Definition and implementation of a fully coupled THM model for unsaturated rocks

机译：非饱和岩石全耦合THM模型的定义与实现

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AThermo-Hydro-Mechanical (THM) model for partially saturated rocks is developed and implemented.rnThe hypothesis of constant air pressure simplifies the equations and improves efficiency of calculationrnwhile still allowing the description of vapor flow.The implementation uses a fully coupled approach. Comparisonrnagainst experimental data is performed. Results are promising, yet additional comparisons are required to fullyrnvalidate the model and its implementation.

机译：开发并实现了部分饱和岩石的AT-Hydro-Hydro-Mechanical（THM）模型。恒定气压的假设简化了方程，提高了计算效率，同时仍然允许描述蒸汽流。该实现采用完全耦合的方法。对比实验数据进行。结果令人鼓舞，但还需要进行其他比较才能完全验证模型及其实现。

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《Rock mechanics for resources, energy and environment》|2013年|507-513|共7页
会议地点 Wroclaw(PL)
作者
A. Haxaire; V. Galavi; R.B.J. Brinkgreve;
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作者单位

Plaxis bv, The Netherlands;

Plaxis bv, The Netherlands;

Faculty of Civil Engineering and Geosciences, Delft University of Technology, The Netherlands;

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正文语种 eng
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Definition and implementation of a fully coupled THM model for unsaturated rocks

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