首页> 外文会议>Transactions of the SPWLA (Society of Professional Well Log Analysts) Forty-Third Annual Logging Symposium, Jun 2-5, 2002, Oiso, Japan >Theoretical and Experimental Studies of Membrane Potential in Shaly Sands for Improved Rw Calculation
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Theoretical and Experimental Studies of Membrane Potential in Shaly Sands for Improved Rw Calculation

机译:改进Rw计算的泥质沙质膜势的理论和实验研究

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Formation water resistivity (Rw) is one of the most important parameters in log interpretation Spontaneous potential or SP logs have been used in Rw calculation, which is especially effective in clean sand However, when the sand contains clay, the clay interferes with the ion diffusion process and thus affects the membrane potential generated. Since the dominant part of SP electrochemical potential is related to the membrane potential, it is very important to study the membrane potential in shaly sand to correctly determine the resistivity of formation water. Because of the difference in the mobility of positive and negative ions, membrane potential is generated when two electrolyte solutions of different concentration come in contact. This membrane potential also depends on the nature of the membrane or the shale content in the sand. In this paper, we present a systematical study of the membrane potential for oil-bearing shaly sands on the basis of the electrochemical theory and the conductivity properties of the shaly sands. Laboratory experiments are designed and carried out. The experimental results agree very well with the theoretical predictions. It is found that the membrane potential of the shaly sands increases with the cation exchange capacity, the hydrocarbon saturation and the salinity difference of the solutions. In addition, the influence of hydrocarbon on the membrane potential is equivalent to a change of the cation exchange capacity of the formation. The electrochemical potential of the shaly sand increases with the increasing hydrocarbon saturation. The developed membrane theory in shaly sands makes an improved SP log interpretation possible. For practical purpose, interpretation graphs calculated based on the developed equations are also presented. Both theoretical and experimental results show that, to calculate Rw from SP in shaly sand, the influences of hydrocarbon saturation and shale content on the spontaneous logs must be taken into account.
机译:地层水电阻率(Rw)是测井解释中最重要的参数之一在Rw计算中使用了自发势或SP测井,这在清洁砂中特别有效。但是,当砂中包含粘土时,粘土会干扰离子扩散过程,从而影响产生的膜电位。由于SP电化学势的主要部分与膜电位有关,因此研究泥质沙中的膜电位以正确确定地层水的电阻率非常重要。由于正离子和负离子的迁移率不同,当两种不同浓度的电解质溶液接触时会产生膜电位。该膜电位还取决于膜的性质或沙子中的页岩含量。在本文中,我们基于电化学理论和导电性特性,对含油泥质砂岩的膜电位进行了系统的研究。设计并进行实验室实验。实验结果与理论预测非常吻合。发现泥质砂岩的膜电位随阳离子交换能力,烃饱和度和溶液盐度差的增加而增大。另外,烃对膜电位的影响等同于地层阳离子交换能力的变化。随着烃饱和度的增加,页岩砂的电化学势也随之增加。泥质砂岩中发达的膜理论使改进的SP测井解释成为可能。出于实际目的,还提供了基于已开发方程式计算的解释图。理论和实验结果均表明,要从泥质砂中的SP计算Rw,必须考虑烃饱和度和页岩含量对自发测井的影响。

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