{"title":"混合赋存状态天然气水合物储层岩石物理模型","authors":"Cun-Zhi Wu, Feng Zhang, Pin-Bo Ding, Peng-Yuan Sun, Zhi-Guang Cai, Bang-Rang Di","doi":"10.1190/geo2023-0211.1","DOIUrl":null,"url":null,"abstract":"Seismic interpretation of gas hydrates requires the assistance of rock physics. Changes in gas hydrate saturation can alter the elastic properties of formations, and this relationship can be considerably influenced by the occurrence state of gas hydrates. Pore-filling, load-bearing, and cementing types are three single gas hydrate occurrence states commonly considered in rock-physics investigations. However, many gas hydrate-bearing formations are observed to have mixed occurrence states, and their rock-physics properties do not fully conform to models of single occurrence states. We present a generalized rock-physics model for gas hydrate-bearing formations with three mixed occurrence states observed in the field or laboratory experiments: coexisting pore-filling-type and matrix-forming-type gas hydrate (case 1); pore-filling type when S h (gas hydrate saturation) < S c (critical saturation) and pore-filling + matrix-forming type when S h > S c (case 2); and matrix-forming type when S h < S c and matrix-forming + pore-filling type when S h > S c (case 3). Instead of initial porosity, the apparent porosity (the volume fraction of an effective pore filler) φ as represents the influence of occurrence states on the pore space. These three mixed occurrence states can be modeled using a unified workflow, in which the volume fractions of various gas hydrate types are expressed in general forms in terms of the apparent porosity. In addition, the model considers the effect of a pore filler on shear modulus. The proposed model is validated through calibration with real well-log data and published experimental data corresponding to five gas hydrate-bearing formations. The model effectively interprets the influences of gas hydrate saturation and occurrence state on these formations. Thus, the generalized model provides a theoretical basis for the analysis of sensitive elastic parameters and quantitative interpretation for gas hydrate reservoirs.","PeriodicalId":55102,"journal":{"name":"Geophysics","volume":"49 ","pages":"0"},"PeriodicalIF":3.0000,"publicationDate":"2023-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Rock physics model of gas hydrate reservoir with mixed occurrence states\",\"authors\":\"Cun-Zhi Wu, Feng Zhang, Pin-Bo Ding, Peng-Yuan Sun, Zhi-Guang Cai, Bang-Rang Di\",\"doi\":\"10.1190/geo2023-0211.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Seismic interpretation of gas hydrates requires the assistance of rock physics. Changes in gas hydrate saturation can alter the elastic properties of formations, and this relationship can be considerably influenced by the occurrence state of gas hydrates. Pore-filling, load-bearing, and cementing types are three single gas hydrate occurrence states commonly considered in rock-physics investigations. However, many gas hydrate-bearing formations are observed to have mixed occurrence states, and their rock-physics properties do not fully conform to models of single occurrence states. We present a generalized rock-physics model for gas hydrate-bearing formations with three mixed occurrence states observed in the field or laboratory experiments: coexisting pore-filling-type and matrix-forming-type gas hydrate (case 1); pore-filling type when S h (gas hydrate saturation) < S c (critical saturation) and pore-filling + matrix-forming type when S h > S c (case 2); and matrix-forming type when S h < S c and matrix-forming + pore-filling type when S h > S c (case 3). Instead of initial porosity, the apparent porosity (the volume fraction of an effective pore filler) φ as represents the influence of occurrence states on the pore space. These three mixed occurrence states can be modeled using a unified workflow, in which the volume fractions of various gas hydrate types are expressed in general forms in terms of the apparent porosity. In addition, the model considers the effect of a pore filler on shear modulus. The proposed model is validated through calibration with real well-log data and published experimental data corresponding to five gas hydrate-bearing formations. The model effectively interprets the influences of gas hydrate saturation and occurrence state on these formations. 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引用次数: 0
摘要
天然气水合物的地震解释需要岩石物理学的帮助。天然气水合物饱和度的变化会改变地层的弹性性质,这种关系受天然气水合物赋存状态的影响较大。孔隙充填型、承载型和胶结型是岩石物理研究中通常考虑的三种单一天然气水合物赋存状态。然而,许多含天然气水合物地层具有混合赋存状态,其岩石物理性质并不完全符合单一赋存状态模型。本文提出了一种具有三种混合赋存状态的含天然气水合物地层的广义岩石物理模型:孔隙填充型和基质形成型天然气水合物共存(案例1);S h(天然气水合物饱和度)<时的孔隙填充类型;S c(临界饱和度)和S h >时孔隙填充+基质形成型;S c(情况2);S h <时为基体形成型;S h >时S c与成基+充孔型;表观孔隙率(有效孔隙填料的体积分数)φ as表示赋存状态对孔隙空间的影响,而不是初始孔隙率。这三种混产状态可以使用统一的工作流程进行建模,其中各种天然气水合物类型的体积分数用表观孔隙度的一般形式表示。此外,该模型还考虑了孔隙填料对剪切模量的影响。通过实际测井资料和已发表的5个含天然气水合物地层的实验数据进行标定,验证了该模型的有效性。该模型有效地解释了水合物饱和度和赋存状态对这些地层的影响。为天然气水合物储层弹性敏感参数分析和定量解释提供了理论依据。
Rock physics model of gas hydrate reservoir with mixed occurrence states
Seismic interpretation of gas hydrates requires the assistance of rock physics. Changes in gas hydrate saturation can alter the elastic properties of formations, and this relationship can be considerably influenced by the occurrence state of gas hydrates. Pore-filling, load-bearing, and cementing types are three single gas hydrate occurrence states commonly considered in rock-physics investigations. However, many gas hydrate-bearing formations are observed to have mixed occurrence states, and their rock-physics properties do not fully conform to models of single occurrence states. We present a generalized rock-physics model for gas hydrate-bearing formations with three mixed occurrence states observed in the field or laboratory experiments: coexisting pore-filling-type and matrix-forming-type gas hydrate (case 1); pore-filling type when S h (gas hydrate saturation) < S c (critical saturation) and pore-filling + matrix-forming type when S h > S c (case 2); and matrix-forming type when S h < S c and matrix-forming + pore-filling type when S h > S c (case 3). Instead of initial porosity, the apparent porosity (the volume fraction of an effective pore filler) φ as represents the influence of occurrence states on the pore space. These three mixed occurrence states can be modeled using a unified workflow, in which the volume fractions of various gas hydrate types are expressed in general forms in terms of the apparent porosity. In addition, the model considers the effect of a pore filler on shear modulus. The proposed model is validated through calibration with real well-log data and published experimental data corresponding to five gas hydrate-bearing formations. The model effectively interprets the influences of gas hydrate saturation and occurrence state on these formations. Thus, the generalized model provides a theoretical basis for the analysis of sensitive elastic parameters and quantitative interpretation for gas hydrate reservoirs.
期刊介绍:
Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics.
Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research.
Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring.
The PDF format of each Geophysics paper is the official version of record.