Projects(2024ZY0165); The Science and Technology Innovation Project of Inner Mongolia Meteorological Bureau(nmqxkjcx202458)

Hao PEI, Hu YE, Yanfeng JIANG, Chengzhen JIA, Lei FAN, Kun ZHANG, Lina XU, Bailing MIAO. Optimization Sampling Schemes for Monitoring Land Gravelization in Desert Areas of Inner Mongolia[J]. Advances in Earth Science, 2025, 40(8): 821-830.

To improve the accuracy of monitoring land gravelization and the efficiency of fieldwork, and further promote the innovation of monitoring methods, a study on the appropriate size and quantity of quadrats was conducted. This study examines the desert region of Inner Mongolia and uses the entropy TOPSIS and Wilcoxon rank sum test methods to determine the optimum sampling scheme for land gravelization monitoring. Based on results using 100 cm×100 cm quadrats as the true values of gravel coverage and surface gravel mass per unit area, new survey areas in the desert regions of Inner Mongolia were selected, and the maximum quadrat was expanded to 200 cm×200 cm to increase the sampling areas and number of quadrats, and optimize the sampling scheme for monitoring land gravelization. The comparative results of the two experiments show that: Q25 exhibits good advantages for monitoring suitability, which can improve field work efficiency while ensuring measurement accuracy; the appropriate quantity and sizing of quadrats vary significantly with changes in the maximum quadrat size; however, for Q25, the change in appropriate quantity (from 9 to 10) is non-significant, indicating good stability; using Q25, the appropriate coverage for monitoring gravelization is consistent with the results from monitoring surface gravel mass per unit area; this not only simplifies the monitoring process, but also ensures the reliability and comparability of monitoring data.

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