姓名：魏玉杰   职称：副教授    E-mail: wyj@mail.hzau.edu.cn

研究方向：土壤结构与土体稳定性、山地灾害风险评价、水土保持与生态修复

个人简历：

bat365中文官方网站副教授，硕士生导师。研究领域为土壤侵蚀过程与机理，主要以土壤结构和土体稳定性为核心，综合岩土力学与山地灾害等理论与技术，系统研究复杂地形条件下滑坡、崩塌等重力侵蚀的水-土耦合动力过程、机理与风险防控。以第一作者或通讯作者在 Geoderma、Soil & Tillage Research、Soil Science Society of America Journal等国际学术期刊发表论文20余篇。担任ANSO-世界黑土联合会理事、《International Soil and Water Conservation》科学编辑、湖北省水土保持学会水土保持技术服务专家、Catena等国际学术期刊审稿人。

教育/工作经历：

2021.4 –至今，bat365中文官方网站，副教授

2018.4 – 2021.4，bat365中文官方网站，团队博士后

2016.9 – 2017.10，美国俄克拉荷马大学土木工程与环境科学学院土木工程系，联合培养博士

2012. 9 – 2017.12，bat365在线登录入口， 土壤学，博士

2008.9 – 2012.06，bat365在线登录入口，农业资源与环境专业，学士

科学研究：

国家自然科学基金面上项目（2023.01-2026.12）：花岗岩风化土体裂隙演化机制及其对崩岗侵蚀的影响，主持；

国家重点研发计划子专题（2021.12-2024.12）：侵蚀退化农田生态生产功能重建机制和提升关键技术与示范，专题负责人；

国家重点研发计划子专题（2021.12-2026.11）：长江中下游坡耕地红黄壤与中低产稻田产能提升技术模式及应用，参与；

国家自然科学基金青年项目（2019.01-2021.12）：干湿交替作用下非均质土体的变形与失稳机制，主持；

中国博士后科学基金（2019.01-2020.04）：崩岗侵蚀区土壤变形与破坏对水分变化的响应，主持；

国家自然科学基金重点项目（2017.01-2021.12）：花岗岩风化岩土体特性的地带性分异及崩岗形成机理研究，参与；

bat365在线登录入口自主科技创新基金（2022.01-2024.12）：不同空间尺度下南方崩岗驱动因子研究，主持；

国家自然科学基金面上项目（2022.01-2024.12）：紫色土坡面水分格局与水文过程对土壤空间异质性的响应，参与；

国家自然科学基金面上项目（2022.01-2024.12）：坡面侵蚀泥沙磷富集率对降雨-径流-土壤混合深度的响应，参与。

获奖及专利

The second International Youth Forum on Soil and Water Conservation—“Youth Outstanding Paper Award (Datum) ”，2018；

第一届湖北省水土保持学会优秀论文一等奖，2018；

基于盐溶液法测定干湿交替条件下土壤水分特征曲线的装置与方法（ZL 202110277346.6），发明专利，完成人：魏玉杰，周小荃，辜婧瑶；

国际会议

Soil Erosion Research: Current & Future Prospective in China and South Africa; 2018/07/08-07/17; ARC-Institute for soil, climate, and water, Pretoria, South Africa; Presentation title: Soil erosion and stability mechanisms of granitic soils in South China.

The Second International Young Scientists Forum on Soil and Water Conservation and ICCE symposium 2018 "Climate Change Impacts on Sediment Dynamics: Measurement, Modelling and Management”; 2018/08/27-09/03; Lomonosov Moscow State University, Moscow, Russia; Presentation title: A field simulation of the infiltration processes for heavy-textured soils from central to south China.

出版著作

《土壤与生活》（参译）科学出版社

主要论文:

[1] Wei, Y., Cai, C.F., Guo, Z.L., Wang, J.G., 2022. Linkage between aggregate stability of granitic soils and the permanent gully erosion in subtropical China. Soil and Tillage Research, 221, 105411.

[2] Wei, Y., Liu, Z., Zhang, Y., Cui, T.T., Guo, Z.L., Cai, C.F., Li, Z.X., 2022. Analysis of gully erosion susceptibility and spatial modelling using a GIS-based approach. Geoderma, 420, 115869.

[3] Zhou, X., Wei, Y.*, He, J., Cai, C.2022. Estimation of gully erosion rate and its determinants in a granite area of southeast China. Geoderma, 429, 116223.

[4] Wei, Y., Wu, X., Wang, J., Yu, H., Xia, J., Deng, Y., ... & Guo, Z. 2021. Identification of geo-environmental factors on Benggang susceptibility and its spatial modelling using comparative data-driven methods. Soil and Tillage Research, 208, 104857.

[5] Wei, Y., Liu, Z., Wu, X., Zhang, Y., Cui, T., Cai, C., ... & Cheng, D. 2021. Can Benggang be regarded as gully erosion? Catena, 207, 105648.

[6] Wei, Y., Wu, X., Zeng, R., Cai, C., & Guo, Z. 2020. Spatial variations of aggregate-associated humic substance in heavy-textured soils along a climatic gradient. Soil and Tillage Research, 197, 104497.

[7] Wei, Y., Wu, X., Xia, J., Zeng, R., Cai, C.*, Wang, T. 2019. Dynamic study of infiltration rate for soils with varying degrees of degradation by water erosion. International Soil and Water Conservation Research, 7(2): 167-175.

[8] Wei, Y., Wu, X., Xia, J., Miller, G. A., Cai, C.*, Guo, Z.*, Arash, H. 2019. The effect of water content on the shear strength characteristics of granitic soils in South China. Soil and Tillage Research, 187: 50-59.

[9] Xia, J., Cai, C., Wei, Y.*, Wu, X. 2019. Granite residual soil properties in collapsing gullies of south China: spatial variations and effects on collapsing gully erosion. Catena, 174: 469-477.

[10] Wei, Y., Wu, X., Li, X., Xia, J., Cai, C.*, Arash, H. 2018. A Novel and Facile Method for Characterizing Shrinkage Geometry along the Granitic Soil Profile. Soil Science Society of America Journal, 82(1):20-30.