Study on influences of geological and gas source conditions on gas-chimney hydrate accumulation using a reservoir numerical simulation method

IF 6.5 3区 工程技术 Q2 ENERGY & FUELS
Liang Zhang , Fuyang Li , Lu Yu , Songhe Geng , Chunjie Li , Yujie Sun
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Abstract

The Shenhu Area in the South China Sea is rich in oil and gas resources and has many vertical gas chimneys, making it an excellent geological environment for hydrate accumulation. This paper examines the geological conditions governing these gas-chimneys. A numerical simulation method based on the partial-equilibrium reaction model of hydrate was applied to simulate the migration of methane gas and the resultant hydrate formation when the gas enters the hydrate stability zone under the seabed through gas-chimneys. The dynamics of this gas-chimney hydrate accumulation were analyzed, and the influences of different factors—namely, the fluid supply time, rate, and temperature—on the formation temperature and ultimate distribution of the hydrate reservoir were evaluated. The simulation results indicate that the accumulation of hydrate via gas-chimneys is significantly affected by the temperature of the gas source, the transfer state of the methane gas, and the number of cycles of alternating gas–water invasion. Hydrate accumulation takes shape in an annular or semi-annular distribution pattern divided by fluid state as follows: a two-phase gas–water zone, a three-phase gas–water–hydrate zone, a two-phase water–hydrate zone, and a phase of water passing from the inside to the outside. Formation inclination and reservoir heterogeneity can greatly affect the distribution shape and abundance of the hydrate. A high fluid supply temperature, frequent alternating invasions of gas and water, and long-term pore-water invasion at a high rate can jointly cause a large central hydrate-free zone. In contrast, a long-term supply shutdown during the alternating gas–water invasion process, and a high gas rate with a low water rate in the gas-dominant invasion stage, foster the accumulation of hydrate in great abundance and with considerable thickness. The results of this study can help us understand the accumulation of hydrate through gas chimneys in the Shenhu Area.
用储层数值模拟方法研究地质条件和气源条件对烟囱型水合物成藏的影响
南海神狐海域油气资源丰富,垂直烟囱多,具有良好的水合物成藏地质环境。本文探讨了控制这些烟囱的地质条件。采用基于水合物部分平衡反应模型的数值模拟方法,模拟了甲烷气体经气烟囱进入海底水合物稳定带时的运移和水合物形成过程。分析了气烟囱型水合物成藏动力学,评价了供液时间、供液速率、供液温度等因素对水合物储层温度和最终分布的影响。模拟结果表明,气源温度、甲烷气体的传递状态以及气水交替侵入循环次数对烟囱水合物的聚集有显著影响。水合物成藏形成按流体状态划分为两相气水区、三相气水水合物区、两相水水合物区和由内向外运移的水相的环状或半环状分布格局。地层倾角和储层非均质性对水合物的分布形态和丰度影响较大。较高的供液温度、频繁的气水交替侵入以及长期高速率的孔隙水侵入可共同造成较大的中心无水合物区。而在气水交替侵入过程中,长期的断供,以及气控侵入阶段的高气率和低水率,则有利于水合物形成丰度大、厚度大的聚集。研究结果有助于认识神狐地区烟囱型水合物的成藏规律。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Natural Gas Industry B
Natural Gas Industry B Earth and Planetary Sciences-Geology
CiteScore
5.80
自引率
6.10%
发文量
46
审稿时长
79 days
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