Numerical Simulation of Sedimentary Dynamics to Estuarine Bar under the Coupled Fluvial - Tidal Control

被引:4
|
作者
Liu X. [1 ,2 ]
Lu S. [2 ]
Tang M. [2 ]
Sun D. [2 ]
Tang J. [1 ,2 ]
Zhang K. [3 ]
He T. [2 ]
Qi N. [1 ,2 ]
Lu M. [2 ]
机构
[1] Key Laboratory of Deep Oil and Gas, China University of Petroleum, Qingdao
[2] School of Geosciences, China University of Petroleum, Qingdao
[3] PetroChina Research Institute of Petroleum Exploration and Development, Beijing
关键词
Estuary; Geological prospecting; Interlayer; Numerical simulation; Sedimentary dynamics; Tidal bar; Tide;
D O I
10.3799/dqkx.2020.305
中图分类号
学科分类号
摘要
The complex sedimentary characteristics and internal structure of the tidal-controlled estuary dam are still unclear. By means of establishment of an ideal tidal-controlled estuary model, using sedimentary dynamics numerical simulation method, quantitative simulation of sedimentation of tidal-controlled estuary dam and internal interlayer was carried out under different flow and tidal energy conditions. The results show that under ideal conditions, large tidal range and medium flow are conducive to large-scale development of tidal-controlled estuary bars. In the analysis of tidal energy factors, the length-to-width ratio of the tidal-controlled estuary dam is 2-15, the length of the interlayer is concentrated at 8 km, and the thickness of the interlayer is 0.1-0.2 m. In the analysis of flow factors, the length-to-width ratio of the tidal-controlled estuary dam body is 1.5-9.0, the interlayer length is 1-2 km, and the interlayer thickness is 0.1-0.2 m. Simulation results show that the coupled action of the river and tide control the formation and distribution of the bar, but the effect of the tide is more remarkable. Numerical simulation of the sedimentary process of tidal-controlled estuaries based on sedimentary dynamics has been verified by well seismic data, which will provide new ideas for the sedimentary evolution of tidal-controlled estuaries and will guide the exploration and development of oil-bearing reservoirs in the tidal-controlled estuary. © 2021, Editorial Department of Earth Science. All right reserved.
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页码:2944 / 2957
页数:13
相关论文
共 42 条
  • [11] Geleynse N., Storms J. E. A., Walstra D. J. R., Et al., Controls on River Delta Formation
  • [12] Insights from Numerical Modelling, Earth and Planetary Science Letters, 302, 1-2, pp. 217-226, (2011)
  • [13] Guezennec L., Lafite R., Dupont J. P., Et al., Hydrodynamics of Suspended Particulate Matter in the Tidal Freshwater Zone of a Macrotidal Estuary (the Seine Estuary, France), Estuaries, 22, 3, pp. 717-727, (1999)
  • [14] Jimenez Robles A. M., Ortega-Sanchez M., Implications of River Discharge Angle and Basin Slope on Mouth Bar Morphology and Discharge Dynamics of Stable Jets, Journal of Hydraulic Engineering, 144, 9, (2018)
  • [15] Kilaru S., Goud B. K., Rao V. K., Crustal Structure of the Western Indian Shield: Model Based on Regional Gravity and Magnetic Data, Geoscience Frontiers, 4, 6, pp. 717-728, (2013)
  • [16] Lesser G. R., Roelvink J. A., van Kester J. A. T. M., Et al., Development and Validation of a Three-Dimensional Morphological Model, Coastal Engineering, 51, 8-9, pp. 883-915, (2004)
  • [17] Leuven J. R. F. W., Braat L., van Dijk W. M., Et al., Growing Forced Bars Determine Nonideal Estuary Planform, Journal of Geophysical Research: Earth Surface, 123, 11, pp. 2971-2992, (2018)
  • [18] Leuven J. R. F. W., Kleinhans M. G., Weisscher S. A. H., Et al., Tidal Sand Bar Dimensions and Shapes in Estuaries, Earth-Science Reviews, 161, pp. 204-223, (2016)
  • [19] Martinius A. W., Fustic M., Garner D. L., Et al., Reservoir Characterization and Multiscale Heterogeneity Modeling of Inclined Heterolithic Strata for Bitumen-Production Forecasting, McMurray Formation, Corner, Alberta, Canada, Marine and Petroleum Geology, 82, pp. 336-361, (2017)
  • [20] Nardin W., Fagherazzi S., The Effect of Wind Waves on the Development of River Mouth Bars, Geophysical Research Letters, 39, 12, (2012)