Improved Thermal Model for Hydrate Formation Drilling Considering Multiple Hydrate Decomposition Effects

Youqiang Liao, Xiaohui Sun, Zhiyuan Wang, Baojiang Sun
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Abstract

Hydrate is ice-like solid non-stoichiometric crystalline compound, which is stable at favorable low temperature and high-pressure conditions. The predominant gas component stored in naturally-occurring hydrate bearing sediment is CH4 and is estimated about 3000–20000 trillion cubic meter worldwide. Thus, it has attracted significant research interests as an energy source from both academic and industry for the past two decades. Ensuring drilling safety is much important to realize efficient exploitation of hydrate source. Additionally, accurate prediction of wellbore temperature field is of great significance to the design of drilling fluid and cement slurry and the analysis of wellbore stability. However, the heat transfer process in wellbore and hydrate layer during drilling through hydrate formation is a complex phenomenon. The calculation method used in the conventional formation cannot be fully applied to hydrate reservoir drilling, largely due to the complex interactions between the hydrate decomposition, multiphase flow and heat transfer behaviors. In this study, an improved thermal model of wellbore for hydrate layer drilling process is presented by coupling the dynamic decomposition of hydrate, the transportation of hydrate particles in cuttings and heat transfer behaviors in multiphase flow. The distribution of temperature field and rules of hydrate decomposition both in wellbore and hydrate layers are thoroughly analyzed with case study, which is very helpful for the designing drilling parameters, avoiding the gas kick accidents. As well as making a detailed guidance of wellbore stability analysis. This proposed mathematical model is a more in-depth extension of the conventional temperature field prediction model of wellbore, it can present some important implications for drilling through gas–hydrate formation for practical projects.
考虑多重水合物分解效应的水合物地层钻井热模型改进
水合物是冰状固体非化学计量晶体化合物,在低温高压条件下稳定存在。天然水合物沉积物中主要的气体成分是CH4,估计全世界约有3000-20000万亿立方米。因此,在过去的二十年里,它作为一种能源吸引了学术界和工业界的极大研究兴趣。保证钻井安全是实现水合物资源高效开采的关键。此外,准确预测井筒温度场对钻井液和水泥浆的设计以及井筒稳定性分析具有重要意义。然而,在水合物地层钻井过程中,井筒和水合物层内的传热过程是一个复杂的现象。由于水合物分解、多相流和换热行为之间的复杂相互作用,常规地层计算方法不能完全应用于水合物储层钻井。将水合物的动态分解、岩屑中水合物颗粒的运移与多相流传热行为相结合,建立了水合物层钻井过程中改进的井筒热模型。结合实例,深入分析了水合物在井筒和水合物层中的温度场分布和水合物分解规律,为钻井参数的设计提供了理论依据,避免了气涌事故的发生。并对井眼稳定性分析进行了详细的指导。该数学模型是对常规井筒温度场预测模型的更深入的扩展,对实际工程中天然气水合物地层钻井具有重要的指导意义。
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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