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Joint inversion with prestack waveform and spectral information for layered media 层状介质叠前波形与谱信息联合反演
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.06.004
Zheng-Yang Kuai, Dan-Ping Cao, Chao Jin
Subsurface reservoirs commonly exhibit layered structures. Conventional amplitude variation with angle (AVA) inversion, which relies on the Zoeppritz equation and its approximations, often fails to accurately estimate elastic parameters because it assumes single-interface models and ignores multiple reflections and transmission losses. To address these limitations, this study proposes a novel prestack time-frequency domain joint inversion method that utilizes the reflection matrix method (RMM) as the forward operator. The RMM accurately simulates wave propagation in layered media, while the joint inversion framework minimizes the misfit between observed and synthetic data in both the time and frequency domains. By incorporating Bayesian theory to optimize the inversion process, the method effectively balances contributions from both time-domain waveforms and frequency-domain spectral information through a weighting factor. Tests on both synthetic data and field data demonstrate that the proposed method outperforms conventional AVA inversion and time-domain waveform inversion in accuracy and robustness. Furthermore, the method demonstrates good robustness against variations in initial models, random noise, and coherent noise interference. This study provides a practical and effective approach for high-precision reservoir characterization, with potential applications in complex layered media.
地下储层通常表现为层状结构。传统的振幅随角度变化(AVA)反演依赖于Zoeppritz方程及其近似,由于其假设为单界面模型,忽略了多重反射和透射损失,往往无法准确估计弹性参数。为了解决这些限制,本研究提出了一种新的叠前时频域联合反演方法,利用反射矩阵法(RMM)作为正演算子。RMM精确地模拟了波在层状介质中的传播,而联合反演框架在时域和频域上最大限度地减少了观测数据与合成数据之间的不匹配。该方法结合贝叶斯理论优化反演过程,通过加权因子有效平衡时域波形和频域频谱信息的贡献。实验结果表明,该方法在精度和鲁棒性上均优于传统的AVA反演和时域波形反演。此外,该方法对初始模型的变化、随机噪声和相干噪声干扰具有良好的鲁棒性。该研究为高精度储层表征提供了一种实用有效的方法,在复杂层状介质中具有潜在的应用前景。
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引用次数: 0
Study on the synergistic effects of dynamic impact damage and acid etching treatment on the mechanical properties and pore characteristics of shale 动态冲击损伤与酸蚀处理对页岩力学性能和孔隙特征的协同效应研究
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.07.011
Mao Jing, Kang Peng, Tao Wu, Han-Kuo Zhang, Si-Yu Gao
The low porosity and low permeability of shale remain the primary challenges in shale gas exploitation. Traditional single permeability enhancement techniques have shown limited efficacy, failing to effectively address these technical bottlenecks. This study investigates the synergistic effects of perforation-induced permeability enhancement and acidizing operations on the mechanical properties and micro-pore structure of shale. The improved Split Hopkinson Pressure Bar (SHPB) technique was employed to simulate dynamic impact damage under triaxial stress conditions. Damaged and undamaged rock specimens were immersed in a 15% hydrochloric acid solution to fabricate combined-damage specimens and acid-etched specimens with varying damage states. Uniaxial compression tests, X-ray diffraction (XRD) analysis, and scanning electron microscopy (SEM) were conducted on these specimens. SEM images were binarized, and combined with low-temperature nitrogen adsorption tests, the effects of different damage states on the mechanical behavior, energy dissipation, micro-morphology, and pore characteristics of shale were systematically evaluated. Results demonstrate that the peak stress and elastic modulus of shale exhibit a negative correlation with acid-etching duration. The mechanical properties of combined-damage specimens are inferior to those of pure acid-etched specimens, with the minimum peak stress reaching 147.10 MPa—a 43.53% reduction compared to untreated specimens. The energy dissipation ratio significantly increases, with a maximum value of 34.74%. XRD analysis reveals that prolonged acid immersion effectively reduces the carbonate content in specimens, while composite treatment accelerates the reaction between rock matrix and acid solution. Microstructural characterization indicates that acid etching enhances the porosity of shale, particularly the area of mesopores and macropores, with more pronounced pore development and a fragmented interface structure. These findings deepen the understanding of physical mechanisms during shale gas extraction and provide critical theoretical support for optimizing integrated permeability enhancement technologies.
页岩低孔低渗是页岩气开发面临的主要挑战。传统的单一增渗技术效果有限,无法有效解决这些技术瓶颈。研究了射孔增渗和酸化作业对页岩力学性能和微孔结构的协同效应。采用改进的劈裂霍普金森压杆(Split Hopkinson Pressure Bar, SHPB)技术模拟了三轴应力条件下的动态冲击损伤。将损伤和未损伤岩石试样浸泡在15%盐酸溶液中,制作不同损伤状态的复合损伤试样和酸蚀试样。对试样进行了单轴压缩试验、x射线衍射(XRD)分析和扫描电镜(SEM)分析。通过对SEM图像进行二值化处理,结合低温氮气吸附试验,系统评价了不同损伤状态对页岩力学行为、能量耗散、微观形貌和孔隙特征的影响。结果表明,页岩的峰值应力和弹性模量与酸蚀时间呈负相关。复合损伤试样的力学性能不如纯酸蚀试样,最小峰值应力达到147.10 mpa,比未经酸蚀处理的试样降低43.53%。能量耗散比显著增大,最大值为34.74%。XRD分析表明,长时间的酸浸有效降低了试样中的碳酸盐含量,而复合处理则加速了岩石基质与酸溶液的反应。微观结构表征表明,酸蚀作用增强了页岩孔隙度,特别是中孔和大孔的面积,孔隙发育更加明显,界面结构破碎。这些发现加深了对页岩气开采物理机制的理解,并为优化综合增渗技术提供了重要的理论支持。
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引用次数: 0
A novel fusion of interpretable boosting algorithm and feature selection for predicting casing damage 一种新的融合可解释增强算法和特征选择的套管损伤预测方法
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.08.011
Juan Li , Mandella Ali M. Fargalla , Wei Yan , Zi-Xu Zhang , Wei Zhang , Zi-Chen Zou , Tang Qing , Tao Yang , Chao-Dong Tan , Guang-Cong Li
Casing damage resulting from sand production in unconsolidated sandstone reservoirs can significantly impact the average production of oil wells. However, the prediction task remains challenging due to the complex damage mechanism caused by sand production. This paper presents an innovative approach that combines feature selection (FS) with boosting algorithms to accurately predict casing damage in unconsolidated sandstone reservoirs. A novel TriScore FS technique is developed, combining mRMR, Random Forest, and F-test. The approach integrates three distinct feature selection approaches—TriScore, wrapper, and hybrid TriScore-wrapper and four interpretable Boosting models (AdaBoost, XGBoost, LightGBM, CatBoost). Moreover, shapley additive explanations (SHAP) was used to identify the most significant features across engineering, geological, and production features. The CatBoost model, using the Hybrid TriScore-rapper G1G2 FS method, showed exceptional performance in analyzing data from the Gangxi Oilfield. It achieved the highestaccuracy (95.5%) and recall rate (89.7%) compared to other tested models. Casing service time, casing wall thickness, and perforation density were selected as the top three most important features. This framework enhances predictive robustness and is an effective tool for policymakers and energy analysts, confirming its capability to deliver reliable casing damage forecasts.
松散砂岩储层出砂造成的套管损坏会严重影响油井的平均产量。然而,由于出砂造成的复杂破坏机制,预测任务仍然具有挑战性。本文提出了一种结合特征选择(FS)和提升算法的创新方法,以准确预测松散砂岩储层的套管损坏。结合mRMR、随机森林和f检验,开发了一种新颖的TriScore FS技术。该方法集成了三种不同的特征选择方法——triscore、wrapper和混合TriScore-wrapper,以及四种可解释的boost模型(AdaBoost、XGBoost、LightGBM、CatBoost)。此外,shapley加性解释(SHAP)用于识别工程、地质和生产特征中最重要的特征。CatBoost模型采用混合TriScore-rapper G1G2 FS方法,在分析港西油田的数据时表现出色。与其他测试模型相比,它达到了最高的准确率(95.5%)和召回率(89.7%)。套管使用时间、套管壁厚度和射孔密度被认为是最重要的三个特征。该框架增强了预测的稳健性,是政策制定者和能源分析师的有效工具,证实了其提供可靠套管损坏预测的能力。
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引用次数: 0
TOC TOC
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/S1995-8226(25)00383-8
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引用次数: 0
Surface erosion thickness and oxygen isotope of the Early Jurassic lake water in northern Sichuan Basin, evidence from clumped isotopes of shell limestones 四川盆地北部早侏罗世湖水表面侵蚀厚度与氧同位素——来自壳灰岩团块同位素的证据
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.05.030
Ping-Ping Li , Shi-Jie He , Zhan-Jie Xu , Dai-Qin Jiang , Hua-Yao Zou , Fang Hao
Oxygen isotope (δ18O) of paleolake water is a key indicator for reconstructing the formation temperature and diagenetic history of lacustrine carbonate minerals. In this study, we use clumped isotopes (Δ47) of lacustrine shell limestones to determine the surface erosion thickness and δ18O of Early Jurassic lake water in the northern Sichuan Basin. We analyzed nine shell limestone and seventeen shale samples from the Early Jurassic Da'anzhai Member (J1z4) in the Yuanba area. Whether the shell's shapes are well or partially preserved, the J1z4 shell limestones in the Yuanba area show no significant recrystallization and dull cathodoluminescence. These characteristics suggest that the shell limestones did not undergo significant diagenetic alteration during late burial. The Δ47 values of the J1z4 shell limestones range from 0.448 ± 0.005‰ to 0.463 ± 0.006‰, yielding clumped isotope temperature (TΔ47) of 64.4 ± 0.8 to 69.7 ± 1.4 °C, which is significantly higher than the Early Jurassic paleotemperature. It suggests that the Δ47 of shell limestones was altered by solid-state reordering, meaning the TΔ47 does not reflect the initial formation temperatures. By integrating organic matter's maturation model (Easy%Ro) of coexisting shales with Δ47 solid-state reordering model of calcite, we constrained the maximum burial temperature (∼170 °C) and the initial formation temperature (∼28 °C) of these shell limestones. Based on reported paleotemperature gradient, we estimated that the surface erosion thickness was about 1500 m. Furthermore, using the determined initial formation temperatures and conventional oxygen isotope thermometer, we determined that the δ18O values of the Early Jurassic lake water in the Sichuan Basin, which ranged from −10.8‰ to −8.0‰ (SMOW). The reconstructed paleotemperature and δ18O of lake water suggest that the Early Jurassic in the Sichuan Basin was warm and humid, which was favorable for the deposition of organic-rich lacustrine shale. The methods developed in this study, which employ Δ47 of shell limestones to reconstruct the maximum burial temperature and paleolake environmental conditions, demonstrate broad applicability to the Sichuan Basin and similar lacustrine basins.
古湖泊水体氧同位素(δ18O)是重建湖泊碳酸盐矿物形成温度和成岩历史的关键指标。本研究利用湖壳灰岩的团块同位素(Δ47)测定了川北早侏罗世湖水的地表侵蚀厚度和δ18O。对元坝地区早侏罗世大安寨段(J1z4) 9个壳灰岩和17个页岩样品进行了分析。元坝地区J1z4壳灰岩无论壳形保存完好还是部分保存完好,其再结晶不明显,阴极发光较暗。这些特征表明,壳灰岩在晚埋藏时期未发生明显的成岩蚀变。J1z4壳灰岩Δ47值范围为0.448±0.005‰~ 0.463±0.006‰,块状同位素温度(TΔ47)为64.4±0.8 ~ 69.7±1.4℃,明显高于早侏罗世古地温。这表明壳灰岩的Δ47被固态重排序改变了,这意味着TΔ47不能反映初始形成温度。通过将共存页岩有机质成熟模型(Easy%Ro)与方解石的Δ47固态重排序模型相结合,限定了这些壳灰岩的最高埋藏温度(~ 170℃)和初始形成温度(~ 28℃)。根据已有的古温度梯度,我们估计地表侵蚀厚度约为1500 m。利用测定的初始地层温度和常规氧同位素温度计,确定了四川盆地早侏罗世湖水的δ18O值为- 10.8‰~ - 8.0‰(SMOW)。重建的古地温和湖水δ18O值表明,四川盆地早侏罗世温暖湿润,有利于富有机质湖相页岩的沉积。本研究利用壳灰岩Δ47重建最高埋藏温度和古湖泊环境条件的方法,对四川盆地和类似的湖泊盆地具有广泛的适用性。
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引用次数: 0
Flow characteristics of shale oil and their geological controls: A case study of the Lucaogou Formation in the Jimsar Sag, Junggar Basin 页岩油流动特征及其地质控制因素——以准噶尔盆地吉木萨尔凹陷芦草沟组为例
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.06.012
Jia-Qi Liu , Jun-Qian Li , Zhao-Jing Song , An-Chao Shen
The Lucaogou Formation in Jimsar has a significant development potential due to its massive shale oil resources. Nevertheless, the complex and heterogeneous lithology, coupled with unclear flow mechanisms, poses a challenge in effectively predicting its development potential. Therefore, it is crucial to clarify the flow characteristics of shale oil and its controlling factors. In this study, we used a flow simulation experiment to investigate the flow characteristics of different samples under various temperatures and confining stresses and quantitatively evaluated flow characteristics using threshold pressure gradient and total loss of flow rate. Additionally, by combining scanning electron microscopy and mercury intrusion capillary pressure techniques for pore structure characterization, and the relationship between microscopic pore structure and flow parameters was discussed. The findings indicate that rock composition and pore throat structure collaboratively control shale oil flow. Mesopores and macropores primarily develop between dolomite or albite, leading to well-developed pore throat structure with larger average throat radius, lower displacement pressure, and better reservoir quality, enhancing shale oil flowability. Dolomitic siltstone often exhibits these characteristics, making it a favorable lithology for shale oil flow. This study reveals the flow mechanism of shale oil under the action of reservoir physical properties, material compositions, temperatures and confining stresses, summarizes the geological characteristics of advantageous reservoirs. It provides theoretical support for layer selection and efficient development of shale oil reservoirs in the Lucaogou Formation of the Jimsar.
吉木萨尔芦草沟组页岩油资源丰富,开发潜力巨大。然而,复杂的非均质岩性,加上不明确的流动机制,给有效预测其开发潜力带来了挑战。因此,弄清页岩油的流动特征及其控制因素至关重要。在本研究中,我们通过流动模拟实验研究了不同温度和围应力下不同样品的流动特性,并利用阈值压力梯度和总损失流量定量评价了流动特性。此外,结合扫描电镜和压汞毛细管压力技术对孔隙结构进行表征,探讨微观孔隙结构与流动参数的关系。研究结果表明,岩石成分和孔喉结构共同控制着页岩油的流动。中孔和大孔主要发育在白云岩或钠长岩之间,孔喉结构发育,平均喉道半径大,驱油压力低,储层质量好,提高了页岩油的流动性。白云岩粉砂岩往往表现出这些特征,是页岩油流动的有利岩性。揭示了页岩油在储层物性、物质组成、温度和围应力作用下的渗流机理,总结了有利储层的地质特征。为吉木萨尔芦草沟组页岩油储层的优选和高效开发提供了理论支持。
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引用次数: 0
Thermal maturity effect on the microscopic pore structure and gas adsorption capacity of shale gas reservoirs: A review 热成熟度对页岩气藏微观孔隙结构和气体吸附能力的影响研究进展
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.07.023
Wei-Dong Xie , Xiao-Fei Fu , Hai-Xue Wang , Yu Sun , Veerle Vandeginste , Xiao-Peng Li
Organic matter (OM) is the primary gas occurrence carrier in shale reservoirs due to their abundant nanopores. To reveal the OM pore structure, adsorption capacity and evolution during thermal maturation, this study collected data from samples spanning the entire evolution stage, from immature to over-mature. Scanning Electron Microscope (SEM) observation and low temperature gases adsorption experiments were used to qualitatively-semi-quantitatively and quantitatively analyze OM pore structure evolution, and CH4 isothermal adsorption experiments were used to reveal the adsorption capacity evolution. Then, the influence and mechanism of maturity and hydrocarbon generation on pore development and adsorption capacity were quantitatively reviewed based on the experimental data. The results show that OM pores are poorly developed in the immature stage due to weak hydrocarbon generation, although micro-fractures are occasionally found at the edges of OM particles. In the low maturity stage, OM pores are partially developed due to liquid hydrocarbon generation, with liquid hydrocarbons also filling some OM pores. The contribution of total organic carbon content (TOC) to adsorption extent is not significant in these two stages. From high to high-over maturity stages, massive gaseous hydrocarbons are generated, significantly improving the surface porosity of OM. Clear positive linear correlations are observed between TOC and adsorption amount. However, the development of OM pores significantly declines when thermal maturity (Ro) exceeds 3.5% due to excessive aromatization. The accuracy of research on the evolution of pore structure and adsorption capacity is limited by several factors: (i) errors caused by sample specification, calculation processes, parameter settings, and kerogen models in isothermal adsorption experiments and molecular simulations; (ii) difficulty in achieving control variables due to the strong heterogeneity of natural maturation shale samples; and (iii) the need to enhance compatibility between thermal simulation experiments and natural thermal evolution. Therefore, isothermal adsorption experiments on bulk shale and molecular simulations of intact shale model are necessary, taking into account the dynamic temperature and pressure of in-situ reservoirs. Moreover, shale samples with varying maturity, influenced by their distance from the paleo-thermal source, may provide significant verification for thermal simulation experiments.
有机质由于具有丰富的纳米孔隙,是页岩储层天然气赋存的主要载体。为了揭示有机质在热成熟过程中的孔隙结构、吸附能力和演化过程,本研究收集了从未成熟到过成熟整个演化阶段的样品数据。采用扫描电镜(SEM)观察和低温气体吸附实验对OM孔隙结构进行定性-半定量和定量分析,采用CH4等温吸附实验揭示吸附容量演化。在此基础上,定量评述了成熟度和生烃对孔隙发育和吸附能力的影响及其机理。结果表明:未成熟阶段有机质孔隙发育较差,生烃能力较弱,但在有机质颗粒边缘偶见微裂缝;在低成熟阶段,由于液态烃的生烃作用,部分有机质孔隙发育,液态烃也充填了部分有机质孔隙。总有机碳含量(TOC)对吸附程度的贡献在两个阶段均不显著。从高成熟度阶段到高过成熟度阶段,大量气态烃生成,显著提高了OM的表面孔隙度。TOC与吸附量呈明显的线性正相关。然而,当热成熟度(Ro)超过3.5%时,由于过度芳构化,OM孔的发育明显下降。在等温吸附实验和分子模拟中,由于样品规格、计算过程、参数设置、干酪根模型等因素造成的误差,限制了孔隙结构和吸附能力演化研究的准确性;(ii)由于天然成熟页岩样品的非均质性强,难以获得控制变量;(三)需要加强热模拟实验与自然热演化的兼容性。因此,考虑原位储层动态温度和动态压力,有必要开展块状页岩等温吸附实验和完整页岩模型分子模拟。此外,不同成熟度的页岩样品受离古热源距离的影响,可为热模拟实验提供重要的验证。
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引用次数: 0
OFC 离岸金融中心
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/S1995-8226(25)00381-4
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引用次数: 0
Hydraulic fracturing induced casing deformation and fault activation: from single-well fracturing to well-factory fracturing 水力压裂引起套管变形和断层活化:从单井压裂到井厂压裂
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.07.014
Yu-Ting He , Yin-Tong Guo , Yun Jiang , Xin Chang , Yu-Xiang Jing , Ming-Nan Xu , Chun-He Yang
Hydraulic fracturing-induced casing deformation and fault activation have greatly hindered the safe and efficient development of shale oil and gas resources. In this study, statistical analysis, physical tests, and numerical simulation methods are used to comprehensively analyze hydraulic fracturing-induced fault activation and casing deformation processes. This study is based on the Longmaxi Formation of LZ block, a deep shale gas reservoir in the southwest Sichuan Basin (China), as a geological background. A large amount of field data on fracturing from the LZ Block is counted, and the main influencing factors are analyzed. The main factors of hydraulic fracturing-induced fault slip are (from strong to weak) parameters related to fluid injection volume, parameters related to segments and clusters, and parameters related to injection rate. Combined with physical experiments and numerical simulations, the fault activation law during fracturing has been studied. The degree of casing deformation and fault slip are linearly correlated. For hydraulic fractures to cross faults is very difficult, fault activation and casing deformation can only be mitigated as much as possible. We find that the number of clusters per segment and the injection rate are negatively correlated with the fault slip distance. Reducing the fluid injection volume can mitigate the fault slip distance. Therefore, low injection rates, low fluid volumes, and more clusters per segment are recommended for fracturing in high-risk segments. It is important to note that the scale and risk of fault activation induced by well-factory fracturing is much higher compared to single-well fracturing. In situations with extremely high risk, the injection volume should preferably not exceed 800 m3 to minimize the risk of geological and casing deformation.
水力压裂引起的套管变形和断层活化严重阻碍了页岩油气资源的安全高效开发。本研究采用统计分析、物理试验和数值模拟等方法,综合分析水力压裂诱发断层活化和套管变形过程。本研究以四川盆地西南部陆岭地块龙马溪组深层页岩气储层为地质背景。对LZ区块的大量现场压裂数据进行了统计,分析了影响压裂效果的主要因素。水力压裂诱发断层滑移的主要影响因素依次为注液量相关参数(由强到弱)、段段和簇段相关参数和注液速率相关参数。结合物理实验和数值模拟,研究了压裂过程中断层活化规律。套管变形程度与断层滑移呈线性相关。水力裂缝穿越断层非常困难,只能尽可能地减轻断层活化和套管变形。我们发现每段的簇数和注入速度与断层滑动距离呈负相关。减小注液量可以减小断层滑动距离。因此,对于高风险段的压裂,建议采用低注入速率、低流体体积和每段更多的压裂簇。值得注意的是,与单井压裂相比,井厂压裂引起的断层活化的规模和风险要高得多。在风险极高的情况下,注入量最好不要超过800 m3,以尽量减少地质和套管变形的风险。
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引用次数: 0
Finite-difference simulation of elastic waves in fluid-solid coupled media with irregular interface 不规则界面流固耦合介质弹性波的有限差分模拟
IF 6.1 1区 工程技术 Q2 ENERGY & FUELS Pub Date : 2025-10-01 DOI: 10.1016/j.petsci.2025.06.017
Xu-Hui Zhou , Yi-Yuan Wang , Shou-Dong Huo
The finite-difference method (FDM) is an essential tool in exploration geophysics, particularly for simulating wave propagation in fluid-solid coupled media. Despite its widespread use, FDM faces significant challenges that affect its accuracy and efficiency. Firstly, the implicit handling of fluid-solid boundary conditions through parameter averaging strategy often results in low simulation accuracy. Secondly, surface topography can introduce staircase diffraction noise when grid spacing is large. To address these issues, this paper presents a novel approach. We derive an implicit expression for fluid-solid boundary conditions based on average medium theory, translating explicit boundary conditions into model parameter modification. This enables implicit handling of fluid-solid boundaries by modifying the parameters near the boundary. Furthermore, to mitigate staircase diffraction noise, we employ multiple interface discretization based on the superposition method. This effectively suppresses staircase diffraction noise without requiring grid refinement. The efficacy of our method in accurately modeling wave propagation phenomena in fluid-solid coupled media is demonstrated by numerical examples. Results align well with those obtained using the spectral element method (SEM), with significant reduction in staircase diffraction noise.
有限差分法(FDM)是勘探地球物理的重要工具,特别是用于模拟流固耦合介质中的波传播。尽管FDM得到了广泛的应用,但它仍然面临着影响其精度和效率的重大挑战。首先,采用参数平均策略隐式处理流固边界条件往往导致仿真精度低。其次,当网格间距较大时,表面形貌会引入阶梯衍射噪声。为了解决这些问题,本文提出了一种新的方法。基于平均介质理论推导了流固边界条件的隐式表达式,将显式边界条件转化为模型参数修正。这样可以通过修改边界附近的参数来隐式处理流固边界。此外,为了消除阶梯衍射噪声,我们采用了基于叠加法的多界面离散化方法。这有效地抑制了阶梯衍射噪声而不需要网格细化。数值算例表明,该方法能准确模拟流固耦合介质中的波传播现象。结果与用谱元法(SEM)得到的结果一致,显著降低了阶梯衍射噪声。
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引用次数: 0
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Petroleum Science
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