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Spatial-temporal Evolution Characteristics of Land Surface Subsidence and Reservoir Parameters Inversion in Sebei Gas Fields
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Yong-lian SHA1, 2, 3, Kun ZHANG1, 2, 3, Zong-ren LI1, 2, 3, *, Ya-ting WANG4, Hui-jun QI1, 2, 3, Na ZHANG1, 2, 3
Science Technology and Engineering | 2025, 25(9) : 3584 - 3592
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Science Technology and Engineering | 2025, 25(9): 3584-3592
Papers·Astronomy and Geosciences
Spatial-temporal Evolution Characteristics of Land Surface Subsidence and Reservoir Parameters Inversion in Sebei Gas Fields
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Yong-lian SHA1, 2, 3, Kun ZHANG1, 2, 3, Zong-ren LI1, 2, 3, *, Ya-ting WANG4, Hui-jun QI1, 2, 3, Na ZHANG1, 2, 3
Affiliations
  • 1 Institute of Geological Survey of Qinghai Province, Xining 810012, China
  • 2 Qinghai Remote Sensing Big Data Engineering Technology Research Center, Xining 810012, China
  • 3 The Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources Laboratory, Xining 810012, China
  • 4 31668 Troops, Xining 810012, China
Published: 2025-03-28 doi: 10.12404/j.issn.1671-1815.2403089
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Subsidence monitoring and reservoir parameters inversion in gas field can provide important supporting information for safe production protection and mining planning. The SBAS-InSAR method was used to investigate the surface subsidence evolution characteristics of Sebei gas fields from February 2022 to September 2023. Furthermore, the InSAR monitoring results were used as the observation measurements to invert the reservoir center projection coordinates, depth, strike and other parameters of the gas fields through the Prolate spheroid source. The results show that the subsidence funnel occurs in the Tainan gas field, the Sebei No.1 gas field and the Sebei No.2 gas field, and the average annual subsidence rate is -124~-109, -275~-34, and -329~-89 mm/a, respectively. Among them, the Sebei No.1 gas field and the Sebei No.2 gas field show a more significant surface subsidence phenomenon. And the surface of all three gas fields continues to sink rapidly. Further, the reservoir parameters were obtained by inversion of InSAR monitoring results. The results show that there is little difference between the deformation derived by using the optimal parameters and the observed deformation, and the spatial distribution is consistent, which indicates that it is feasible to invert the reservoir parameters of Sebei gas fields based on SBAS-InSAR deformation results.

Sebei gas fields  /  SBAS-InSAR  /  surface subsidence  /  parameters inversion
Yong-lian SHA, Kun ZHANG, Zong-ren LI, Ya-ting WANG, Hui-jun QI, Na ZHANG. Spatial-temporal Evolution Characteristics of Land Surface Subsidence and Reservoir Parameters Inversion in Sebei Gas Fields[J]. Science Technology and Engineering, 2025 , 25 (9) : 3584 -3592 . DOI: 10.12404/j.issn.1671-1815.2403089
Year 2025 volume 25 Issue 9
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doi: 10.12404/j.issn.1671-1815.2403089
  • Receive Date:2024-04-26
  • Online Date:2025-07-09
  • Published:2025-03-28
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  • Received:2024-04-26
  • Revised:2024-12-15
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Affiliations
    1 Institute of Geological Survey of Qinghai Province, Xining 810012, China
    2 Qinghai Remote Sensing Big Data Engineering Technology Research Center, Xining 810012, China
    3 The Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources Laboratory, Xining 810012, China
    4 31668 Troops, Xining 810012, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
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Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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