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In recent years, artificial intelligence has demonstrated strong pattern recognition and classification capabilities across various fields, providing new insights for lithology identification. Starting from three methods: support vector machines, neural networks, and ensemble learning, the basic principles, advantages and disadvantages of these machine learning algorithms were reviewed, as well as their research progress and application in the field of uranium ore bed lithology identification. The results show that machine learning can effectively identify the correlation between logging data and different lithologies through model training, transforming the process of lithology identification into a machine learning process. This can greatly improve the automation level and accuracy of lithology identification, holding significant practical importance and a broad development prospect.
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近年来,人工智能在各个领域展现出了强大的模式识别和分类能力,为岩性识别提供了新的思路。从支持向量机、神经网络、集成学习这3种方法出发,综述这些机器学习算法的基本原理、优缺点及其在铀矿层岩性识别领域的研究进展和应用情况。结果表明:机器学习通过训练模型可以有效识别出测井数据与不同岩性之间的关联,将岩性识别过程转化为机器学习的过程,可以极大地提高岩性识别自动化程度和识别准确率,具有重要的现实意义和广阔的发展前景。
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肖昆(1987—),男,汉族,江西抚州人,博士,副教授。研究方向:地球物理测井理论与方法。E-mail:xiaokun0626@163.com。
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肖昆(1987—),男,汉族,江西抚州人,博士,副教授。研究方向:地球物理测井理论与方法。E-mail:xiaokun0626@163.com。
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18: 53-64., articleTitle=Lithology identification of uranium drilling based on SMOTE algorithm logic-CNN, refAbstract=null)], funds=[Fund(id=1179786724847792871, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, awardId=20204BCJ23027, language=CN, fundingSource=江西省主要学科学术和技术带头人培养计划(20204BCJ23027), fundOrder=null, country=null), Fund(id=1179786724902318824, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, awardId=2022NRE-LH-18, language=CN, fundingSource=核资源与环境国家重点实验室联合创新基金(2022NRE-LH-18), fundOrder=null, country=null), Fund(id=1179786724956844777, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, awardId=20232BAB203072, language=CN, fundingSource=江西省自然科学基金(20232BAB203072), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1179786721446212261, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, xref=1, ext=[AuthorCompanyExt(id=1179786721450406566, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, companyId=1179786721446212261, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
1 Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China), AuthorCompanyExt(id=1179786721458795175, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, companyId=1179786721446212261, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
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2 Nuclear Industry Group No.243, Chifeng 024000, China), AuthorCompanyExt(id=1179786721525904042, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, companyId=1179786721513321128, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=
2 核工业二四三大队, 赤峰 024000)])], figs=[ArticleFig(id=1179786723836965593, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Fig.1, caption=
Based on neural network model rock recognition results map[25], figureFileSmall=Krd4mjL1vQpti4bHuh3YOQ==, figureFileBig=A/TQEojNN2qOy3/Gx3re+Q==, tableContent=null), ArticleFig(id=1179786723899880154, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=图1, caption=
基于神经网络模型岩性识别成果图[25] CS为粗粒砂岩;MS为中粒砂岩;FS为细粒砂岩;CG为钙质砂岩;MD为泥岩
, figureFileSmall=Krd4mjL1vQpti4bHuh3YOQ==, figureFileBig=A/TQEojNN2qOy3/Gx3re+Q==, tableContent=null), ArticleFig(id=1179786723971183323, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Fig.2, caption=
Discriminant results of support vector machines[46], figureFileSmall=+F0hnEMAQ6tjFqNYDgbjuQ==, figureFileBig=Lx3yeXc9TSkOq3wrVzr+LQ==, tableContent=null), ArticleFig(id=1179786724055069404, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=图2, caption=
支持向量机的判别结果[46] GR为自然伽马测井曲线;DEN为密度测井曲线;CAL为井径测井曲线;RT为电阻率测井曲线;AC为声波时差测井曲线;IP为极化率测井曲线;Mas为磁化率测井曲线,其单位中的CGS是厘米-克-秒(centimeter-gram-second)单位制的缩写,Mas测井曲线反映的是岩石的磁化率,在CGS单位制中,磁化率是一个无量纲的量,它表示物质被磁化的难易程度
, figureFileSmall=+F0hnEMAQ6tjFqNYDgbjuQ==, figureFileBig=Lx3yeXc9TSkOq3wrVzr+LQ==, tableContent=null), ArticleFig(id=1179786724122178269, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Fig.3, caption=
Comparison of lithology identification[76], figureFileSmall=VRvGz96t5LmauDjzvoT6zA==, figureFileBig=xA7vhcGlSGaKaLgI5zC25Q==, tableContent=null), ArticleFig(id=1179786724180898526, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=图3, caption=
岩性识别对比图[76] SCXDY为三侧向电压测井曲线,mV;SSSC为双采集时差测井曲线,μs/m;DMZKMD为密度测井曲线,g/cm3;ZRDW为自然电位测井曲线,mV;DZL为钻井液电阻率测井曲线,Ω·m;DYJ为短源距放射性测井曲线,API;DMZKGG为井径测井曲线,mm;
1为泥岩;2为粉砂岩;3为细砂岩;4为中砂岩;5为粗砂岩
, figureFileSmall=VRvGz96t5LmauDjzvoT6zA==, figureFileBig=xA7vhcGlSGaKaLgI5zC25Q==, tableContent=null), ArticleFig(id=1179786724235424479, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Fig.4, caption=
Comparison of GBDT+NoBalancing method and GBDT+SMOTE method[83], figureFileSmall=CDn89GeZZJwVG94rB6jTfw==, figureFileBig=Pw0GfOYmfnEiO/xP039frg==, tableContent=null), ArticleFig(id=1179786724302533344, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=图4, caption=
GBDT+NoBalancing方法与GBDT+SMOTE方法的比较[83] GBDT+NoBalancing为梯度提升决策树+不进行样本平衡;GBDT+SMOTE为梯度提升决策树+少数类过采样法
, figureFileSmall=CDn89GeZZJwVG94rB6jTfw==, figureFileBig=Pw0GfOYmfnEiO/xP039frg==, tableContent=null), ArticleFig(id=1179786724357059297, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Table 1, caption=
Tanlangole uranium lithology identification confusion matrix[25]
, figureFileSmall=null, figureFileBig=null, tableContent=
| 预测 | 真实 | 总计 |
| 砾岩 | 粗砂岩 | 中砂岩 | 细砂岩 | 泥岩 |
| 砾岩 | 26 | 0 | 0 | 0 | 0 | 26 |
| 粗砂岩 | 10 | 40 | 2 | 0 | 0 | 52 |
| 中砂岩 | 0 | 4 | 391 | 25 | 4 | 424 |
| 细砂岩 | 0 | 0 | 20 | 55 | 5 | 80 |
| 泥岩 | 0 | 0 | 1 | 6 | 10 | 17 |
| 灵敏度/% | 72.22 | 90.91 | 94.44 | 63.95 | 52.63 | 74.83 |
| 特异性/% | 100.00 | 99.63 | 81.72 | 79.81 | 100.00 | 92.23 |
| 精度/% | 100.00 | 76.92 | 92.22 | 68.75 | 58.82 | 79.34 |
| 准确率/% | 88.31 |
), ArticleFig(id=1179786724415779554, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=表1, caption=
塔然高勒铀矿岩性识别混淆矩阵[25]
, figureFileSmall=null, figureFileBig=null, tableContent=
| 预测 | 真实 | 总计 |
| 砾岩 | 粗砂岩 | 中砂岩 | 细砂岩 | 泥岩 |
| 砾岩 | 26 | 0 | 0 | 0 | 0 | 26 |
| 粗砂岩 | 10 | 40 | 2 | 0 | 0 | 52 |
| 中砂岩 | 0 | 4 | 391 | 25 | 4 | 424 |
| 细砂岩 | 0 | 0 | 20 | 55 | 5 | 80 |
| 泥岩 | 0 | 0 | 1 | 6 | 10 | 17 |
| 灵敏度/% | 72.22 | 90.91 | 94.44 | 63.95 | 52.63 | 74.83 |
| 特异性/% | 100.00 | 99.63 | 81.72 | 79.81 | 100.00 | 92.23 |
| 精度/% | 100.00 | 76.92 | 92.22 | 68.75 | 58.82 | 79.34 |
| 准确率/% | 88.31 |
), ArticleFig(id=1179786724491277027, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Table 2, caption=
SVM model optimization methods[48-52]
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| 优化方法 | 方法描述 | 参考文献 |
| 引入隶属度 | 根据样本重要性赋予隶属度 | 张翔等[48] |
| 主成分分析法 | 提取测井数据中影响岩性识别因素 | 钟仪华等[49] |
| 粒子群算法 | 优化核函数参数γ和惩罚因C | 陈钢花等[50] |
| 遗传算法 | 优选核函数参数σ和惩罚因子C | 张昭杰等[51] |
| 变分不等式算法 | 优化问题转变为求解不等式 | Mou等[52] |
), ArticleFig(id=1179786724549997284, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=表2, caption=
SVM模型优化方法[48-52]
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| 优化方法 | 方法描述 | 参考文献 |
| 引入隶属度 | 根据样本重要性赋予隶属度 | 张翔等[48] |
| 主成分分析法 | 提取测井数据中影响岩性识别因素 | 钟仪华等[49] |
| 粒子群算法 | 优化核函数参数γ和惩罚因C | 陈钢花等[50] |
| 遗传算法 | 优选核函数参数σ和惩罚因子C | 张昭杰等[51] |
| 变分不等式算法 | 优化问题转变为求解不等式 | Mou等[52] |
), ArticleFig(id=1179786724608717541, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=EN, label=Table 3, caption=
Comparison of different machine learning methods for uranium seam identification[32,40,51,65,72]
, figureFileSmall=null, figureFileBig=null, tableContent=
| 机器学习方法 | 输出类别 | 准确率/% | 主要优缺点 | 参考文献 |
| 神经网络(ANN) | 矿化层、异常层非矿化层 | 86.55 | 抗干扰能力强,能快速获取未知孔的异常信息 | 张平等[32] |
长短期记忆神经 网络(LSTM) | 泥岩、粉砂岩、细砂岩、粗砂岩、中砂岩 | 85.00 | 模型的循环单元简单,性能稳定,少量样本岩性识别效果较差 | 陈炫沂[40] |
| 支持向量机(SVM) | 泥岩、泥质粉砂岩、中细砂岩、砂砾岩 | 81.60 | 适用于小样本,中砂岩和泥岩识别易混淆 | 张昭杰等[51] |
| 随机森林(RF) | 泥岩、细砂岩、中砂岩、粗砂岩、砾岩 | 82.85 | 有较高鲁棒性和泛化能力,薄层岩性识别效果较差 | 马东来等[65] |
| 梯度提升决策树(GBDT) | 黏土、泥岩、粉砂岩、细砂岩、中砂岩、粗砂岩、砂砾岩 | 98.52 | 简单高效,可以提供特征重要性评估,但薄层岩性识别准确率较低 | 段忠义等[72] |
), ArticleFig(id=1179786724675826406, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149774725708214893, language=CN, label=表3, caption=
铀矿层识别的不同机器学习方法对比[32,40,51,65,72]
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| 机器学习方法 | 输出类别 | 准确率/% | 主要优缺点 | 参考文献 |
| 神经网络(ANN) | 矿化层、异常层非矿化层 | 86.55 | 抗干扰能力强,能快速获取未知孔的异常信息 | 张平等[32] |
长短期记忆神经 网络(LSTM) | 泥岩、粉砂岩、细砂岩、粗砂岩、中砂岩 | 85.00 | 模型的循环单元简单,性能稳定,少量样本岩性识别效果较差 | 陈炫沂[40] |
| 支持向量机(SVM) | 泥岩、泥质粉砂岩、中细砂岩、砂砾岩 | 81.60 | 适用于小样本,中砂岩和泥岩识别易混淆 | 张昭杰等[51] |
| 随机森林(RF) | 泥岩、细砂岩、中砂岩、粗砂岩、砾岩 | 82.85 | 有较高鲁棒性和泛化能力,薄层岩性识别效果较差 | 马东来等[65] |
| 梯度提升决策树(GBDT) | 黏土、泥岩、粉砂岩、细砂岩、中砂岩、粗砂岩、砂砾岩 | 98.52 | 简单高效,可以提供特征重要性评估,但薄层岩性识别准确率较低 | 段忠义等[72] |
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