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The U. S. Geological Survey carbon dioxide storage efficiency value methodology: results and observations

机译:U. S.地质调查二氧化碳储存效率值方法:结果与观察

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In order to complete the 2013 U.S. Geological Survey (USGS) assessment of carbon dioxide (CO2) storage resources [1], a methodology was needed to determine the CO2 storage efficiency of individual rock strata [2]. The method that was used involved a storage efficiency approximation by MacMinn et al. [3], combined with a brine viscosity model by Mao and Duan [4], and thermal and pressure data from petroleum fields across basins [5]. The resulting efficiencies indicated that both salinity of the pore fluid and the thermal gradient have a strong effect on the amount of CO2 that strata could store.
机译:为了完成二氧化碳(CO2)储存资源的2013年的美国地质调查(USGS)评估[1],需要一种方法来确定单个岩石阶层的CO2储存效率[2]。使用的方法涉及Macminn等人的存储效率近似。 [3],与Mao和Duan [4]的盐水粘度模型相结合,以及来自盆地的石油场的热和压力数据[5]。所产生的效率表明,孔隙流体的盐度和热梯度的盐度对地层可以存储的CO 2的量具有很强的效果。

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