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Influences of Gamma Ray Irradiation on Thermal Decomposition and Petrophysical Properties of Carbonate Rocks

机译:γ射线辐射对碳酸盐岩热分解及岩石物理性质的影响

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Gamma rays are bursts of high-energy electromagnetic waves that are emitted naturally by some radioactive elements.Laboratory experiments were undertaken to assess the influences of gamma irradiation on thermal decomposition and petrophysical properties of carbonate rocks of aquifers and oil reservoirs.A constant gamma ray dose of 9 MGy was applied on identical calcium carbonate core samples,extracted from actual oil reservoir.The core samples were analyzed using thermogravimetric analysis(TGA),differential thermal analysis(DTA),infrared spectrum(IR)and scanning electron microscope(SEM)before and after application of gamma ray irradiation.The attained data was used to interpret thermal decomposition,phase transition and mechanical stability of calcium carbonate rocks.Furthermore the effect of gamma irradiation on pertophysical properties of porosity and permeability were studied experimentally for water and oil saturated carbonate rocks.Chemical composition of the carbonate core samples was determined using titration method and its sulfur content was determined using precipitation method.Application of Differential Thermal Analysis(DTA)proved the purification of the used core samples.Chemical analysis indicated that the core ha 99.8% calcium carbonate.The Infrared(IR)indicated that no chemical changes of irradiated core samples have been observed.The analysis using DTA and TGA indicated that gamma irradiation enhanced thermal decomposition of carbonate rocks of oil reservoirs.The obtained results indicated that calcium carbonate rocks are stable rocks.In addition,the gamma ray irradiation has been proven to have almost no effect on porosity and permeability of these reservoir rocks.Applications of the attained results are expected to have real impact on deep understanding of rock stability,using gamma ray tools and measuring gamma ray levels in oil fields,and improvements in future interpretation of attained data from gamma ray measurements such as gamma ray log.
机译:伽马射线是由一些放射性元素自然发射的高能电磁波的突发。制造实验是为了评估γ辐射对含水层和油藏碳酸盐岩的热分解和岩石物理性质的影响。常数γ射线剂量施加9米的相同碳酸钙核心样品,从实际储油液中提取。使用热重分析(TGA),差分热分析(DTA),红外光谱(IR)和扫描电子显微镜(SEM)分析核心样品在施用γ射线照射之后。达到的数据用于解释碳酸钙岩石的热分解,相转变和机械稳定性。实验研究水和油饱和碳酸盐的γ辐射对孔隙率和渗透性的术后性质的影响岩石。碳酸盐核样品的化学成分使用滴定法测定S,使用沉淀法测定其硫含量。差分热分析(DTA)的应用证明了使用的核样品的纯化。化学分析表明核酸核碳酸钙99.8%。红外(IR)表明,未观察到辐照核心样品的化学变化。使用DTA和TGA的分析表明,γ辐射增强了碳酸盐储存器的碳酸盐岩的热分解。得到的结果表明,碳酸钙岩石是稳定的岩石。另外,伽玛已经证明,射线照射几乎没有对这些水库岩石的孔隙率和渗透率的影响。达到的结果的应用有望对利用伽马射线工具和油田中测量伽马射线水平来对岩石稳定性的深刻理解产生真正的影响,并改善未来的伽马射线测量达到伽马射线测量数据的解释。

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