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Modelling Simulation of Fluid Flow Behaviour During Carbondioxide Sequestration in Coal Structure Using Comsol Multiphysics

机译:基于Comsol多物理的二氧化碳在煤固存过程中流动行为的建模与仿真。

摘要

In the present world, Global Warming has been one of the biggest problems regarding environmental aspect and CO2 is held responsible for that. It is an inevitable necessity to mitigate the concentration of CO2 in the atmosphere. CO2 sequestration is one of the best methods to reduce its concentration by trapping it beneath the earth in different geological conditions. The unmined coal seams and thin bands of coal provide a potential storage for CO2 with suitable geological environment. These days it has become necessary to study the relationship between coal structure and flow of fluids inside. In this project, an effort has been made to study the behaviour of fluids i.e. carbon dioxide and methane inside of coal and the analysis has been carried out to study their velocity and pressure variations using COMSOL Multiphysics. Coal contains both cleat and porous structure. Cleats are the natural fractures in coal and pores are the important factors for migration of fluid inside coal. Two separate models are developed to understand the fluid flow behaviour in both cleat and porous structure of coal. A study on 3D model has also been carried out by developing a uniform coal block to analyze pressure and velocity variations inside it.
机译:在当今世界,全球变暖一直是环境方面的最大问题之一,二氧化碳对此负有责任。减轻大气中二氧化碳的浓度是不可避免的。固存二氧化碳是通过在不同地质条件下将其捕获在地下之下来降低其浓度的最佳方法之一。未开采的煤层和薄煤带为具有合适地质环境的二氧化碳提供了潜在的储存地。这些天来,有必要研究煤结构与内部流体流动之间的关系。在该项目中,已努力研究煤内部的流体(即二氧化碳和甲烷)的行为,并使用COMSOL Multiphysics进行了分析以研究其速度和压力变化。煤既具有割理又具有多孔结构。煤层是煤中的天然裂缝,孔隙是煤中流体运移的重要因素。开发了两个独立的模型以了解煤的割理和多孔结构中的流体流动行为。通过开发均匀的煤块来分析其中的压力和速度变化,也已经对3D模型进行了研究。

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