巴伦支海海上油气田设施设计依据研究

O. Gudmestad
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引用次数: 0

摘要

巴伦支海油气田的开发通常包括地面处理单元;因此,我们必须考虑到该地点可能结冰的情况。或者,可以开发较小的油田,作为现有生产单位的卫星。在可以记录管道流动状况的情况下,气田也可以考虑采用完整的井流到岸上的设施,从而避免水合物的形成。尽管历史上整个巴伦支海都存在冰川,但在南部地区遇到冰川的可能性非常低,有些人认为“可以忽略不计”。然而,由于过去的经验表明,芬马克郡海岸出现了冰川,而且与全球变暖有关的持续进程可能会增加巴伦支近海地区南部地区遇到冰山的可能性,因此,人们不确定未来在哪个纬度会出现海冰和冰川。我们将讨论与巴伦支海(包括巴伦支海的俄罗斯部分)设计基础选择相关的问题,并讨论“可忽略不计”一词。特别令人感兴趣的是与生产单元的断开选项需求相关的标准。所提出的研究的目的是提请注意设计基础的重要性,对于所有现场设施的适当设计。应认识到气候条件每年的变化,并特别强调过去的极端情况,这些极端情况不能排除将来会出现,即使在过去几十年平均气温一直在上升的北极地区也是如此。论文最后提出了为整个巴伦支海地区全面准备设计基础的建议。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on Design Basis for Barents Sea Offshore Oil and Gas Field Facilities
Development of hydrocarbon fields in the Barents Sea would normally include surface process units; thus, we must take into account the potential for ice conditions at the location. Alternatively, smaller fields can be developed as satellites to existing production units. Full well-stream to shore facilities may also be considered for gas fields, in the case that one can document the flow conditions in pipeline(s), so hydrate formation is avoided. Although glacial ice historically has been present all over the Barents Sea, the probability of meeting glacial ice in the southern part is very low, regarded by some as “negligible”. At which latitude one could expect sea and glacial ice in the future is, however, uncertain, as past experience has seen glacial ice on the Coast of Finnmark County and there are ongoing processes related to global warming which might increase the probability of iceberg encounter at southern locations of the Barents Offshore Region. We will discuss concerns related to the selection of the design basis for the Barents Sea, including the Russian part of the Barents Sea, and discuss the term “negligible”. Of particular interest are criteria related to the need for disconnection options for production units. The objective of the presented research is to draw attention to the importance of the design basis, for the proper design of all field facilities. The variability in climate conditions from one year to another should be recognized with particular emphasis on past extremes, which cannot be excluded to appear in the future, even in the case of an Arctic where the average temperatures have been increasing during the last decades. The paper concludes with recommendations for thorough preparation of the design basis for the entire Barents Sea area.
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