水下流体力学对亚马逊河口油气井喷的影响

H. L. Varona, M. Silva, D. Veleda, F. S. Leite, M. Moura, M. Araújo
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引用次数: 5

摘要

这项研究的重点是分析位于巴西北部大陆架的井喷进入深水的石油/天然气羽流的行为。采用区域海洋模拟系统(ROMS)模式模拟了60.5°-24.0°W/5°S-16°N区域的海洋动力学,分辨率为0.25°,垂直高度为32,考虑了亚马逊河和帕尔河的流量。将ROMS输出与简单海洋数据同化(SODA)数据集进行比较。选取(50°W, 5.25°N)、(44.5°W, 0.5°N)和(42.75°W, 1°S) 3个点进行数值模拟。Lee和Cheung(1990)建议的时间步长由于各点的特殊海洋学条件进行了调整,其中初速度趋于零,将原方程的系数0.1替换为0.0250和0.0375。所有的羽流都表现为3型。从底部到表面的季节流速度较小,通常不超过0.25 ms-1;羽流从其起源点的最大位移不大于1m。地表平均羽流直径为54 ~ 79.7 m,到达地表的时间为7.25 ~ 8.05 h。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Influence of underwater hydrodynamics on oil and gas blowouts off Amazon River Mouth
This study is focused on analyzing the behavior of oil/gas plumes from blowouts into deepwater, located at the northern Brazil continental shelf. The Regional Ocean Modeling System (ROMS) model is used to simulate ocean dynamics in the region 60.5°-24.0°W/5°S-16°N with 0.25° of resolution, 32 vertical levels and considering the discharges of the Amazon and Pará Rivers. The ROMS output are compared to Simple Ocean Data Assimilation (SODA) dataset. Three points were selected to make the numerical simulations, located at (50°W, 5.25°N), (44.5°W, 0.5°N) and (42.75°W, 1°S). The time step suggested by Lee and Cheung (1990) was adjusted due to the particular oceanographic conditions at each point, in which, the initial velocity tends to zero and the coefficient 0.1 of the original equation was replaced by 0.0250 and 0.0375. All the plumes behaved as type 3. The seasonal current speed was small from the bottom to the surface, usually not exceeding 0.25 ms-1; the maximum displacement of the plumes from its point of origin was not greater than 1 m. The mean plumes diameter on the surface ranged 54 - 79.7 m and the arrival time to the surface was from 7.25 to 8.05 hours.
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