Acta Geodaetica et Cartographica Sinica ›› 2025, Vol. 54 ›› Issue (5): 819-830.doi: 10.11947/j.AGCS.2025.20240449

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Simulation and verification of regional hydrological gravity effect considering undulating terrain: a case study of the head region of Three Gorges Reservoir

Mingtao ZHU1(), Yi ZHANG2, Xian MA3, Linsong WANG1,4()   

  1. 1.School of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
    2.School of Earth Science, Zhejiang University, Hangzhou 310027, China
    3.Innovation Academy for Precision Measurement Science and Technology, CAS, Wuhan 430077, China
    4.Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan 430074, China
  • Received:2024-11-01 Revised:2025-03-20 Online:2025-06-23 Published:2025-06-23
  • Contact: Linsong WANG E-mail:zhumingtao@cug.edu.cn;wanglinsong@cug.edu.cn
  • About author:ZHU Mingtao (2000—), male, PhD candidate, majors in ground precision gravity measurement and its application in geology. E-mail: zhumingtao@cug.edu.cn
  • Supported by:
    The National Natural Science Foundation of China(42274110)

Abstract:

The cutoff of the Three Gorges Dam has led to changes in the region's hydrology and even the Yangtze River basin. Most previous studies using river digital elevation and regional hydrological models focused on analyzing the gravity response of simplified water storage models and regional equivalent water heights, without considering the impact of river slopes and surrounding undulating terrain. This study constructed a water storage load model based on the river boundary of the head area of the Three Gorges Reservoir extracted by the Gaofen-1 (GF-1) satellite image. It used the Delaunay method to triangulate the complex water body surface and surrounding terrain. The regional hydrological gravity and gravity gradient effect were simulated using a high-precision polyhedron external gravity field algorithm. The research results indicate that considering the dynamic variation of water level and its impact on the slope provides a more reasonable simulation of the gravitational effects during the reservoir impoundment process. The relative error concerning absolute gravity measurements is 14%, which represents a significant improvement compared to the previous static reservoir models (with relative errors of 50% and 71% for low and high water levels, respectively). Furthermore, the regional hydrological gravity effect simulation suggests that when calculating gravity changes using global or regional hydrological models, the topography surrounding the observation points should be considered. The high-precision reservoir load modeling and forward simulation results for the Three Gorges Reservoir area presented in this paper will provide important support for long-term regional gravity monitoring, comparative analysis, and hydrological gravity correction. The findings also contribute to further exploration of the dynamic processes triggered by reservoir impoundments, such as landslides and seismic activities in the reservoir area.

Key words: the head region of Three Gorges Reservoir, hydrological load, Delaunay triangulation, time-varying gravity, undulating terrain

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