An Uncertainty Quantification Framework for Studying the Effect of Spatial Heterogeneity in Reservoir Permeability on CO2 Sequestration
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- 作者：Zhangshuan Hou (1)
Dave W. Engel (2)
Guang Lin (2)
Yilin Fang (1)
Zhufeng Fang (1) - 关键词：Uncertainty quantification ; Efficient sampling ; Reservoir heterogeneity ; Carbon sequestration
- 刊名：Mathematical Geosciences
- 出版年：2013
- 出版时间：October 2013
- 年：2013
- 卷：45
- 期：7
- 页码：799-817
- 全文大小：4473KB
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Dave W. Engel (2)
Guang Lin (2)
Yilin Fang (1)
Zhufeng Fang (1)
1. Earth Systems Science Division, Pacific Northwest National Laboratory, Post Office Box 999, Richland, WA, 99352, USA
2. Computational Science & Mathematics Division, Pacific Northwest National Laboratory, Post Office Box 999, Richland, WA, 99352, USA - ISSN：1874-8953
文摘
A new uncertainty quantification framework is adopted for carbon sequestration to evaluate the effect of spatial heterogeneity of reservoir permeability on CO2 migration. Sequential Gaussian simulation is used to generate multiple realizations of permeability fields with various spatial statistical attributes. In order to deal with the computational difficulties, the following ideas/approaches are integrated. First, different efficient sampling approaches (probabilistic collocation, quasi-Monte Carlo, and adaptive sampling) are used to reduce the number of forward calculations, explore effectively the parameter space, and quantify the input uncertainty. Second, a scalable numerical simulator, extreme-scale Subsurface Transport Over Multiple Phases, is adopted as the forward modeling simulator for CO2 migration. The framework has the capability to quantify input uncertainty, generate exploratory samples effectively, perform scalable numerical simulations, visualize output uncertainty, and evaluate input-output relationships. The framework is demonstrated with a given CO2 injection scenario in heterogeneous sandstone reservoirs. Results show that geostatistical parameters for permeability have different impacts on CO2 plume radius: the mean parameter has positive effects at the top layers, but affects the bottom layers negatively. The variance generally has a positive effect on the plume radius at all layers, particularly at middle layers, where the transport of CO2 is highly influenced by the subsurface heterogeneity structure. The anisotropy ratio has weak impacts on the plume radius, but affects the shape of the CO2 plume.