陈超，男，汉族，湖南澧县人，博士后。2008年毕业于湖南农业大学工学院，获工学学士学位；2019年毕业于中国农业大学水利与土木工程学院，获工学博士学位；2023年从中国科学院教育部水土保持与生态环境研究中心博士后流动站出站。

主要经历

（1）2023-10 至今，银河yh0076，经济地理学院

（2）2019-02 至 2023-08，中国科学院教育部水土保持与生态环境研究中心，农业资源与环境，博士后，导师：雷廷武

（3）2013-09 至 2019-01，中国农业大学，农业水土工程，博士，导师：雷廷武

（4）2008-09 至 2012-06，湖南农业大学，水利水电工程专业，学士

研究方向

主要研究领域：土壤侵蚀与水土保持

课题成果

[1] 高海拔寒区融水土壤侵蚀机理与过程模拟研究，国家自然科学基金重点项目，41230746，2017年，参与。

主要论文

[1] Chen C, Ban Y, Wang X, et al. Measuring flow velocity on frozen and non-frozen slopes of black soil through leading edge method[J]. International Soil and Water Conservation Research, 2017, 5(3):180-189. （第一作者）

[2] Chen C, Ban Y, Lei T, et al. Water flow velocity over frozen and nonfrozen black soil slopes[J]. Hydrological Processes, 2017, 32(14):2231-2238. （第一作者）

[3] Chen C, Lei T, Ban Y, et al. Effects of slope lengths on rill erosion under different hydrodynamic conditions in black soil sloping farmland of Northeast China[J]. Transactions of the Chinese Society of Agricultural Engineering, 2019, 35(5),155-162. （第一作者）

[4] Chen C, Ban Y, Lei T, et al. Experimental study on soil erosion by concentrated waterflow affected by thawed soil depth[J]. CATENA, 2021,207, 105657. （第一作者）

[5] Chen C, Lei T, Ban Y. Influence of slope, flow rate, and thawed depth on soil detachment rate in partially thawed black soils[J]. Journal of Hydrology, 2021, Volume 603, Part C, 127009. （第一作者）

[6] Ban Y, Lei T, Liu Z, Chen C. Comparison of rill flow velocity over frozen and thawed slopes with electrolyte tracer method[J]. Journal of Hydrology, 2016,534:630-637.

[7] Wang, Y, Yang K, Tang Z, Chen C. The Effectiveness of the Consolidated Desert Surface by Mixing of Fly Ash and Polyacrylamide in Wind Erosion Control[J]. Water, Air & Soil Pollution, 2016, 227(12):429.

[8] Ban Y, Lei T, Chen C, et al. Meltwater erosion process of frozen soil as affected by thawed depth under concentrated flow in high altitude and cold regions[J]. Earth Surface Processes & Landforms, 2017, 42(13): 2139-2146.

[9] Ban Y, Lei T, Liu Z, Chen C. Comparative study of erosion processes of thawed and non-frozen soil by concentrated meltwater flow[J]. CATENA, 2017, 148: 153-159.

[10] Ban Y, Lei T, Chen C, et al. Study on the facilities and procedures for meltwater erosion of thawed soil[J]. International Soil & Water Conservation Research, 2016, 4(2): 142-147.

[11] Zhang J, Lei T, Qu L, Chen P, Chen C, et al. Method to measure soil matrix infiltration in forest soil[J]. Journal of Hydrology, 2017, 552: 241-248.

[12] Gao X, Li F, Chen C, et al. Effects of thawed depth on the sediment transport capacity by melt water on partially thawed black soil slope[J]. Land Degradation and Development, 2018(13), 1-10.

[13] Fen R, Wang F, Ban Y, Chen C. Method for estimating overland flow velocity on sandified slopes from measured solute transport process with bias errors[J]. Journal of Hydrology, 2020, 589, 125116.

[14] Zhang J, Lei T, Qu L, Zhang M, Chen P, Gao X, Chen C, et al. Method to quantitatively partition the temporal preferential flow and matrix infiltration in forest soil[J]. Geoderma,347, 150-159.