基于纳米压痕的非均质性页岩基质力学尺度效应研究
批准号:
52104075
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
张成朋
依托单位:
学科分类:
矿山开采基础理论
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
张成朋
中文摘要
页岩基质力学精细表征是我国页岩气大规模高效开发的前提,目前学者普遍采用宏观力学实验开展页岩力学变形与破坏机理研究,忽略了矿物成分及微观结构强非均质性的影响。鉴于此,本项目将通过分子动力学模拟、压痕试验、三维有限元数值仿真和理论分析等手段开展非均质性页岩基质微观力学特性及其尺度效应研究。构建页岩基质矿物纳米压痕的分子动力学模型,揭示页岩矿物颗粒变形机制,建立纳观尺度基质矿物弹塑性力学本构关系。开展页岩基质靶向微、纳米压痕实验,验证基质矿物力学本构关系,分析非均质性页岩微观力学特性的主控因素。基于页岩数字岩芯和纳观力学本构关系建立三维有限元数值仿真模型,实现跨尺度压痕实验反演分析,提出基于页岩基质矿物组织结构非均质性特征和微观力学参数的力学多尺度升级模型,探明页岩基质力学特性尺寸依赖演化规律。研究结果能够揭示非均质页岩基质的力学变形机制,为页岩气储层精细评价提供理论依据。
英文摘要
The fine characterization of shale matrix mechanics is the premise of large-scale and efficient development of shale gas in China. At present, scholars generally study the mechanism of deformation and failure of shale mechanics by using micromechanics experiments, ignoring the influence of strong heterogeneity of mineral composition and microstructure. This project aims to study on the micromechanical properties and mechanical scale effect of heterogeneous shale matrix by means of molecular dynamics simulation, indentation test, three-dimensional finite element method and theoretical analysis. Molecular dynamics model of polycrystalline shale minerals of nano-indentation experiments is constructed to explain the deformation mechanism of shale mineral particles and to establish the elastic-plastic mechanical constitutive relationship of nano-scale matrix minerals. Then targeting micro and nano indentation experiments of shale matrix are conducted to verify the mechanical constitutive relationship, and the main controlling factors of micro-mechanical properties of heterogeneous shale are analyzed. Three-dimensional finite element model is built based on the digital core of shale sample and the established constitutive relationship, realizing the across-scale inversion analysis of indentation experiments. Based on the heterogeneity of the mineral composition and microstructure of shale matrtix and the microscopic mechanical parameters, a multi-scale upgrade model of mechanical properties of shale matrix is proposed to reveal the scale-dependent evolution law of mechanical properties of shale matrix. The results help to reveal the deformation mechanism of heterogeneous shale matrix, and provides a theoretical basis for the fine characterization of shale gas reservoirs.
我国经济发展新常态将推动能源结构不断优化调整,为页岩气大规模开采提供了宝贵的战略机遇。然而,国内对页岩微观力学变形机理及多尺度力学演化规律的认知还十分缺乏,造成了页岩气储层力学特性评价结果的可信度低。因此,揭示非均质性页岩纳米压痕力学响应机制和多尺度力学特性演化规律是表征页岩基质力学特性所面临和亟需解决的关键科学问题。为此,本项目结合理论分析、室内实验、数值仿真相结合的方法开展研究,并取得以下研究成果:构建了页岩基质石英矿物压痕过程分子动力学模型,阐明了压痕大小、晶粒大小和压头半径等因素对于石英微观力学特性的影响规律,发现简化杨氏模量和硬度随压痕深度的增大而增大,随压头尺寸的增大而减小,在小晶粒尺寸下,变形机制主要由晶界滑动主导,而不是晶内位错控制;利用靶向纳米压痕实验开展页岩基质微观力学特性测试,实现了页岩基质不同矿物颗粒弹性模量、硬度等微观力学参数精细表征,如石英、方解石、白云石和粘土矿物的平均弹性模量E分别为101.60GPa、64.61GPa、125.04GPa和53.93GPa,纳米压痕数据的离散性表明页岩基质微观力学性质具有较强的非均质性。ScCO2和水溶浸后,由于溶解作用引起的晶体结构变化,页岩矿物发生了不同程度的弹性模量E和硬度H值的降低,不同矿物的含量也发生变化。hf/hm和Wp/Wt的值可以结合P-h曲线所围成的滞回环来定性分析压痕过程中所产生的主要功和不可逆变形量。从压痕形貌观察,与其他矿物不同的是,粘土矿物中产生了大量微裂缝,这与压痕中产生明显的塑性变形量和其层状晶体结构密切相关。结合SEM/EDS分析技术建立了压痕实验的数值模拟仿真模型,通过反演分析结果探明了矿物成分及微观结构非均质性特征对页岩基质微观力学特性的影响规律,揭示了其力学特性跨尺度演化机制,提出了页岩基质力学多尺度升级演化模型。研究成果为页岩基质微、纳观力学变形机制、纳观-微观-宏观跨尺度力学特性演化评价提供理论支撑。
基于纳米压痕的饱和SC-CO2页岩基质微观力学损伤机理研究
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批准号:CSTB2023NSCQ-MSX0560
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项目类别:省市级项目
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资助金额:10.0万元
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批准年份:2023
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负责人:张成朋
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依托单位:
国内基金
海外基金