电磁加热作用下地层岩石性质变化的实验研究

Lanxiao Hu, H. Li, T. Babadagli
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引用次数: 5

摘要

电磁加热因其对环境的友好性而被提出用于重油的回收。以往的研究主要集中在研究这种非水方法的可行性和提高采收率方面。然而,电磁加热对地层岩石性质变化的影响仍然是难以捉摸的。为了了解电磁加热对改变地层岩石物理性质的影响,需要进行详细的实验/测量。采用商用微波炉进行电磁加热实验。研究了不同类型的地层岩石(页岩、beria -砂岩、致密砂岩和indiana -碳酸盐岩)。各种技术,包括扫描电镜(SEM)、能量色散x射线(EDX)、N2吸附/解吸和x射线荧光(XRF),用于表征实验前后页岩样品的性质。对Berea砂岩、致密砂岩和Indiana碳酸盐岩进行了孔隙度和渗透率测量。红外温度计用来测量样品的表面温度。此外,还进行了电炉加热实验,以区分导电加热和电磁加热对岩样性质变化的影响。结果表明:不同类型岩石对电磁加热的响应不同;与砂岩和碳酸盐相比,页岩样品表现出更高的温度,因为粘土和黄铁矿具有更好的EM能量吸收。页岩样品经电磁加热后破碎或破裂,而砂岩和碳酸盐样品经电磁加热后基本保持不变。SEM结果表明,EM加热导致了黏土的拉伸破坏、收缩和挥发性有机物向页岩样品的释放。N2吸附/解吸实验表明,粘土收缩导致孔隙体积显著增大,而EM加热后转化的沥青干酪根会堵塞部分孔隙。由于石英和方解石对电磁波的透明,EM加热对Berea砂岩和Indiana碳酸盐几乎没有影响。然而,由于电磁加热使孔隙压力迅速上升,使饱和水致密砂岩发生破裂。
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Property Changes of Formation Rocks under Electromagnetic Heating: An Experimental Study
Electromagnetic (EM) heating has been proposed to recover heavy oil due to its great environmental friendliness. Previous studies focused on investigating the feasibility and enhancing the oil recovery of such non-aqueous method. However, the effect of EM heating on the variations of formation rock properties is still elusive. Detailed experiments/measurements are required to understand the effect of EM heating on changing the petrophysical properties of formation rocks. A commercial microwave oven is used to conduct the EM heating experiments. Different types of formation rocks (shale, Berea-sandstone, tight sandstone, and Indiana-carbonate) are investigated. Various techniques, including scanning electron microscopy (SEM), energy dispersive X-ray (EDX), N2 adsorption/desorption, and X-Ray fluorescence (XRF), are used to characterize the properties of shale samples before/after experiments. The porosity and permeability measurement are performed to Berea sandstone, tight sandstone, and Indiana carbonate. An infrared thermometer is used to measure the samples’ surface temperatures. Furthermore, oven-heating experiments are conducted to distinguish the effects of conductive-heating and EM heating on the property changes of rock-samples. Results show that different types of rocks exhibit different responses to EM heating; shale samples exhibit a higher temperature compared with sandstone and carbonate because of the better EM energy absorbance of clays and pyrite. The shale samples are crumbled into pieces or fractured after EM heating, while the sandstone and carbonate samples remain almost unchanged after EM heating. The SEM results reveal that EM heating causes tensile failure, shrinkage of clay, and release of volatile organic content to the shale sample. The N2 adsorption/desorption measurements demonstrate that the pore volume significantly increases due to clay shrinkage, while part of the pore can be blocked by the converted bituminous kerogen after EM heating. EM heating has almost no effect on Berea sandstone and Indiana carbonate due to the transparency of quartz and calcite to EM waves. However, the EM heating can fracture the tight sandstone that is saturated with water because of the rapid rise of pore pressure under EM heating.
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