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Research on OBN secondary location method in shallow water environment
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ZhongCheng WANG1, 2, DaMing GE1, Ning QIN1, *, PeiTi LIU1, JingGe WANG1
Progress in Geophysics | 2026, 41(1) : 481 - 490
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Progress in Geophysics | 2026, 41(1): 481-490
Research on OBN secondary location method in shallow water environment
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ZhongCheng WANG1, 2, DaMing GE1, Ning QIN1, *, PeiTi LIU1, JingGe WANG1
Affiliations
  • 1Geophysical Research Institute, SINOPEC Shengli Oilfield Company, Dongying 257022, China
  • 2Working Station for Postdoctoral Scientific Research, Shengli Oilfield, Dongying 257000, China
Published: 2026-02-20 doi: 10.6038/pg2026JJ0058
Outline
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Accurate observation system information is the foundation of high-precision seismic data processing. Due to the inability to use conventional GPS positioning for OBN receiver points, specialized technical means are usually required to determine the coordinates of the receiver points. Common secondary positioning methods for receiver points include least squares method, approximate tetrahedron method, search method, fitting surface method, equivalent velocity method, vector synthesis method, etc. However, they are all based on direct wave travel time for positioning. Shallow water OBN data only has direct waves within a small offset distance, making those methods difficult to apply. Another commonly used secondary positioning method is refracted wave secondary positioning, which has low positioning accuracy due to its inability to handle speed gradients, interface bending, and other situations. In response to the problem of inaccurate positioning of receiver points in shallow water environments, this paper proposes a positioning method based on first arrival travel time fitting. Firstly, the first arrival time is accurately picked up from the common receiver point gather. Then, a polynomial is used to fit the relationship curve between the first arrival time and offset. The coordinates of the receiver points are adjusted by the difference between the actual picked travel time and the corresponding value on the curve, and multiple iterations are carried out until convergence. Finally, based on the water depth values measured in the survey, the corresponding Z coordinates can be obtained by projecting the X and Y coordinates of the receiver points, thus obtaining accurate three-dimensional coordinates of the receiver points. The method proposed in this article has been applied to both simulated and actual OBN data, achieving ideal results.

OBN  /  Common receiver point  /  First-arrival travel time  /  Secondary positioning
王忠成, 葛大明, 秦宁, 刘培体, 王敬阁. 浅水环境OBN二次定位方法研究. 地球物理学进展, 2026 , 41 (1) : 481 -490 . DOI: 10.6038/pg2026JJ0058
ZhongCheng WANG, DaMing GE, Ning QIN, PeiTi LIU, JingGe WANG. Research on OBN secondary location method in shallow water environment[J]. Progress in Geophysics, 2026 , 41 (1) : 481 -490 . DOI: 10.6038/pg2026JJ0058
Year 2026 volume 41 Issue 1
153
66
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Article Info
doi: 10.6038/pg2026JJ0058
  • Receive Date:2025-04-30
  • Online Date:2026-09-23
  • Published:2026-02-20
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  • Received:2025-04-30
  • Revised:2025-11-05
Affiliations
    1Geophysical Research Institute, SINOPEC Shengli Oilfield Company, Dongying 257022, China
    2Working Station for Postdoctoral Scientific Research, Shengli Oilfield, Dongying 257000, China
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表12种不同金属材料的力学参数
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Family
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Number of
genus
种数
Number of
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Number of
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Percentage of total
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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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