Pressure Index (PI): A Novel Practical Method for Evaluating Pressure in Offshore Malaysia

Y. Sugiharto, Gamal R. Gaafar, Isham F. Ishak, Benard Ralphie, Muhammad Banuri
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Abstract

Pressure analysis is concerned with the study of systematic variations of reservoir pore pressure with depth. The most common interpretation for pressure analysis is pressure-depth plot analysis, but other techniques that magnify understated pressure differences are also available. Formation pressure measurement is of immense value in quantitative evaluation and risking of prospects. Once the pressure data has been acquired, we need to understand how to interpret the data received because reservoir pressure data has numerous applications and interpreting it wrongly could make the results misleading. At equilibrium state (i.e. there are no net forces, and no acceleration), a fluid in the system is called hydrostatic equilibrium. Hydrostatic pressure increases with depth measured from the surface due to the increasing weight of fluid exerting downward force from above. The traditional pressure evaluation is usually done in conventional unit such as psi, kPa, psi/feet, psi/m, kPa/m, ppg. The current work will introduce the concepts and definitions of formation pressure evaluation using Pressure Index (PI) with the unit g/cc. For better understanding of the application of PI, some reservoir studies are also discussed in this paper.
压力指数(PI):一种评估马来西亚近海压力的新颖实用方法
压力分析是研究储层孔隙压力随深度的系统变化。压力分析最常见的解释是压力-深度图分析,但也有其他技术可以放大被低估的压力差。地层压力测量在油气远景定量评价和风险评估中具有重要价值。一旦获得了压力数据,我们需要了解如何解释接收到的数据,因为储层压力数据有许多应用,错误的解释可能会导致结果具有误导性。在平衡状态下(即没有净力,也没有加速度),系统中的流体称为流体静力平衡。静水压力随着测量深度的增加而增加,这是由于从上方施加向下力的流体重量的增加。传统的压力评估通常以psi、kPa、psi/feet、psi/m、kPa/m、ppg等常规单位进行。目前的工作将介绍使用单位为g/cc的压力指数(PI)进行地层压力评估的概念和定义。为了更好地理解PI的应用,本文还讨论了一些油藏研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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