A Comprehensive Study of Wellbore Stability in Laminated Carbonate Rocks by Nuclear Magnetic Resonance Experiments

H. Kesserwan, Ji Guodong
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Abstract

To counter the consequences of the wellbore instability problems, a thorough analysis of the borehole conditions is performed throughout the entire life-cycle of a hydrocarbon well from planning during the early stages to completion and production. The analysis comprises the following: first, a rigorous understanding of the rock properties e.g. geochemistry and geomechanics mainly the stress magnitudes and rock strength. Second, the mud properties and the entailed interactions with the formation. For instance, numerous borehole failures in laminated rocks have been attributed to the interaction of the drilling/fracturing fluid with the layered-matrix e.g. interaction of water-based-mud with reactive clay minerals. This paper focuses on the impacts of the pore fluids redistribution on wellbore stability in organic rich carbonate rocks. The experimental method consisted of measuring the Nuclear-Magnetic-Resonance transverse relaxation time (NMR T2) on samples saturated by spontaneous imbibition of oil and brine. The wellbore stability was investigated by analyzing the changes in the NMR T2 distribution of each sample after imbibition sequences. The obtained results demonstrated the elevated impacts the wettability and pore structure characteristics on the spatial distribution of the fluids in these rocks. The type of clay content in the bedding planes and its consequent interaction with the drilling mud was identified as a potential driver of the rock instability problems. The discrepancies in the wetting traits were magnified by the presence of fractures that enhanced the network connectivity of both hydrophobic and hydrophilic pores or even across them. Furthermore, the fractures allowed the fluids to surpass the vertical bedding planes and thus accelerating the fluid distribution processes inside the pore space.
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层状碳酸盐岩井筒稳定性的核磁共振综合研究
为了应对井筒不稳定问题的后果,从早期规划到完井和生产,在一口烃井的整个生命周期中,都要对井眼状况进行彻底的分析。分析包括以下内容:首先,严格了解岩石性质,例如地球化学和地质力学,主要是应力大小和岩石强度。其次,泥浆的性质及其与地层的相互作用。例如,在层状岩石中,许多钻孔失败归因于钻井/压裂液与层状基质的相互作用,例如水基泥浆与活性粘土矿物的相互作用。本文重点研究了富有机质碳酸盐岩孔隙流体再分配对井筒稳定性的影响。实验方法是测量油和盐水自吸饱和样品的核磁共振横向弛豫时间(NMR T2)。通过分析吸胀后各样品核磁共振T2分布的变化,研究了井眼稳定性。结果表明,润湿性和孔隙结构特征对岩石中流体的空间分布有较大的影响。层理面中粘土含量的类型及其与钻井泥浆的相互作用被认为是岩石失稳问题的潜在驱动因素。裂缝的存在增强了疏水和亲水孔隙之间甚至是跨孔隙之间的网络连通性,从而放大了润湿特性的差异。此外,裂缝允许流体超越垂直层理平面,从而加速流体在孔隙空间内的分布过程。
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