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Mathematical modelling on transport of petroleum hydrocarbons in saturated fractured rocks

机译:饱和裂隙岩中石油烃运移的数学模型

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The present paper addresses critical issues that describe the dissolution mass transfer of petroleum hydrocarbons in a saturated subsurface system. The field procedure associated with the estimation of Light Non-Aqueous Phase Liquid (LNAPL) thickness in site monitor wells is revisited. A brief theory has been included on the composition and transport of petroleum hydrocarbons following an onshore oil spill in order to demonstrate the level of complexity associated with the LNAPL dissolution mass transfer even in a classical porous medium. However, such studies in saturated fractured rocks are highly complex and limited, and hence, deserve a special attention as the fate and transport of the petroleum hydrocarbons are not uncommon in saturated fractured rocks. In this context, an improved mathematical model has been proposed that will better describe the dissolution kinetics of petroleum hydrocarbons in saturated fractured rocks at the scale of a single fracture using dual-porosity concept. The lumped mass transfer coefficient in a classical porous medium proposed depends on mean grain size, while the same parameter has been replaced by an equivalent average thickness of fracture aperture that better describes the LNAPL dissolution rate in a coupled fracture-matrix system. A set of nonlinear coupled partial differential equations is deduced for a coupled fracture-matrix system in analogy with the differential equations of a classical porous medium. The proposed mathematical model may work well for the fracture aperture thicknesses varying between 100 and 500 microns with a relatively low Reynolds Number and initial NAPL saturation.
机译:本文解决了描述饱和地下系统中石油碳氢化合物溶解传质的关键问题。重新研究了与现场监测井中轻质非水相液体(LNAPL)厚度估算有关的现场程序。关于陆上溢油事故后石油烃的组成和运输的简要理论已被包括在内,以证明即使在传统的多孔介质中,与LNAPL溶出质量转移相关的复杂程度也是如此。但是,在饱和裂隙岩中进行的此类研究非常复杂且受限制,因此,在饱和裂隙岩中石油烃的命运和运输并不罕见,因此值得特别关注。在这种情况下,已经提出了一种改进的数学模型,该模型将使用双孔隙率概念更好地描述在单个裂缝范围内的饱和裂缝性岩石中石油烃的溶解动力学。提出的经典多孔介质中的集总传质系数取决于平均晶粒尺寸,而相同的参数已被等效的裂隙平均厚度所代替,该裂隙平均厚度更好地描述了耦合裂隙基质系统中的LNAPL溶解速率。类似于经典的多孔介质的微分方程,推导了一套耦合的裂缝矩阵系统的非线性耦合的偏微分方程组。对于具有相对较低的雷诺数和初始NAPL饱和度的100至500微米之间变化的裂缝孔径厚度,所提出的数学模型可能效果很好。

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