世界许多地区如墨西哥湾,存在着大量天然气渗漏并形成水合物的现象。出于科学、生态、气候和安全的需要,人类有必要弄清存在于海底以水合物形式存在的天然气的比例。因此,构建了水合物形成量的线性动力学模型,以分析墨西哥湾GC185块区Bush高地海底渗漏天然气的地质过程和行为。Bush高地渗漏的天然气来源于附近的Jolliet气藏,结果表明,渗漏天然气中约有9%在海底形成了水合物。 In many parts of the world, such as the Gulf of Mexico, there is a significant amount of gas seepage and hydrate formation. For the sake of science, ecology, climate and security, it is necessary for mankind to understand the proportion of natural gas that exists in the sea as a hydrate. Therefore, a linear kinetic model of hydrate formation was constructed to analyze the geological process and behavior of gas seepage from the seabed of the Bush Highlands in the GC185 block of the Gulf of Mexico. Natural gas seepage from Bush heights originates from the nearby Jolliet gas reservoir and results show that about 9% of seepage gas forms hydrates at the seabed.