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基于小波与反褶积结合的薄互层岩性界面识别方法 被引量:1
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作者 李志鹏 黄莉莎 +3 位作者 闫建平 杨明林 乌洪翠 王敏 《测井技术》 CAS 2024年第5期602-612,共11页
准噶尔盆地莫西庄地区三工河组二段岩性复杂多样、变化快,单砂岩体中薄层岩性频繁互层,存在较强的岩性、物性、含油非均质性特征。精细划分薄互层岩性并识别其分层界面是开展储层识别、流体解释及有效储层厚度确立等重要的前提工作。为... 准噶尔盆地莫西庄地区三工河组二段岩性复杂多样、变化快,单砂岩体中薄层岩性频繁互层,存在较强的岩性、物性、含油非均质性特征。精细划分薄互层岩性并识别其分层界面是开展储层识别、流体解释及有效储层厚度确立等重要的前提工作。为了精确地识别薄互层岩性的分层界面,从测井信息采集分辨率与信号分析角度出发,提出了基于小波与反褶积相结合的薄互层岩性分层界面识别方法。首先,利用小波变换多尺度分解和重构原理,对自然伽马测井曲线进行高、低频分解,提取出反映地层岩性变化的有效信号与高频噪声;然后,对有效信号进行重构,构建一条去除噪声能够表征更接近真实地层信息的自然伽马测井曲线;最后,利用反褶积方法对重构的自然伽马测井曲线进行高分辨率处理,很大程度上提高了自然伽马测井曲线响应薄层岩性的纵向分辨率。经实例井取心岩性资料验证,利用该方法处理得到高分辨率自然伽马测井曲线的形态与数值特征能够有效地提高单砂岩体中多套薄互层岩性分层界面识别的精度,为莫西庄三工河组二段储层有效性精细评价提供了依据。 展开更多
关键词 岩性非均质性 “小波+反褶积”组合法 曲线重构 提高分辨率 界面识别
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页岩气井分段压裂套损影响因素分析 被引量:34
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作者 李军 李玉梅 +2 位作者 张德龙 杨宏伟 孙世斌 《断块油气田》 CAS 北大核心 2017年第3期387-390,共4页
四川盆地长宁—威远页岩气示范区分段压裂过程中出现的套管变形、挤毁问题已经严重影响到页岩气井的井筒完整性以及勘探开发效果。考虑非均匀地应力、套管偏心、页岩各向异性、地层岩性非均质性等多因素的逐级耦合作用,利用有限元数值... 四川盆地长宁—威远页岩气示范区分段压裂过程中出现的套管变形、挤毁问题已经严重影响到页岩气井的井筒完整性以及勘探开发效果。考虑非均匀地应力、套管偏心、页岩各向异性、地层岩性非均质性等多因素的逐级耦合作用,利用有限元数值方法建立了偏心套管-水泥环-地层耦合的全尺寸数值模型,对页岩气水平井分段压裂过程中套管损坏机理进行研究分析。研究发现:套管偏心不是套管先期损坏的主控因素;随着非均匀地应力比增大,套管内壁应力极值及周向应力不均匀程度明显增大;页岩各向异性比越大,偏心角径向位置对应的套管内壁应力越大,此处承载风险也越高;套管内壁应力最大值出现在岩性交替变化界面,非均质性差异对套管内壁应力极值有较大的影响。研究结果可为页岩气井分段压裂过程中套损预测提供理论依据。 展开更多
关键词 词页 套管变形 套管偏心 匀地应力 各向异 岩性非均质性
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鄂尔多斯盆地吴起地区长10段复杂油水层测井识别方法 被引量:2
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作者 王艳梅 席辉 +2 位作者 谭玉涵 戚林河 马明哲 《长江大学学报(自然科学版)》 CAS 2020年第6期14-20,M0003,共8页
鄂尔多斯盆地吴起地区延长组长10段为主要的含油层系,储层非均质性强、地层水矿化度变化大,油、水层测井响应关系复杂,流体性质识别困难,测井解释符合率低。利用地质、测井、分析化验和试油等资料,分析了中高阻水层成因机理,认为地层水... 鄂尔多斯盆地吴起地区延长组长10段为主要的含油层系,储层非均质性强、地层水矿化度变化大,油、水层测井响应关系复杂,流体性质识别困难,测井解释符合率低。利用地质、测井、分析化验和试油等资料,分析了中高阻水层成因机理,认为地层水矿化度低、高阻填隙物体积分数高是导致油水关系复杂的主要原因。基于阿尔奇公式,利用常规测井资料反演了视地层水电阻率及视地层水电阻率谱,拾取了视地层水电阻率谱均值、方差及歪度等特征参数,创新构建了地层水特征指示参数和岩性非均质性表征参数,建立了基于岩性和水性的流体性质识别方法。应用结果表明,测井解释符合率大幅度提高,效果显著。 展开更多
关键词 复杂油水层 岩性非均质性 视地层水电阻率谱 流体识别 吴起地区
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Effect of heterogeneity on mechanical and acoustic emission characteristics of rock specimen 被引量:8
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作者 李术才 李国莹 《Journal of Central South University》 SCIE EI CAS 2010年第5期1119-1124,共6页
The influence of heterogeneity on mechanical and acoustic emission characteristics of rock specimen under uniaxial compress was studied with numerical simulation methods.Weibull distribution function was adopted to de... The influence of heterogeneity on mechanical and acoustic emission characteristics of rock specimen under uniaxial compress was studied with numerical simulation methods.Weibull distribution function was adopted to describe the mesoscopic heterogeneity of rocks.The failure process of heterogeneous rock specimen under uniaxial loading was simulated using FLAC 3D software.Five schemes were adopted to investigate the influence of heterogeneity.The results demonstrate that as the homogeneity increases,the peak strength and brittleness of rocks increase,and the macro elastic modulus improves as well.Heterogeneity has great influence on macro elastic modulus and strength when the homogeneity coefficient is less than 20.0.The volume expansion is not so obvious when the homogeneity increases.As the homogeneity coefficient increases the acoustic emissions modes change from swarm shock to main shock.When the homogeneity coefficient is high,the cumulative acoustic emission events-axial strain curve is gentle before the rock failure.The numerical results agree with the previously numerical results and earlier experimental measurements. 展开更多
关键词 HETEROGENEITY acoustic emission strain softening numerical simulation uniaxial compression elastic modulus
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Effects of porosity heterogeneity on chemical dissolution-front instability in fluid-saturated rocks 被引量:4
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作者 ZHAO Chong-bin Peter SCHAUBS Bruce HOBBS 《Journal of Central South University》 SCIE EI CAS CSCD 2017年第3期720-725,共6页
Homogeneity and heterogeneity are two totally different concepts in nature.At the particle length scale,rocks exhibit strong heterogeneity in their constituents and porosities.When the heterogeneity of porosity obeys ... Homogeneity and heterogeneity are two totally different concepts in nature.At the particle length scale,rocks exhibit strong heterogeneity in their constituents and porosities.When the heterogeneity of porosity obeys the random uniform distribution,both the mean value and the variance of porosities in the heterogeneous porosity field can be used to reflect the overall heterogeneous characteristics of the porosity field.The main purpose of this work is to investigate the effects of porosity heterogeneity on chemical dissolution front instability in fluid-saturated rocks by the computational simulation method.The related computational simulation results have demonstrated that:1) since the propagation speed of a chemical dissolution front is inversely proportional to the difference between the final porosity and the mean value of porosities in the initial porosity field,an increase in the extent of the porosity heterogeneity can cause an increase in the mean value of porosities in the initial porosity field and an increase in the propagation speed of the chemical dissolution front.2) An increase in the variance of porosities in the initial porosity field can cause an increase in the instability probability of the chemical dissolution front in the fluid-saturated rock.3) The greater the mean value of porosities in the initial porosity field,the quicker the irregular morphology of the chemical dissolution front changes in the supercritical chemical dissolution systems.This means that the irregular morphology of a chemical dissolution front grows quicker in a porosity field of heterogeneity than it does in that of homogeneity when the chemical dissolution system is at a supercritical stage. 展开更多
关键词 porosity heterogeneity chemical dissolution front instability computational simulation porous rocks
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