Article(id=1149773876252598287, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1149773869357167407, articleNumber=null, orderNo=null, doi=10.12404/j.issn.1671-1815.2405875, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1722787200000, receivedDateStr=2024-08-05, revisedDate=1739116800000, revisedDateStr=2025-02-10, acceptedDate=null, acceptedDateStr=null, onlineDate=1752057053863, onlineDateStr=2025-07-09, pubDate=1746633600000, pubDateStr=2025-05-08, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1752057053863, onlineIssueDateStr=2025-07-09, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1752057053863, creator=13701087609, updateTime=1752057053863, updator=13701087609, issue=Issue{id=1149773869357167407, tenantId=1146029695717560320, journalId=1146123166801305609, year='2025', volume='25', issue='13', pageStart='5273', pageEnd='5704', issueExtLink='null', onlineDate='null', pubDate='null', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=0, createTime=1752057052207, creator=13701087609, updateTime=1768456769392, updator=13701087609, preIssue=null, nextIssue=null, ext={EN=IssueExt(id=1218559268744253990, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1149773869357167407, language=EN, specialIssueTitle=, coverIllustrator=, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1218559268744253991, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1149773869357167407, language=CN, specialIssueTitle=, coverIllustrator=, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null}, startPage=5340, endPage=5350, ext={EN=ArticleExt(id=1149773876487479312, articleId=1149773876252598287, tenantId=1146029695717560320, journalId=1146123166801305609, language=EN, title=Susceptibility Assessment of Geological Hazards on Major Traffic Arteries in Western Sichuan Based on Stacking Ensemble Machine Learning Models, columnId=1156262729351549255, journalTitle=Science Technology and Engineering, columnName=Papers·Astronomy and Geosciences, runingTitle=null, highlight=null, articleAbstract=
The terrain in western Sichuan is complex and varied, and the geological structure is active, which makes the construction and maintenance of the traffic trunk line face the challenge of frequent geological disasters. Ensemble learning algorithm can optimize the shortcomings of the algorithm in geological hazard susceptibility assessment and improve the accuracy of the model, which has significant advantages in geological hazard susceptibility assessment. Taking the riverside high-speed as an example, 12 feature variables such as slope and relief were selected to construct the geological hazard susceptibility evaluation system. The forecasting performance of the modeling of the integrated algorithm and a single algorithm was compared and analyzed. The main control factors of the geological disasters along the riverside high-speed were discussed and the practicability of the model was verified. The results show that the proportion of high and extremely high geological hazard prone areas along the Yangtze River high speed is 18.21% and 9.85%, respectively, which are concentrated in the Leibo section and Jinyang section. The area under curve (AUC) of the receiver operating characteristics (ROC) curve and the precision-recall (P-R) curve in the integrated model. The AUC of ROC curve (0.84~0.86), the AUC of P-R curve (0.81~0.85) and the F1 score (0.78~0.79) of the three single machine learning models are significantly higher, and the prediction performance is better than that of a single machine learning algorithm. The development of high-speed geological hazards along the Yangtze River is controlled by topographic and geomorphic factors. The new damage points are located in the highly prone areas of the model, which verifies the accuracy and reliability of the Stacking model.
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川西地区地形复杂多变,地质构造活跃,致使交通干线的建设与维护面临着地质灾害频发的挑战。集成学习算法能优化地质灾害易发性评估中算法的不足,提升模型的精度,在地质灾害易发性评估中具有显著优势。以沿江高速为例,选取坡度、起伏度等12个特征变量构建地质灾害易发性评价体系,比较分析Stacking集成算法与单一算法建模的预测性能,探讨了沿江高速地质灾害的主控因素,并验证了模型的实用性。结果表明:沿江高速沿线地质灾害高和极高易发区占比分别为18.21%和9.85%,集中分布在雷波段和金阳段;Stacking集成模型受试者操作特征(receiver operating characteristics,ROC)曲线和精确率-召回率(precision-recall,P-R)曲线的曲线下的面积(area under curve,AUC)均达到0.89,F1分数也达到0.84,显著高于3个单一机器学习模型的ROC曲线的AUC(0.84~0.86)、P-R曲线的AUC(0.81~0.85)和F1分数(0.78~0.79),比单一机器学习算法有更好的预测性能;沿江高速地质灾害的发育受地形地貌因素控制;新增灾害点位于模型中的极高易发区,印证了Stacking模型的精确度和可靠性。
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吴逢涛(2000—),男,汉族,云南临沧人,硕士研究生。研究方向:地质灾害形成机理与防治。E-mail:635399281@qq.com。
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Geographical location of the study area, figureFileSmall=gJUDEO5Ut9SKQkeOp+iuNA==, figureFileBig=TipZnaPjqOumU58oofMXTA==, tableContent=null), ArticleFig(id=1176923426775253530, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图1, caption=
研究区地理位置, figureFileSmall=gJUDEO5Ut9SKQkeOp+iuNA==, figureFileBig=TipZnaPjqOumU58oofMXTA==, tableContent=null), ArticleFig(id=1176923426901082651, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.2, caption=
Flow chart of research method, figureFileSmall=9iP7n1Azfj/mGOepYBJt2Q==, figureFileBig=TmMXUU3G/B4AC+6hBvmMww==, tableContent=null), ArticleFig(id=1176923426963997212, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图2, caption=
研究方法流程图, figureFileSmall=9iP7n1Azfj/mGOepYBJt2Q==, figureFileBig=TmMXUU3G/B4AC+6hBvmMww==, tableContent=null), ArticleFig(id=1176923427031106077, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.3, caption=
Comparison of field investigation and remote sensing interpretation of geological disasters, figureFileSmall=1++HAHwjWocNyQnImG2mCQ==, figureFileBig=qUeJPUzE218zyBcgaSxO5A==, tableContent=null), ArticleFig(id=1176923427094020638, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图3, caption=
实地调查与遥感解译地质灾害对比, figureFileSmall=1++HAHwjWocNyQnImG2mCQ==, figureFileBig=qUeJPUzE218zyBcgaSxO5A==, tableContent=null), ArticleFig(id=1176923427211461151, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.4, caption=
Evaluation factor classification, figureFileSmall=abmodJq+RRLwEwCF481M3A==, figureFileBig=IZ1IwLxsECHMrrQt8H79EA==, tableContent=null), ArticleFig(id=1176923427278570016, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图4, caption=
评价因子分级, figureFileSmall=abmodJq+RRLwEwCF481M3A==, figureFileBig=IZ1IwLxsECHMrrQt8H79EA==, tableContent=null), ArticleFig(id=1176923427341484577, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.5, caption=
Poisson correlation coefficient between characteristic variable, figureFileSmall=TVJBKNu/X0KtPXWDFf5V3w==, figureFileBig=+JEKMK6nbWI5pQFfol6S4Q==, tableContent=null), ArticleFig(id=1176923427408593442, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图5, caption=
特征变量之间的泊松相关系数, figureFileSmall=TVJBKNu/X0KtPXWDFf5V3w==, figureFileBig=+JEKMK6nbWI5pQFfol6S4Q==, tableContent=null), ArticleFig(id=1176923427479896611, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.6, caption=
Variance inflation factor, figureFileSmall=wuawDuRggAdxMtmwcyCwYA==, figureFileBig=tN1J4xm6ksHShCnJz2KL6Q==, tableContent=null), ArticleFig(id=1176923427551199780, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图6, caption=
方差膨胀系数, figureFileSmall=wuawDuRggAdxMtmwcyCwYA==, figureFileBig=tN1J4xm6ksHShCnJz2KL6Q==, tableContent=null), ArticleFig(id=1176923427618308645, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.7, caption=
Geological hazard susceptibility zoning map, figureFileSmall=uhoR05jnyyr3IOhPDF2HOw==, figureFileBig=82NDG9VXyCFbLWv7lF4gqQ==, tableContent=null), ArticleFig(id=1176923427677028902, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图7, caption=
地质灾害易发性分区图, figureFileSmall=uhoR05jnyyr3IOhPDF2HOw==, figureFileBig=82NDG9VXyCFbLWv7lF4gqQ==, tableContent=null), ArticleFig(id=1176923427739943463, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.8, caption=
Curves comparison analysis, figureFileSmall=W95C4rXDtQfiZTxDL5edsA==, figureFileBig=U/zg+NfnkFqnZN1Q14ny0A==, tableContent=null), ArticleFig(id=1176923427840606760, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图8, caption=
曲线对比分析, figureFileSmall=W95C4rXDtQfiZTxDL5edsA==, figureFileBig=U/zg+NfnkFqnZN1Q14ny0A==, tableContent=null), ArticleFig(id=1176923427899327017, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.9, caption=
Analysis results of control factor weights based on stacked ensemble model, figureFileSmall=mhLi/kYkDT7tRqkD4LiF3A==, figureFileBig=D8YOzLtPvCyakc1GDoFa4A==, tableContent=null), ArticleFig(id=1176923427983213098, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图9, caption=
基于堆叠集成模型的控制因子权重分析结果, figureFileSmall=mhLi/kYkDT7tRqkD4LiF3A==, figureFileBig=D8YOzLtPvCyakc1GDoFa4A==, tableContent=null), ArticleFig(id=1176923428033544747, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.10, caption=
Topography and geomorphology of Jinyang County, figureFileSmall=OeOq/8UaykskdUMpWrut+A==, figureFileBig=kx4nt7dzCH0bxSco/ZKvAw==, tableContent=null), ArticleFig(id=1176923428096459308, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图10, caption=
金阳县地形地貌, figureFileSmall=OeOq/8UaykskdUMpWrut+A==, figureFileBig=kx4nt7dzCH0bxSco/ZKvAw==, tableContent=null), ArticleFig(id=1176923428159373869, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Fig.11, caption=
Verification of prediction model and field inspection diagram, figureFileSmall=HhSJb2XYCyyf1qUoyRSL7g==, figureFileBig=4R7Eq6nY0mZ7DKyQVHgt1g==, tableContent=null), ArticleFig(id=1176923428222288430, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=图11, caption=
预测模型验证及实地考察图 (a)Stacking集成模型地质灾害易发性图;(b)RF模型地质灾害易发性图;(c)XGBoost模型地质灾害易发性图;(d)SVM模型地质灾害易发性图;(e)灾害点影像图;(f)灾害点现场拍摄图
, figureFileSmall=HhSJb2XYCyyf1qUoyRSL7g==, figureFileBig=4R7Eq6nY0mZ7DKyQVHgt1g==, tableContent=null), ArticleFig(id=1176923428281008687, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Table 1, caption=
The evaluation factors selected for the study
, figureFileSmall=null, figureFileBig=null, tableContent=
| 评价因子 | 评价因子释义 | 数据来源 |
| NDVI | NDVI是通过比较近红外和红光反射率来评估植被健康和密度的数值指标 | 国家青藏高原科学数据中心 |
| DEM | 数字高程模型(digital elevation model,DEM),高程指某点沿铅垂线方向到绝对基面的距离 | NASA地球科学数据网站 |
| 剖面曲率 | 剖面曲率是指地表在垂直方向上的曲率 | 基于DEM数据和ArcGIS分析得出 |
| 平面曲率 | 平面曲率是指地表在水平方向上的曲率 |
| 起伏度 | 起伏度是指地表在水平方向上的高程变化程度 |
| 坡度 | 坡度是指地表某一点的坡降 |
| 坡向 | 坡向是地表某一点向下倾斜的方向 |
| 岩性 | 岩性是指岩石的性质和组成特征 | 中华人民共和国1∶250万数字地质图空间数据库 |
| 植被类型 | 不同类型的植被对地质灾害的影响也有所不同 | 中国科学院地理科学与资源研究所数据中心 |
| PGA | PGA是描述地震强度的重要参数 | GB18306—2015附录A:中国地震动峰值加速度区划图 |
| 断层距离 | 断层距离通常指地质学中测量的一个点到断层面的最短距离 | 中国地理空间数据集 |
| 降雨 | 降雨指的是研究区每年总降雨量平均值 | 国家青藏高原科学数据中心 |
), ArticleFig(id=1176923428343923248, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=表1, caption=
研究选取的评价因子
, figureFileSmall=null, figureFileBig=null, tableContent=
| 评价因子 | 评价因子释义 | 数据来源 |
| NDVI | NDVI是通过比较近红外和红光反射率来评估植被健康和密度的数值指标 | 国家青藏高原科学数据中心 |
| DEM | 数字高程模型(digital elevation model,DEM),高程指某点沿铅垂线方向到绝对基面的距离 | NASA地球科学数据网站 |
| 剖面曲率 | 剖面曲率是指地表在垂直方向上的曲率 | 基于DEM数据和ArcGIS分析得出 |
| 平面曲率 | 平面曲率是指地表在水平方向上的曲率 |
| 起伏度 | 起伏度是指地表在水平方向上的高程变化程度 |
| 坡度 | 坡度是指地表某一点的坡降 |
| 坡向 | 坡向是地表某一点向下倾斜的方向 |
| 岩性 | 岩性是指岩石的性质和组成特征 | 中华人民共和国1∶250万数字地质图空间数据库 |
| 植被类型 | 不同类型的植被对地质灾害的影响也有所不同 | 中国科学院地理科学与资源研究所数据中心 |
| PGA | PGA是描述地震强度的重要参数 | GB18306—2015附录A:中国地震动峰值加速度区划图 |
| 断层距离 | 断层距离通常指地质学中测量的一个点到断层面的最短距离 | 中国地理空间数据集 |
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), ArticleFig(id=1176923428419420721, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=EN, label=Table 2, caption=
Partition statistics of susceptibility zoning
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| 分区等级 | Stacking集成 | | RF | | SVM | | XGBoost |
| 面积比例/% | 灾害点数/个 | 面积比例/% | 灾害点数/个 | 面积比例/% | 灾害点数/个 | 面积比例/% | 灾害点数/个 |
| 极低 | 4.81 | 22 | | 14.67 | 89 | | 15.53 | 1 | | 16.45 | 116 |
| 低 | 34.15 | 81 | | 32.19 | 134 | | 30.68 | 110 | | 21.76 | 304 |
| 中 | 32.98 | 165 | | 25.15 | 234 | | 36.93 | 310 | | 25.72 | 239 |
| 高 | 18.21 | 378 | | 20.07 | 260 | | 15.20 | 415 | | 22.18 | 165 |
| 极高 | 9.85 | 294 | | 7.92 | 223 | | 1.67 | 104 | | 13.89 | 116 |
), ArticleFig(id=1176923428486529586, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149773876252598287, language=CN, label=表2, caption=
易发性分区统计结果
, figureFileSmall=null, figureFileBig=null, tableContent=
| 分区等级 | Stacking集成 | | RF | | SVM | | XGBoost |
| 面积比例/% | 灾害点数/个 | 面积比例/% | 灾害点数/个 | 面积比例/% | 灾害点数/个 | 面积比例/% | 灾害点数/个 |
| 极低 | 4.81 | 22 | | 14.67 | 89 | | 15.53 | 1 | | 16.45 | 116 |
| 低 | 34.15 | 81 | | 32.19 | 134 | | 30.68 | 110 | | 21.76 | 304 |
| 中 | 32.98 | 165 | | 25.15 | 234 | | 36.93 | 310 | | 25.72 | 239 |
| 高 | 18.21 | 378 | | 20.07 | 260 | | 15.20 | 415 | | 22.18 | 165 |
| 极高 | 9.85 | 294 | | 7.92 | 223 | | 1.67 | 104 | | 13.89 | 116 |
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