流量和流体碱度对储层砂岩细颗粒运动及岩石物性的影响

Passer Journal Pub Date : 2019-09-01 DOI:10.24271/psr.05
K. Ahmad
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引用次数: 2

摘要

与细运移有关的渗透率下降是大多数油藏中最普遍的现象之一。砂岩储层精细运移强度大,但常被误读。细颗粒的运动可能难以识别,甚至不容易预测和解释。本研究的主要目的是研究流量和流体碱度对选定储层砂岩岩石物性的影响。为了确定粘土矿物的类型,并计算每种类型的百分比以及岩石基质中的形状、位置和分布,首先对选定的岩心样品进行了x射线衍射和扫描电子显微镜检查。这也是为了确定总体矿物学和粘土分数。研究结果表明,高碱度流体流过储层地层可能导致渗透率显著降低。在低pH流体中,损伤程度小于高pH流体。然而,通过注入碱性溶液(pH 9和pH 11),逐步增加流速(50、100、200 ml/ h),进行了一系列岩心驱替实验,估计了渗透率的降低,并在测试前测量了这些孔隙度的基本岩石物理性质和初始渗透率。最后,进行了一系列岩心驱替试验,研究粘土矿物含量、pH值和流量对砂岩储层渗透率的影响。在pH值为11的碱性溶液中,渗透率降低幅度高达36% ~ 50%,而在pH值为9的碱性溶液中,渗透率降低程度较轻。因此,高流速和高ph值对储层的破坏程度更大。结果表明,岩心中黏土矿物具有精细运移的特征,对储层特征产生了负面影响。
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The Role of Flow Rate and Fluid Alkalanity on Fine Particles Movement and Influencing the Petrophysical Properties of Reservoir Sandstone
Permeability decline related with fine migration is one of the most widespread phenomenon that occurs in most oil reservoirs. Fine migration is intensive in sandstone reservoir, but frequently misinterpreted. Movement of fine particles might be problamatic to identify and even not easy to predict and interpret. The main goal of this study is to  investigate the influence of flow rate and fluid alakalinity on petrophysical properties of selected reservoir sandstone.  To determine the types of clay minerals with calculating the percentage of each types and the shape, position, and distribution within the rock matrix, first selected core samples were examined by X-ray diffraction and scanning electron microscopy. This is also to identify the bulk mineralogy and clay fraction.. The result of this study shows that higher alakalinity fluid flow through reservoir standtone might cause a significant reduction on permeability. While at low pH fluid, the degree of damage is less damage than high pH value. However, the reduction on permeability was estimated by conducting a series of core flood experiments by injecting alkaline solution (pH 9 and pH 11) with stepwise increasing flow rate (50, 100, 200 ml/ h). Furthermore, the basic petrophysical properties of such porosity and initial permability were measured prior to testing.  Ultimately, a series of core flooding were also conducted to investigate the influence of clay mineral content, pH and flow rate on sandtone reservoir permeability. High pH solutions significant permeability reductions were recorded, during the flood of pH 11 alkaline solution reductions as high as 36- 50-% were obtained while, the degree of damage was observed  less severe with (pH9). Hence, the magnitude of damage was more severe with high flow rate and higher pH. The result shows that the clay minerals present in the cores were characteristics to fine migration thus causing negative impact on reservoir characteristics.
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CiteScore
0.50
自引率
0.00%
发文量
23
审稿时长
12 weeks
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