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Influence of stress and formation water properties on velocity sensitivity of lignite reservoir using simulation experiment

机译:应力和地层水性质对褐煤储层速度敏感性的模拟实验

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摘要

To study the velocity sensitivity of a lignite reservoir under different stresses and formation water conditions, orthogonal experiments are performed with pH, salinity, and effective stress as the main factors, and evaluation indexes are extracted at different stages. The effects of the main factors on each index are analyzed by means of range analysis, variance analysis, and effect diagram to study the mechanism of velocity sensitivity in a lignite reservoir. Under a given effective stress condition, the change in lignite permeability with the variation of fluid pressure undergoes three evolutionary stages (stable-rise, decline, and fluctuation) and two effects (sensitization and velocity sensitivity effects) exist. On the basis of the seven evaluation indexes, an evaluation index (D-m) suitable for describing velocity sensitivity damage in the presence of sensitization stage is proposed. Extreme and variance analyses show that salinity is the main factor that controls the lignite sensitization (rise) stage. In the velocity sensitivity (decline) stage, the permeability attenuation rate is controlled by pH and salinity, and the sustained range of velocity sensitivity is affected by pH and effective stress. The fluctuation stage is mainly affected by effective stress. It is analyzed that pH mainly controls the migration and agglomeration of pulverized coal particles through hydrophilicity, and salinity controls the dispersion and agglomeration of pulverized coal particles through the zeta potential generated by an electric double layer. Effective stress influences the sensitivity of lignite reservoir by effecting pore structure.
机译:为了研究褐煤储层在不同应力和地层水条件下的速度敏感性,以pH,盐度和有效应力为主要因素进行正交试验,并提取了不同阶段的评价指标。通过范围分析,方差分析和效果图分析了主要因素对每个指标的影响,以研究褐煤储层的速度敏感性机理。在给定有效应力条件下,褐煤渗透率随流体压力的变化经历了三个演化阶段(稳定上升,下降和波动),并且存在两个效应(敏化效应和速度敏感性效应)。在这七个评价指标的基础上,提出了一种适用于描述感光阶段存在的速度灵敏度损伤的评价指标(D-m)。极端和方差分析表明,盐度是控制褐煤敏化(上升)阶段的主要因素。在速度敏感性(下降)阶段,渗透率衰减率受pH和盐度控制,速度敏感性的持续范围受pH和有效应力影响。波动阶段主要受有效应力影响。分析表明,pH值主要通过亲水性控制粉煤颗粒的迁移和结块,而盐度则通过双电层产生的zeta电位控制粉煤颗粒的分散和结块。有效应力通过影响孔隙结构影响褐煤储层的敏感性。

著录项

  • 来源
    《Fuel》 |2018年第jul15期|579-590|共12页
  • 作者单位

    China Univ Min & Technol Sch Resources & Geosci Xuzhou 221116 Jiangsu Peoples R China|Minist Educ China Key Lab CBM Resources & Dynam Accumulat Proc Xuzhou 221116 Jiangsu Peoples R China;

    Hebei Univ Engn Key Lab Resource Survey & Res Hebei Prov Handan 056038 Peoples R China;

    Suzhou NanZee Sensing TechnologyCo Ltd Suzhou 215123 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Lignite; Velocity sensitivity; pH; Salinity; Effective stress;

    机译:褐煤;速度灵敏度;pH值盐度;有效压力;

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