[1]李 龙,张尚轩,高鑫宇,等.次降雨下砒砂岩坡面细沟形态发育及其对侵蚀产沙的影响[J].水土保持研究,2023,30(03):1-9.[doi:10.13869/j.cnki.rswc.2023.03.008]
 LI Long,ZHANG Shangxuan,HE Jun,et al.Development of Rill Morphology on Sandstone Slopes Under Individual Rainfall Event and Its Effect on Erosion and Sediment Production[J].Research of Soil and Water Conservation,2023,30(03):1-9.[doi:10.13869/j.cnki.rswc.2023.03.008]
点击复制

次降雨下砒砂岩坡面细沟形态发育及其对侵蚀产沙的影响

参考文献/References:

[1] 肖培青,郑粉莉,汪晓勇,等.黄土坡面侵蚀方式演变与侵蚀产沙过程试验研究[J].水土保持学报,2008,22(1):24-27.
[2] He J J, Sun L Y, Gong H L, et al. Laboratory Studies on the influence of rainfall pattern on rill erosion and its runoff and sediment characteristics[J]. Land Degradation and Development, 2017,28:1615-1625.
[3] 裴冠博,龚冬琴,付兴涛.晋西黄绵土坡面细沟形态及其对产流产沙的影响[J].水土保持学报,2017,31(6):79-84,182.
[4] 张宽地,王光谦,吕宏兴,等.模拟降雨条件下坡面流水动力学特性研究[J].水科学进展,2012,23(2):229-235.
[5] 郑良勇,李占斌,李鹏,等.稀土元素示踪坡面次降雨条件下的侵蚀过程[J].农业工程学报,2010,26(3):87-91.
[6] Shi Z H, Fang N F, Wu F Z, et al. Soil erosion processes and sediment sorting associated with transport mechanisms on steep slopes[J]. Journal of Hydrology, 2012,455(3):123-130.
[7] 耿晓东.主要水蚀区坡面土壤侵蚀过程与机理对比研究[D].陕西杨凌:中国科学院水土保持与生态环境研究中心,2010.
[8] Bryan R B. Soil erodibility and processes of water erosion on hillslope[J]. Geomorphology, 2000,32(3):385-415.
[9] 郝好鑫,郭忠录,王先舟,等.降雨和径流条件下红壤坡面细沟侵蚀过程[J].农业工程学报,2017,33(8):134-140.
[10] Meyer L D, Foster G R, Romkens M J M. Source of soil eroded by water from upland slopes[J]. Agricultural Research Service Report, 1975,40:177-189.
[11] Yan M J, HaiJ S, Zhong M W, et al. The dynamic process of slope rill erosion analyzed with a digital close range photogrammetry observation system under laboratory conditions[J]. Geomorphology, 2020,350:106893.
[12] 赵新凯,龚家国,任政,等.黒垆土坡面细沟形态演变规律试验研究[J].水利水电技术,2020,51(2):205-212.
[13] 黎武.基于三维激光扫描的坡面细沟形态演化研究[D].四川南充:西华师范大学,2018.
[14] 张若曦,秦富仓,李龙,等.水力侵蚀对砒砂岩区土壤有机碳空间变异性的影响[J].水土保持学报,2020,34(6):117-124.
[15] 常平,李晓丽,李明玉,等.冲蚀条件下砒砂岩坡面细沟侵蚀特性分析[J].人民黄河,2018,40(5):98-102,106.
[16] 胡剑汝.基于WEPP的坡面尺度砒砂岩复合侵蚀治理生态水文效应评价[D].北京:北京林业大学,2019.
[17] 常平.冲蚀条件下砒砂岩坡面水力侵蚀特性试验研究[D].呼和浩特:内蒙古农业大学,2018.
[18] 沈海鸥,郑粉莉,温磊磊,等.雨滴打击对黄土坡面细沟侵蚀特征的影响[J].农业机械学报,2015,46(8):104-112,89.
[19] 胡伟,翟星雨,李浩,等.黑土区农地集水区次降雨径流与输沙特征研究[J].土壤与作物,2019,8(4):405-414.
[20] Shen H O, Zheng F L, Wen L L, et al. An experimental study of rill erosion and morphology [J]. Geomorphology, 2014,231(231):193-201.
[21] 雷廷武, Nearing M A.侵蚀细沟水力学特性及细沟侵蚀与形态特征的试验研究[J].水利学报,2000,31(11):49-54.
[22] 何育聪,郑浩杰,韩剑桥.间歇性与连续性降雨对黄土坡面细沟侵蚀影响的比较[J].水土保持学报,2020,34(6):8-13.
[23] 王颢霖,焦菊英,唐柄哲,等.陕北子洲“7·26”暴雨后坡耕地细沟侵蚀及其影响因素分析[J].农业工程学报,2019,35(11):122-130.
[24] 王莹.紫色土坡面细沟侵蚀发育过程研究[D].成都:四川农业大学,2019.
[25] 张攀,姚文艺,唐洪武,等.黄土坡面细沟形态变化及对侵蚀产沙过程的影响[J].农业工程学报,2018,34(5):114-119.
[26] Ou X Y, Hu Y X, Li X W, et al. Advancements and challenges in rill formation, morphology, measurement and modeling[J]. Catena, 2021,196:104932.
[27] 张建文.覆沙坡面细沟侵蚀发育过程与形态特征研究[D].西安:西安理工大学,2020.
[28] 郭明明,王文龙,李建明,等.野外模拟降雨条件下矿区土质道路径流产沙及细沟发育研究[J].农业工程学报,2016,32(24):155-163.
[29] Shi Q H, Wang W L, Guo M M, et al. The impact of flow discharge on the hydraulic characteristics of headcut erosion processes in the gully region[J]. Chinese Journal of Applied Ecology, 2018,29(12):3891-3899.
[30] 霍云云,吴淑芳,冯浩,等.基于三维激光扫描仪的坡面细沟侵蚀动态过程研究[J].中国水土保持科学,2011,9(2):32-37,46.
[31] 速欢,王文龙,康宏亮,等.露天矿排土场平台—边坡系统侵蚀形态及径流产沙特征[J].应用生态学报,2020,31(9):3194-3206.
[32] 张攀,唐洪武,姚文艺,等.细沟形态演变对坡面水沙过程的影响[J].水科学进展,2016,27(4):535-541.
[33] 赵宇,陈晓燕,米宏星,等.基于体积法对黄土细沟侵蚀沿程分布模拟的研究[J].土壤学报,2014,51(6):1234-1241.

相似文献/References:

[1]张扬,赵世伟,侯庆春.草地植被恢复对次降雨土壤水分动态的影响分析[J].水土保持研究,2009,16(03):70.
 ZHANG Yang,ZHAO Shi-wei,HOU Qing-chun.Effects of Vegetation Restoration on Soil Water Dynamics of Individual Rainfall in Typical Steppe[J].Research of Soil and Water Conservation,2009,16(03):70.
[2]于国强,贾莲莲,朱冰冰,等.不同坡位的植被缓冲带对坡面侵蚀产沙来源的影响[J].水土保持研究,2020,27(06):9.
 YU Guoqiang,JIA Lianlian,ZHU Bingbing,et al.Effect of Vegetation Buffers of Different Positions on Sediment Source in the Slope[J].Research of Soil and Water Conservation,2020,27(03):9.
[3]张若曦,秦富仓,李 龙,等.砒砂岩区坡面微地貌变化与侵蚀产沙的响应关系[J].水土保持研究,2022,29(06):21.
 ZHANG Ruoxi,QIN Fucang,LI Long,et al.Responses of Slope Micro-geomorphology to Erosion and Sediment Yield in Arsenic Sandstone Area[J].Research of Soil and Water Conservation,2022,29(03):21.

备注/Memo

收稿日期:2022-03-06 修回日期:2022-04-14
资助项目:国家自然科学基金“砒砂岩坡面侵蚀时空变异与植被斑块格局演变互馈机制”(42267049); 内蒙古教育厅“高等教育改革发展项目—青年科技英才计划”(NJYT22046); 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:李龙(1989—)男,吉林桦甸人,副教授,博士,主要从事土壤侵蚀及水土保持相关研究。E-mail:lilongdhr@126.com

更新日期/Last Update: 2023-04-10