[1] 张攀,姚文艺,刘国彬,等.土壤复合侵蚀研究进展与展望[J].农业工程学报,2019,35(24):154-161.[2] 殷水清,薛筱婵,岳天雨,等.中国降雨侵蚀力的时空分布及重现期研究[J].农业工程学报,2019,35(9):105-113.[3] Mark A N, Yin S Q, Pasquale B, et al. Rainfall erosivity:A historical review[J]. Catena, 2017,157:357-362.[4] Alavinia M, Saleh F N, Asadi H, et al. Effects of rainfall patterns on runoff and rainfall-induced erosion[J]. International Journal of Sediment Research, 2019,34(3):270-278.[5] Dakhlalla A O, Parajuli P B. Evaluation of the best management practices at the watershed scale to attenuate peak streamflow under climate change scenarios[J]. Water Resources Management, 2016,30(3):963-982.[6] 林庆明,丁文峰,张长伟,等.模拟降雨条件下红壤坡面侵蚀产沙水动力学特征[J].水土保持通报,2019,39(2):16-21.[7] 陈戎欣,吕锡芝,倪用鑫,等.人工降雨下草被对黄土丘陵沟壑区坡面径流的调控及临界阈值[J].生态环境学报,2020,29(1):122-128.[8] 刘晓燕,李晓宇,高云飞,等.黄土丘陵沟壑区典型流域产沙的降雨阈值变化[J].水利学报,2019,50(10):1177-1188.[9] 沈海鸥,刘健,王宇,等.降雨强度和坡度对黑土区土质道路路面侵蚀特征的影响[J].水土保持学报,2017,31(6):123-126.[10] Emeh C, Igwe O. Variations in soils derived from an erodible sandstone formation and factors controlling their susceptibility to erosion and landslide[J]. Journal of the Geological Society of India, 2017,90(3):362-370.[11] Bruthans J, Soukup J, Vaculikova J, et al. Sandstone landforms shaped by negative feedback between stress and erosion[J]. Nature Geoscience, 2014,7(8):597-601.[12] Vecchio J D, Dibiase R A, Denn A R, et al. Record of coupled hillslope and channel response to Pleistocene erosion and deposition in a sandstone headwater valley, central Pennsylvania[J]. Geological Society of America Bulletin, 2018,130(11/12):1903-1917.[13] 王愿昌,吴永红,寇权,等.砒砂岩分布范围界定与类型区划分[J].中国水土保持科学,2007,5(1):14-18.[14] 张汉雄.黄土高原的暴雨特性及其分布规律[J].地理学报,1983,83(4):416-425.[15] 谢云,刘宝元,章文波.侵蚀性降雨标准研究[J].水土保持学报,2000,14(4):6-11.[16] 王万忠,焦菊英.中国的土壤侵蚀因子定量评价研究[J].水土保持通报,1996,16(5):1-20.[17] 杨振奇,秦富仓,李旻宇,等.砒砂岩区不同土地利用类型土壤入渗性能及其影响因素研究[J].生态环境学报,2020,29(4):733-739.[18] 杨振奇,秦富仓,李龙,等.砒砂岩区小流域土壤有机质空间分布特征及其影响因素[J].农业工程学报,2019,35(17):154-161.[19] 高光耀,傅伯杰,吕一河,等.干旱半干旱区坡面覆被格局的水土流失效应研究进展[J].生态学报,2013,33(1):12-22.[20] 于国强,李占斌,李鹏,等.不同植被类型的坡面径流侵蚀产沙试验研究[J].水科学进展,2010,21(5):593-599.[21] 余新晓,张晓明,武思宏,等.黄土区林草植被与降水对坡面径流和侵蚀产沙的影响[J].山地学报,2006,24(1):19-26.[22] 陈丽华,张艺,余新晓,等.北京山区典型森林植被林冠截留特征及模拟[J].应用基础与工程科学学报,2013,21(3):423-431.[23] 王改玲,王青杵,石生新.晋北黄土区降雨特征及其对坡地土壤侵蚀的影响[J].水土保持学报,2013,27(1):1-5.
[1]普隽泽,吕锡芝,张秋芬,等.黄土丘陵沟壑区典型草被产流产沙特征及其影响因素[J].水土保持研究,2023,30(02):1.[doi:10.13869/j.cnki.rswc.2023.02.015]
PU Junze,Lv Xizhi,ZHANG Qiufen,et al.Characteristics and Influencing Factors of Runoff and Sediment Yield of Typical Grassland in Loess Hilly and Gully Region[J].Research of Soil and Water Conservation,2023,30(01):1.[doi:10.13869/j.cnki.rswc.2023.02.015]
[2]赵文卓,秦富仓,董晓宇,等.裸露砒砂岩区沟坡泻溜侵蚀特征与地形因子的关系[J].水土保持研究,2024,31(05):155.[doi:10.13869/j.cnki.rswc.2024.05.012]
Zhao Wenzhuo,Qin Fucang,Dong Xiaoyu,et al.Relationship Between Gully Slope Slumping Erosion Characteristics and Topographic Factors in Bare Sandstone Area[J].Research of Soil and Water Conservation,2024,31(01):155.[doi:10.13869/j.cnki.rswc.2024.05.012]
收稿日期:2020-12-14 修回日期:2021-01-11资助项目:内蒙古自治区科技兴蒙行动重点专项“十大孔兑综合治理与水资源集约高效利用集成示范”(KJXM-EEDS-2020005); 内蒙古自治区科技计划项目“黄河十大孔兑流域生态修复空间精准识别与智慧水土保持技术”(2021GG0052)第一作者:杨振奇(1993—),男,内蒙古赤峰市人,博士,工程师,主要从事水土保持与荒漠化防治方面的研究。E-mail:843296578@qq.com通信作者:郭建英(1979—),男,内蒙古呼和浩特市人,高级工程师,硕士生导师,主要从事水土保持、矿区生态修复等方面的科研工作。E-mail:guojianying1980@126.com