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Heat and mass transfer analysis of depressurization-induced hydrate decomposition with different temperatures of over- and underburden

机译:减压诱导水合物分解的热量和传质分析,不同的过度卷积温度

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Natural Gas Hydrate (NGH) reserves are large and regarded as an important alternative future energy source. Safely and efficiently exploiting natural gas hydrates has recently become a hot issue around the world. The decomposition of natural gas hydrate requires a great deal of absorbed heat. The decomposition process is a complicated heat and mass transfer process with phase changes, such that heat and mass transfer will have a great impact on the decomposition results. Focusing on the heat transfer effect, a two dimensional mathematical model of natural gas hydrate decomposition was established. Using a numerical simulation method, the thermal conductivities of different porous mediums were selected and the bottom hole pressure (BHP) was changed under different overburden and underburden temperatures to simulate the depressurization exploitation of natural gas hydrates. The reservoir temperature distribution, hydrate decomposition front, gas production rate, and cumulative gas production under different cases were obtained. The results show that the incoming heat directly influenced the reservoir temperature distribution, hydrate decomposition rate, and gas production and the temperature at any point on the decomposition front is constant under certain BHP. When there was no external heat introduced into the hydrate-bearing layers, the impact of thermal conductivity on decomposition was greater, but decreased with increasing temperature of overburden and underburden. When no external heat was introduced into the hydrate-bearing layers, the BHP became the main controlling factor of the cumulative gas production, and the effect of the BHP on the cumulative gas production was gradually weakened with increasing temperatures of the overburden and underburden. (C) 2017 Elsevier B.V. All rights reserved.
机译:天然气水合物(NGH)储量巨大,被视为未来重要的替代能源。安全高效地开采天然气水合物已成为当今世界的热点问题。天然气水合物的分解需要大量吸收热量。分解过程是一个复杂的相变传热传质过程,传热传质对分解结果影响很大。以传热效应为核心,建立了天然气水合物分解的二维数学模型。采用数值模拟方法,选取不同多孔介质的导热系数,在不同的上覆和下覆温度下改变井底压力(BHP),模拟天然气水合物的降压开采。得到了不同情况下的储层温度分布、水合物分解前沿、产气量和累积产气量。结果表明,在一定的压头压力下,进入的热量直接影响储层的温度分布、水合物分解速率和产气量,分解前缘任意点的温度都是恒定的。当没有外部热量进入水合物层时,导热系数对分解的影响更大,但随着上覆层和下覆层温度的升高而减小。当不向含水合物层引入外部热量时,BHP成为累积产气量的主要控制因素,并且随着上覆岩层和下覆岩层温度的升高,BHP对累积产气量的影响逐渐减弱。(C) 2017爱思唯尔B.V.版权所有。

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