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首页> 外文期刊>Water resources research >Impact of Three-Phase Relative Permeability and Hysteresis Models on Forecasts of Storage Associated With CO_2-EOR
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Impact of Three-Phase Relative Permeability and Hysteresis Models on Forecasts of Storage Associated With CO_2-EOR

机译:三相相对磁导率和滞后模型对与CO_2-EOR关联的储层预测的影响

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Geological CO2 sequestration in conjunction with enhanced oil recovery (CO2-EOR) includes complex multiphase flow processes compared to CO2 storage in deep saline aquifers. Two of the most important factors affecting multiphase flow in CO2-EOR are three-phase relative permeability and associated hysteresis, both of which are difficult to measure and are usually represented by numerical interpolation models. The purpose of this study is to improve understanding of (1) the relative impacts of different three-phase relative permeability models and hysteresis models on CO2 trapping mechanisms, and (2) uncertainty associated with these two factors. Four different three-phase relative permeability models and three hysteresis models were applied to simulations of an active CO2-EOR site, the SACROC unit located in western Texas. To eliminate possible bias of deterministic parameters, we utilized a sequential Gaussian simulation technique to generate 50 realizations to describe heterogeneity of porosity and permeability, based on data obtained from well logs and seismic survey. Simulation results of forecasted CO2 storage suggested that (1) the choice of three-phase relative permeability model and hysteresis model led to noticeable impacts on forecasted CO2 sequestration capacity; (2) impacts of three-phase relative permeability models and hysteresis models on CO2 trapping are small during the CO2-EOR injection period, and increase during the post-EOR CO2 injection period; (3) the specific choice of hysteresis model is more important relative to the choice of three-phase relative permeability model; and (4) using the recommended three-phase WAG (Water-Alternating-Gas) hysteresis model may increase the impact of three-phase relative permeability models and uncertainty due to heterogeneity.
机译:与将CO2储存在深层盐水中相比,地质CO2隔离和提高采油率(CO2-EOR)包括复杂的多相流过程。影响CO2-EOR中多相流动的两个最重要的因素是三相相对渗透率和相关的滞后现象,这两者都很难测量,并且通常用数值插值模型来表示。这项研究的目的是增进对(1)不同三相相对渗透率模型和磁滞模型对CO2捕集机制的相对影响的理解,以及(2)与这两个因素相关的不确定性。四个不同的三相相对渗透率模型和三个磁滞模型被用于模拟活跃的CO2-EOR站点,即位于德克萨斯州西部的SACROC单元。为了消除确定性参数的可能偏差,我们基于从测井和地震勘测获得的数据,利用顺序的高斯模拟技术生成了50个描述孔隙度和渗透率异质性的实现。预测的CO2封存模拟结果表明:(1)三相相对渗透率模型和滞后模型的选择对预测的CO2封存量产生了明显的影响; (2)三相相对渗透率模型和滞后模型在CO2-EOR注入期间对CO2捕集的影响很小,而在EOR后注入CO2期间则增加。 (3)相对于三相相对磁导率模型的选择,磁滞模型的具体选择更为重要; (4)使用推荐的三相WAG(水交替气)滞后模型可能会增加三相相对渗透率模型的影响以及由于异质性带来的不确定性。

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