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首页> 外文期刊>Hydrology and Earth System Sciences Discussions >Probabilistic modeling of field-scale CO 2 generation by carbonate–clay reactions in sedimentary basins
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Probabilistic modeling of field-scale CO 2 generation by carbonate–clay reactions in sedimentary basins

机译:泥土粘土反应在沉积盆地中碳酸盐粘土反应的概率建模

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This work explores a probabilistic modeling workflow and its implementation targeting CO 2 generation rate and CO 2 source location by the occurrence of carbonate–clay reactions (CCRs) in three-dimensional realistic sedimentary basins. We ground our study on the methodology proposed for a one-dimensional case study and a single CCR formulation by Ceriotti et?al. ( 2017 ) which includes a framework to account for thermodynamic parameter uncertainties. This methodology is here extended to a realistic three-dimensional sedimentary basin setting and transferred to encompass different types of CCRs, including two newly formulated CCRs which account for minerals typically observed in sedimentary environments. While testing the ability of the selected procedure to model diverse CCRs in three-dimensional realistic subsurface sedimentary systems, we quantitatively compare the impact of CCR formulation on the spatial distribution of CO 2 source location, temperature and pressure compatible with CO 2 gaseous generation, and CO 2 generation rate in three-dimensional environments characterized by complex and non-uniform stratigraphy. The application of the procedure to various types of CCRs enables us to provide an insight into the impact of mineralogical composition on the activation temperature and pressure and the amount of CO 2 released by the different CCR mechanisms. Finally, we show the implementation of the proposed probabilistic framework to define scenarios associated with various levels of probability to be used as the input and boundary conditions for CO 2 migration and transport models in the subsurface.
机译:这项工作探讨了概率建模工作流程及其实施,其通过三维现实沉积盆中的碳酸盐粘土反应(CCR)发生了靶向CO 2生成率和CO 2源定位。我们研究了我们对一维案例研究的方法的研究和Ceriotti等的单一CCR配方。 (2017)包括一个框架,用于考虑热力学参数不确定性。此方法在此延伸到现实的三维沉积盆地设置,并转移以包含不同类型的CCR,包括两个新配制的CCR,其考虑了通常在沉积环境中观察到的矿物质。在测试所选步骤的能力,在三维现实地下沉积系统中进行模拟各种CCR的能力,我们可以定量比较CCR配方对CO 2源位置,温度和压力的空间分布的影响,与CO 2气体等一体相容,以及三维环境中的二氧化碳生成率,其特征在于复杂和非均匀地层。该程序的应用对各种类型的CCR使我们能够深入了解矿物学组合物对由不同CCR机制释放的CO 2的影响的影响。最后,我们展示了所提出的概率框架来定义与各种概率相关的场景,以用作子下CO 2迁移和传输模型的输入和边界条件。

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