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首页> 外文期刊>Erdol Erdgas Kohle >Effect of Pressure and Temperature on Petrophysieal Characteristics in the Case of Carbonate Reservoirs
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Effect of Pressure and Temperature on Petrophysieal Characteristics in the Case of Carbonate Reservoirs

机译:碳酸盐岩储层中压力和温度对岩石物性的影响

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摘要

The effect of temperature on petrophysical properties reduction might be one of the main reasons in the failure of thermal enhanced oil recovery pilot tests. The temperature and pressure changes constitute the fundamental elements in controlling fluid circulation. Thus, the conducted study is aimed to investigate this statement in the context of carbonate reservoirs and their petrophysical characteristics. Intensive runs of flooding experiments were performed using carbonate samples from Middle East reservoirs at different effective pressures up to 4000 psi (276 bar) and temperatures reaching 100 °C to investigate fluid circulation behavior. In addition a tex-tural examination of the carbonate samples was conducted using an ordinary microscope and scanning electron microscope (SEM). Results indicated that permeability reduction increases gradually with increasing pressure and temperature. It was found that a permeability reduction of 50% was recorded at temperatures above 50 °C compared with the initial permeability at 25 °C. Furthermore, the permeability reduction reached 59% at an effective pressure of 4000 psi at 100 °C compared to initial permeability at 725 psi (50 bar) and at 25 °C. According to the overall results, the effect of temperature on permeability reduction in the applied carbonate samples is as important as that of the effective pressure. The reduction phenomenon can be explained by the process of packing and compaction leading to rock deformation. In addition, and based on the textural analysis, no formation damage was noticed, and permeability reduction occurred at the applied conditions was reversible.
机译:温度对岩石物理性能降低的影响可能是热强化采油率先导试验失败的主要原因之一。温度和压力的变化是控制流体循环的基本要素。因此,进行的研究旨在研究碳酸盐岩储层及其岩石物理特征的背景。使用中东储层的碳酸盐样品在高达4000 psi(276 bar)的不同有效压力和温度达到100°C的条件下进行了密集的驱油实验,以研究流体的循环行为。另外,使用普通显微镜和扫描电子显微镜(SEM)进行碳酸盐样品的tex-tural检查。结果表明,渗透率降低随压力和温度的升高而逐渐增加。发现在高于50℃的温度下记录的磁导率降低了25%,而在25℃下的初始磁导率降低了50%。此外,与在725 psi(50 bar)和25°C的初始渗透率相比,在100°C的有效压力为4000 psi时,渗透率下降达到59%。根据总体结果,温度对所施加碳酸盐样品渗透率降低的影响与有效压力同样重要。减少现象可以通过导致岩石变形的堆积和压实过程来解释。另外,基于组织分析,未发现地层破坏,并且在所施加的条件下发生的渗透率降低是可逆的。

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