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首页> 外文期刊>Journal of Heat Transfer >Heat-Induced Evolution of Phase Transformations in Tetrahydrofuran Hydrate-Bearing Sediment
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Heat-Induced Evolution of Phase Transformations in Tetrahydrofuran Hydrate-Bearing Sediment

机译:四氢呋喃水合物沉积物中相变的热诱导演化

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摘要

Heat conduction and phase transformations are basic physical-chemical process and control the kinetics of dissociation, fluid flow and strata deformation during hydrate dissociation in sediments. This paper presents a simplified analysis of the thermal process by assuming that the heat-induced evolution can be decoupled from flow and deformation processes. Self-similar solutions for one-, two- and three-phase transformation fronts are obtained. A series of experiments on THF-hydrate-bearing sediments was conducted to test the theory. The theoretical, numerical and experimental results on the evolution of hydrate dissociation front in the sediment are in good agreement.
机译:导热和相变是基本的物理化学过程,可控制沉积物中水合物分解过程中的解离动力学,流体流动和地层变形。本文假设热诱导的演化可以与流动和变形过程分离,从而对热过程进行了简化分析。获得了一相,两相和三相变换前沿的自相似解。对含THF水合物的沉积物进行了一系列实验以验证该理论。沉积物中水合物离解锋演化的理论,数值和实验结果吻合良好。

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