Measurement of Effective Hydrogen-Methane Gas Diffusion Coefficients in Reservoir Rocks

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Vladislav Arekhov, Timur Zhainakov, Torsten Clemens, Jonas Wegner
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Abstract

Summary If hydrogen is stored in depleted gas fields, the remaining hydrocarbon gas can be used as cushion gas. The composition of the backproduced gas depends on the magnitude of mixing between the hydrocarbon gas and the hydrogen injected. One important parameter that contributes to this process of mixing is molecular diffusion. Although diffusion models are incorporated in the latest commercial reservoir simulators, effective diffusion coefficients for specific rock types, pressures, temperatures, and gas compositions are not available in the literature. Thus, laboratory measurements were performed to improve storage performance predictions for an underground hydrogen storage (UHS) project in Austria. An experimental setup was developed that enables measurements of effective multicomponent gas diffusion coefficients. Gas concentrations are detected using infrared light spectroscopy, which eliminates the necessity of gas sampling. To test the accuracy of the apparatus, binary diffusion coefficients were determined using different gases and at multiple pressures and temperatures. Effective diffusion coefficients were then determined for different rock types. Experiments were performed multiple times for quality control and to test reproducibility. The measured binary diffusion coefficients without porous media show a very good agreement with the published literature data and available correlations based on the kinetic gas theory (Chapman-Enskog, Fuller-Schettler-Giddings). Measurements of effective diffusion coefficients were performed for three different rock types that represent various facies in a UHS project in Austria. A correlation between static rock properties and effective diffusion coefficients was established and used as input to improve the numerical model of the UHS. This input is crucial for the simulation of backproduced gas composition and properties which are essential parameters for storage economics. In addition, the results show the impact of pressure on effective diffusion coefficients, which impacts UHS performance.
储层岩石中氢-甲烷气体有效扩散系数的测定
如果将氢气储存在枯竭的气田中,剩余的碳氢化合物气可以用作缓冲气。回产气的组成取决于烃类气体和注入的氢之间的混合程度。导致这一混合过程的一个重要参数是分子扩散。尽管最新的商业油藏模拟器中包含了扩散模型,但在文献中还没有针对特定岩石类型、压力、温度和气体成分的有效扩散系数。因此,进行了实验室测量,以改善奥地利地下储氢(UHS)项目的存储性能预测。开发了一种实验装置,可以测量有效的多组分气体扩散系数。利用红外光谱法检测气体浓度,消除了气体采样的必要性。为了测试仪器的准确性,在不同的气体和不同的压力和温度下测定了二元扩散系数。然后确定了不同岩石类型的有效扩散系数。实验进行了多次质量控制和测试再现性。根据动力学气体理论(Chapman-Enskog, Fuller-Schettler-Giddings),测量的无多孔介质二元扩散系数与已发表的文献数据和可用的相关性非常吻合。在奥地利的UHS项目中,对代表不同相的三种不同岩石类型进行了有效扩散系数的测量。建立了岩石静态特性与有效扩散系数之间的相关性,并将其作为输入来改进UHS数值模型。这种输入对于模拟回采气体的成分和性质至关重要,而这些又是储气经济性的重要参数。此外,研究结果还显示了压力对有效扩散系数的影响,从而影响UHS性能。
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
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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