（1）岩土体入渗规律

（2）滑坡机制

（3）黄土灾害链过程

（4）灾害情景再现

（5）监测预警

（1）岩土体入渗规律

（2）滑坡机制

（3）黄土灾害链过程

（4）灾害情景再现

（5）监测预警

本科生课程：地质学基础、土力学、地质工程数据信息新技术

研究生课程：地质灾害学（Geologicaldisasters）,英文课

（1）国家重点研发计划子课题，黄土高原重大链生灾害时空演化与成灾放大效应，2023-2026，70万，主持。

（2）国家自然科学基金面上项目，沟谷区黄土灾害链的演进转化机制与成灾放大效应研究，2025-2028，47万，主持。

（3）国家自然科学基金青年项目，黄土细观界面形成演化机制试验研究，2022-2024，30万，主持。

（4）国家自然科学基金重大项目子课题，静态液化型黄土滑坡启滑机制与判据，2021-2025，50万，主持。

（5）国家自然科学基金重大项目子课题，秦岭生态地质环境系统演化与灾害风险管控，2023-2026，50万，主持。

（6）国家自然科学基金重大项目子课题，黄河流域地质地表过程与重大灾害效应，2021-2024，30万，主持。

代表性论文

第一/通讯论文：

[1]Evolutionof loess gullies and geohazard chains in the Dongzhi tableland,China. Geomorphology.

[2]Formationmechanism and evolution characteristics of the loess–mudstoneinterface landslide in Yan’an, China. Bulletinof Engineering Geology and the Environment.

[3]Failuremechanism of a loess-red silty clay interface landslide on theHeifangtai platform, China. Bulletinof Engineering Geology and the Environment.

[4]Thefailure modes and evolution process of loess landslide dams via flumetests. Landslides.

[5]Influencesof freeze-thaw cycles on desiccation cracking of an intactloess. EngineeringGeology.

[6]Erosionand potential geological hazards chain in the East African RiftSystem controlled by volcanic sediments properties and geologicalstructure. Geomorphology.

[7]Characteristicand disaster effects of loess meso-interfaces: A field geologicalinvestigation[J]. CATENA.

[8]The Impact of the Densest and Highest-Capacity Reservoirs on theEcological Environment in the Upper Yellow River Basin of China: From2000 to 2020. RemoteSensing.

[9]Impactsof Cascade Reservoirs on Adjacent Climate and Land Use Change in theUpper Yellow River, China. AppliedSciences.

[10]EvolutionCharacteristics and Failure Mechanisms of Retrogressive LoessLandslides: A Case Study from the South Jingyang Platform,China. AppliedSciences.

[11]Permeabilitycharacteristics, structural failure characteristics, and triggeringprocess of loess landslides in two typical stratastructures. EngineeringGeology.

[12]Theshear behavior of the slip zone loess and landslidemechanism. Journalof Asian Earth Sciences.

[13]Microstructureresponse to shear strength deterioration in loess after freeze-thawcycles. EngineeringGeology.

[14]Effectof fracture distribution on the triaxial shear behavior ofloess. Frontiersin Earth Science.

[15]Acomprehensive method for the risk assessment of ground fissures: casestudy of the eastern weihe basin. Journalof Earth Science.

[16]Initiationmechanism of loess mudflows by flume experiments. Journalof Earth Science.

[17]Characteristicsof loess landslides triggered by different factors in the ChineseLoess Plateau. Journalof mountain science.

[18]Flumetests to investigate the initiation mechanism of loess mudflows onthe Chinese Loess Plateau. Frontiersin Earth Science.

[19]Themechanisms of a loess landslide triggered by diversion irrigation: Acase study of the South Jingyang Platform, China. Bulletinof Engineering Geology and the Environment.

[20]Loesslandslides on the South Jingyang Platform in Xi’an,China. QuarterlyJournal of Engineering Geology and Hydrogeology.

[21]Interactionbetween landsliding materials and the underlying erodible bed in aloess flowslide, EngineeringGeology.

[22]论黄土地质灾害链（一）.自然灾害学报.

[23]论黄土地质灾害链（二）.自然灾害学报.

[24].黑方台地区马兰黄土渗透特性及结构损伤试验研究.地质科技通报.

[25]甘肃黑方台“10·5”黄土滑坡启动及运动特征分析.中国地质灾害与防治学报.

[26]黑方台区域黄土红黏土界面渗透特性研究.工程地质学报.

[27]不同上游来水流量下黄土堰塞坝下切过程试验研究.工程地质学报

[28]不同来水流量下黄土堰塞坝溃口展宽历程的水槽试验研究.灾害学.

[29]基于多模型对比的甘肃庆阳地区滑坡易发性评价. 地球科学与环境学报.

[30]一种基于弹塑性理论的黄土湿陷评价模型.工程地质学报.

[31]泾阳南塬典型黄土滑坡成因、堆积及运动特征分析.工程地质学报.

[32]陕西泾阳“3·8”蒋刘黄土滑坡成因及运动特征分析.工程地质学报.

[33]黄土浅层降雨入渗规律研究.水土保持通报.

[34]陕西蓝田铜鹅沟泥石流发育特征及危险性分析.中国地质灾害与防治学报.

[35]典型黄土残余强度变化规律分析——以陕西泾阳南塬黄土为例.中国地质灾害与防治学报.

陕西省高校优秀青年人才支持计划

陕西省优秀博士论文

2020-08至今，长安大学，地质工程与测绘学院，讲师、副教授、教授。