首页> 外文会议>7th International Symposium on Reservoir Wettability Mar 12-15, 2002 Tasmania Australia >Fluorescence evidence of polar hydrocarbon coating on quartz grains and implications to alteration of reservoir wettability
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Fluorescence evidence of polar hydrocarbon coating on quartz grains and implications to alteration of reservoir wettability

机译:石英颗粒上极性碳氢化合物涂层的荧光证据及其对储层润湿性改变的影响

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摘要

Petrographic analysis of reservoir rocks in apparent water-wet system under UV light indicates the ubiquitous presence of micro-sized oil inclusions within quartz grains. The micro-sized inclusions are often trapped along healed micro-fractures or along quartz overgrowth boundaries. The apertures of the micro-fractures are usually a few microns in width, an order of magnitude smaller than the typical pore aperture (throat) of reservoir rocks. When these same reservoir rocks were analysed using a high sensitive fluorescence spectrophotometer after series of cleaning steps using solvents and oxidizing agents, it was revealed that tightly coated polar organic compounds are present on quartz grain surfaces after a series cleaning steps. Examination of the quartz grain surface using Scanning Electron Microscope (SEM) and an online Energy Dispersive X-ray (EDAX) system confirmed the presence of fine residual hydrocarbon particles associated with clay minerals coated on the highly irregular quartz grain surface. The presence of polar organic compounds and/or asphaltenes on water-wet quartz surfaces provides the pre-requisite for wettability alteration under reservoir condition, which may allow the direct contact between hydrocarbon and the water-wet quartz grains and the formation of micro-size oil inclusions in quartz grains.
机译:在紫外光下,表观水-湿系统中的岩石储层岩石学分析表明,石英晶粒中普遍存在微尺寸油包裹体。微小的夹杂物通常被截留在愈合的微裂缝中或石英的过度生长边界上。微裂缝的孔通常宽度为几微米,比典型的储层岩石孔(喉)孔小一个数量级。在使用溶剂和氧化剂进行一系列清洁步骤后,使用高灵敏度荧光分光光度计分析这些相同的储集岩时,发现在一系列清洁步骤之后,石英颗粒表面存在紧密包覆的极性有机化合物。使用扫描电子显微镜(SEM)和在线能量色散X射线(EDAX)系统对石英颗粒表面进行检查,确认存在与残留在高度不规则石英颗粒表面上的粘土矿物相关的细小残留烃颗粒。水湿石英表面上极性有机化合物和/或沥青质的存在为储层条件下改变润湿性提供了先决条件,这可能允许烃与水湿石英颗粒之间直接接触并形成微尺寸石英颗粒中的油夹杂物。

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