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Modeling deepwater oil/gas blowouts with hydrate formation and decomposition.

机译:利用水合物的形成和分解来模拟深水油气井喷。

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摘要

When gas is spilled in deepwater, the high pressure and low temperature can convert the gases into hydrates. The hydrates formed from natural gases are buoyant. As these hydrates travel upwards they will encounter regions of lower pressure. The hydrates can decompose into free gas under these conditions. The presence or absence of hydrates has a significant impact on the behavior of the jet/plume due to the alteration of the buoyancy. The free gas may dissolve in water.; This thesis describes a computer model developed to simulate the behavior of oil and gas released from deepwater locations in the ocean. The model integrates the hydrodynamics of the jet/plume, thermodynamics of the jet/plume, thermodynamics and kinetics of hydrate formation and decomposition, dissolution of gases. The possibility of gas separation from the main plume is modeled.; An integrated formulation to calculate the buoyant velocity of bubbles/droplets of various sizes and shapes developed by Zheng and Yapa (2000) is used. This formulation can be applied to solids, liquid, or gases. An improved method from Zheng and Yapa (2002) is used to compute dissolution from gas bubbles in ultra-deep water plumes, where the non-ideal nature of gasses under high pressures is taken into account. Both methods (Zheng and Yapa, 2000, 2002) account for non-spherical shapes of gas bubbles, and the computed results show a good match compared with previously conducted lab experiments.; The comprehensive model is used to simulate the Deepspill experiments. The simulations compare well with Echo sounder data from the Deepspill experiments for both vertical profiles and the Bird's eye view. A series of parametric analysis is made to show the effect on the behavior of the jet/plume due to variations in key input parameters. Scenario simulations are presented to show the behavior of oil/gas under different deepwater conditions.
机译:当气体泄漏到深水中时,高压和低温会将气体转化为水合物。由天然气形成的水合物是漂浮的。随着这些水合物向上传播,它们将遇到低压区域。在这些条件下,水合物可分解成游离气体。由于浮力的改变,水合物的存在或不存在对射流/柱塞的行为有重大影响。游离气体可溶于水。本文描述了一种计算机模型,该模型被开发为模拟从海洋深水位置释放的石油和天然气的行为。该模型综合了射流/泥浆的流体力学,射流/泥浆的热力学,水合物形成和分解,气体溶解的热力学和动力学。模拟了从主羽流中分离出气体的可能性。使用一个综合公式来计算由Zheng和Yapa(2000)开发的各种大小和形状的气泡/液滴的浮力速度。该制剂可以应用于固体,液体或气体。 Zheng and Yapa(2002)的一种改进方法用于计算超深水羽流中气泡的溶解,其中考虑了高压下气体的非理想特性。两种方法(Zheng和Yapa,2000,2002)都说明了气泡的非球形形状,与先前进行的实验室实验相比,计算结果显示出良好的匹配性。综合模型用于模拟Deepspill实验。对于垂直剖面和鸟瞰图,该模拟与Deepspill实验中的回声测深仪数据进行了很好的比较。进行了一系列参数分析,以显示由于关键输入参数的变化而对射流/柱塞行为的影响。提出了场景模拟,以显示不同深水条件下的油气行为。

著录项

  • 作者

    Chen, Fanghui.;

  • 作者单位

    Clarkson University.;

  • 授予单位 Clarkson University.;
  • 学科 Engineering Civil.; Engineering Environmental.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 177 p.
  • 总页数 177
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 建筑科学;环境污染及其防治;
  • 关键词

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