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A new approach to multiphase geochemical speciation modeling

机译:多相地球化学形态模拟的新方法

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摘要

Geochemical modeling based on equilibrium thermodynamics has become a recognized tool for understanding water-rock interaction processes and mechanisms. However, for the last 40. years, little attention has been given to the interaction of water-rock-gas systems or water-rock-gas-petroleum systems, possibly due to the complexity of the equilibrium calculations. The program described here is particularly useful for modeling geochemical interactions in oil and gas reservoirs, where brines and minerals are just some of the phases present, together with gases, and petroleum liquids, or other liquid phases. It all seems that, through a global minimization procedure, the equilibrium state of all the components (or pseudo-components) present in a hydrocarbon charged reservoir can be easily calculated at any pressure and temperature, by combining classical fluid phase equilibrium concepts, electrolyte theory, and solid-liquid equilibrium theory.
机译:基于平衡热力学的地球化学建模已经成为了解水-岩相互作用过程和机理的公认工具。然而,在过去的40年中,由于平衡计算的复杂性,很少有人关注水-岩-气系统或水-岩-气-石油系统的相互作用。这里描述的程序对于在油气藏中模拟地球化学相互作用特别有用,在油气藏中,盐水和矿物质只是一些相,还有气体,石油液体或其他液相。似乎,通过整体最小化程序,通过结合经典的液相平衡概念,电解质理论,可以很容易地在任何压力和温度下计算出充烃油藏中所有组分(或拟组分)的平衡状态。 ,以及固液平衡理论。

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