Estimating nuclear magnetic resonance transverse surface relaxivity in pre-salt carbonates of the Santos Basin, Brazil

IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Marta H. Jácomo , Gelvam A. Hartmann , Everton Lucas-Oliveira , Daniel Rojas , Emilson P. Leite
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引用次数: 0

Abstract

This study explores the Nuclear Magnetic Resonance (NMR) characteristics of pre-salt carbonates rocks, focusing on transverse relaxation time (T₂) cut off values and surface relaxivity parameters. We analyzed nine carbonate samples to capture the petrophysical heterogeneity of the Barra Velha and Itapema Formations in the Santos Basin, Brazil. By relating NMR T₂ with the surface-area-to-volume (S/V) ratio, surface relaxivity was determined using Mercury Injection Capillary Pressure (MICP) and X-ray microcomputed tomography (μCT) to enhance pore size estimation. Based on NMR results, samples were grouped into three categories: Group 1 (Samples A, B2, B3, C, D2, D3, E): T₂ peaks above the cut off, dominated by macropores; Group 2 (Sample B1): Bimodal T₂ distribution, indicating a mix of macro- and micropores; Group 3 (Sample D1): T₂ peaks below the cut off, suggestive of micropore dominance and irreducible fluid storage. The study observes that while these patterns are not sufficient for distinguishing facies types, a comparative analysis of MICP pore-throat sizes and NMR T₂ distributions reveals essential insights into pore system variability. Notably, larger dissolution-related pores in Samples A (coquina) and D2 (spherulitic shrubstone) affect permeability estimation. The maximum T₂ cut off for spherulitic shrubstones was 0.65 s, highlighting the significance of pore structure in fluid storage and transport. Additionally, results underscore the vital role of surface relaxivity in converting T₂ to pore size, showing that relaxivity is more influenced by rock morphology and texture processes than solely by iron composition such as presence of coatings or presence of vuggy or cavities. Incorporating relaxivity into NMR models significantly improved permeability estimation accuracy, with the ρ-corrected model (R2 = 0.84) outperforming traditional SDR and TIM models. These findings emphasize the necessity of integrating NMR, MICP, and μCT techniques for a comprehensive understanding of pore architecture and fluid flow in heterogeneous carbonate reservoirs.
巴西Santos盆地盐下碳酸盐岩核磁共振横向表面弛豫度估算
研究了盐下碳酸盐岩的核磁共振(NMR)特征,重点研究了横向弛豫时间(T₂)截断值和表面弛豫参数。为了捕捉巴西Santos盆地Barra Velha和Itapema地层的岩石物理非均质性,研究人员分析了9个碳酸盐样品。通过将核磁共振T₂与表面积体积比(S/V)联系起来,利用压汞毛细管压力(MICP)和x射线微计算机断层扫描(μCT)来确定表面弛豫度,以增强孔径估计。根据核磁共振结果,将样品分为三类:第一类(样品A、B2、B3、C、D2、D3、E):截断点以上的t2峰,以大孔隙为主;第2组(样品B1):双峰T₂分布,表明宏观和微观孔隙混合;第3组(样品D1):截断线以下的T 2峰,提示微孔优势和不可还原的流体储存。研究发现,虽然这些模式不足以区分相类型,但对MICP孔喉大小和NMR T₂分布的比较分析揭示了孔隙系统变异性的基本见解。值得注意的是,样品A (coquina)和D2(球晶灌木)中较大的溶解相关孔隙影响了渗透率的估计。球晶灌木的最大T₂截断值为0.65 s,突出了孔隙结构在流体储存和输送中的重要性。此外,结果强调了表面弛豫度在将T₂转化为孔隙大小方面的重要作用,表明弛豫度更多地受到岩石形态和纹理过程的影响,而不仅仅是铁成分(如涂层或空洞或空腔的存在)的影响。在核磁共振模型中加入弛豫度显著提高了渗透率估计精度,ρ校正模型(R2 = 0.84)优于传统的SDR和TIM模型。这些发现强调了综合NMR、MICP和μCT技术对非均质碳酸盐岩储层孔隙结构和流体流动的必要性。
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来源期刊
Journal of Applied Geophysics
Journal of Applied Geophysics 地学-地球科学综合
CiteScore
3.60
自引率
10.00%
发文量
274
审稿时长
4 months
期刊介绍: The Journal of Applied Geophysics with its key objective of responding to pertinent and timely needs, places particular emphasis on methodological developments and innovative applications of geophysical techniques for addressing environmental, engineering, and hydrological problems. Related topical research in exploration geophysics and in soil and rock physics is also covered by the Journal of Applied Geophysics.
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