首页> 外文期刊>Science in China. Series D, Earth sciences >Determination of paleo-pressure for a natural gas pool formation based on PVT characteristics of fluid inclusions in reservoir rocks ―A case study of Upper-Paleozoic deep basin gas trap of the Ordos Basin
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Determination of paleo-pressure for a natural gas pool formation based on PVT characteristics of fluid inclusions in reservoir rocks ―A case study of Upper-Paleozoic deep basin gas trap of the Ordos Basin

机译:基于储集岩中流体包裹体PVT特征的天然气藏地层古压力确定-以鄂尔多斯盆地上古生界深盆气藏为例

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摘要

It has been proved to be a difficult problem to determine directly trapping pressure of fluid inclusions. Recently, PVT simulation softwares have been applied to simulating the trapping pressure of petroleum inclusions in reservoir rocks, but the reported methods have many limitations in practice. In this paper, a method is suggested to calculating the trapping pressure and temperature of fluid inclusions by combining the isochore equations of a gas-bearing aqueous inclusion with its coeval petroleum inclusions. A case study was conducted by this method for fluid inclusions occurring in the Upper-Paleozoic Shanxi Formation reservoir sandstones from the Ordos Basin. The results show that the trapping pressure of these inclusions ranges from 21 to 32 MPa, which is 6—7 MPa higher than their minimum trapping pressure although the trapping temperature is only 2—3 ℃ higher than the homogenization temperature. The trapping pressure and temperature of the fluid inclusions decrease from southern area to northern area of the basin. The trapping pressure is obviously lower than the state water pressures when the inclusions formed. These data are consistent with the regional geological and geochemicai conditions of the basin when the deep basin gas trap formed.
机译:已经证明,确定直接捕获流体夹杂物的压力是一个困难的问题。近来,PVT模拟软件已经被用于模拟储层岩石中石油夹杂物的捕集压力,但是所报道的方法在实践中有很多局限性。本文提出了一种通过结合含气含水包裹体与其等价石油包裹体的等时线方程来计算流体包裹体的捕集压力和温度的方法。用这种方法对鄂尔多斯盆地上古生界山西组储层砂岩中发生的流体包裹体进行了案例研究。结果表明,尽管夹杂物的夹杂温度仅比均质温度高2-3℃,但夹杂物的夹杂压力范围为21至32 MPa,比其最小夹杂压力高6-7 MPa。流体包裹体的俘获压力和温度从盆地的南部到北部下降。夹杂物形成时,捕集压力明显低于状态水压。这些数据与深盆气藏形成时盆地的区域地质和地球化学条件是一致的。

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