[1]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(05):155-163.[doi:10.13869/j.cnki.rswc.2024.05.012]
Copy

Relationship Between Gully Slope Slumping Erosion Characteristics and Topographic Factors in Bare Sandstone Area

References:
[1]刘秉正,吴发启.黄土塬区沟谷侵蚀与发展[J].西北林学院学报,1993,8(2):7-15.
Liu B Z, Wu F Q. Gully erosion and its development on Loess Plateau[J]. Journal of Northwest Forestry University, 1993,8(2):7-15.
[2]李育鸿.黄土残塬区泻溜侵蚀土体水分物理性质研究[J].人民黄河,2018,40(8):96-98,119.
Li Y H. Research on hydro-physical properties of slumping erosion in remained loess area[J]. Yellow River, 2018,40(8):96-98,119.
[3]高健健,艾琦森,韩立钦,等.2017—2018年黄土丘陵沟壑区第一副区辛店沟流域重力侵蚀观测数据集[J].中国科学数据,2021,6(3):113-120.
Gao J J, Ai Q S, Han L Q, et al. An observation-based dataset of gravity erosion of Xindiangou watershed in the first sub-region of Loess Hilly-Gully Region during 2017—2018[J]. China Scientific Data, 2021,6(3):113-120.
[4]王斌科.海东黄土区的泻溜侵蚀[J].中国水土保持,1990(5):25-26.
Wang B K. The erotic erosion of loess area of Haidong city[J]. Soil and Water Conservation in China, 1990(5):25-26.
[5]曾伯庆,马文中,张治国,等.三趾马红土泻溜侵蚀规律研究[J].中国水土保持,1991(7):21-25,51.
Zeng B Q, Ma W Z, Zhang Z G, et al. Study on erosion of slumping in sanzhima red day area[J]. Soil and Water Conservation in China, 1991(7):21-25.
[6]涂安千.“红土”陡坡的泻溜侵蚀及其防治[J].水土保持通报,1981,1(4):29-34.
Tu A Q. Sluggish erosion of ‘red soil' steep slope and its prevention and control[J]. Bulletin of Soil and Water Conservation, 1981,1(4):29-34.
[7]柴亚凡,周波,吕文强,等.人工模拟降雨条件下泻溜红土坡积体的侵蚀过程和入渗特征[J].中国水土保持科学,2019,17(1):10-15.
Chai Y F, Zhou B, Lü W Q, et al. Erosion process and infiltration features of red soil slumping slope sediment under artificial simulated rainfall condition[J]. Science of Soil and Water Conservation, 2019,17(1):10-15.
[8]Kuhn J N, Oost V K, Cammeraat E. Soil erosion, sedimentation and the carbon cycle[J]. Catena, 2012,94:1-2.
[9]张建文,李鹏,高海东,等.覆沙坡面微地形变化与侵蚀产沙的响应关系[J].干旱区研究,2020,37(3):757-764.
Zhang J W, Li P, Gao H D, et al. Response relationship between micro-relief variation and slope erosion under sand-covered conditions[J]. Arid Zone Research, 2020,37(3):757-764.
[10]王莹,郑子成,李廷轩,等.水蚀过程中玉米生长季横垄坡面地表糙度变化及其与侵蚀量的关系[J].中国水土保持科学,2018,16(6):31-37.
Wang Y, Zheng Z C, Li T X, et al. Change of soil surface roughness during maize growing season and its relationship with soil erosion amount on slope of contour tillage during water erosion process[J]. Science of Soil and Water Conservation, 2018,16(6):31-37.
[11]丁琳,刘辉.延河流域沟壑密度统计学特征及影响因素分析[J].安徽农学通报,2016,22(14):108-110,116.
Ding L, Liu H. Characteristics of gully density in the Yanhe River Basin and its influencing factors[J]. Anhui Agricultural Science Bulletin, 2016,22(14):108-110,116.
[12]Morbidelli R, Saltalippi C, Flammini A, et al. Infiltration on sloping surfaces:Laboratory experimental evidence and implications for infiltration modeling[J]. Journal of Hydrology, 2015,523:79-85.
[13]钱秋颖,秦富仓,李龙,等.自然降雨条件下坡面侵蚀地表粗糙度的空间异质性[J].水土保持学报,2021,35(3):46-52.
Qian Q Y, Qin F C, Li L, et al. Spatial heterogeneity of surface roughness of slope erosion under natural rainfall[J]. Journal of Soil and Water Conservation, 2021,35(3):46-52.
[14]Zheng Z C, He S Q, Wu F Q. Changes of soil surface roughness under water erosion process[J]. Hydrological Processes, 2014,28(12):3919-3929.
[15]王靖滢.地表起伏度与区域水土流失的相关性分析[D].重庆:重庆师范大学,2014.
Wang J Y. The correlation analysis between relief degree of land surface and regional scale of soil erosion intensity in Chongqing City[D]. Chongqing:Chongqing Normal University, 2014.
[16]吴秉校,侯雷,宋敏敏,等.基于汇流累积计算的沟壑密度分析方法[J].水土保持研究,2017,24(3):39-44.
Wu B X, Hou L, Song M M, et al. Gully density analysis based on flow accumulation method[J]. Research of Soil and Water Conservation, 2017,24(3):39-44.
[17]陈学兄,张小军,常庆瑞.陕西省地形起伏度最佳计算单元研究[J].水土保持通报,2016,36(3):265-270,370.
Chen X X, Zhang X J, Chang Q R. A study on optimal statistical unit for relief amplitude of land surface in Shaanxi Province[J]. Bulletin of Soil and Water Conservation, 2016,36(3):265-270,370.
[18]郑子成.坡面水蚀过程中地表糙度的作用及变化特征研究[D].陕西杨凌:西北农林科技大学,2007.
Zheng Z C. Study on the effect and change characteristic of soil surface roughness during the course of water erosion[D]. Yangling,Shaanxi:Northwest A&F University, 2007.
[19]文慧,倪世民,冯舒悦,等.赣南崩岗的发育阶段及部位对土壤水力性质的影响[J].农业工程学报,2019,35(24):136-143.
Wen H, Ni S M, Feng S Y, et al. Effects of developmental stages and parts of collapsing gully on soil hydraulic properties in southern Jiangxi[J]. Transactions of the Chinese Society of Agricultural Engineering, 2019,35(24):136-143.
[20]徐加盼,王秋霞,邓羽松,等.基于三维激光扫描技术的花岗岩风化土体侵蚀表面特征研究[J].水土保持学报,2016,30(2):14-19.
Xu J P, Wang Q X, Deng Y S, et al. Study on characteristics of erosion surface on weathered granite soil based on three-dimensional laser scanning technology[J]. Journal of Soil and Water Conservation, 2016,30(2):14-19.
[21]张鹏,郑粉莉,王彬,等.高精度GPS,三维激光扫描和测针板三种测量技术监测沟蚀过程的对比研究[J].水土保持通报,2008,28(5):11-15.
Zhang P, Zheng F L, Wang B, et al. Comparative study of monitoring gully erosion morphology change process by using high precision GPS, leica HDS 3000 laser scanner and needle board method[J]. Bulletin of Soil and Water Conservation, 2008,28(5):11-15.
[22]李明,杜继稳,高维英.陕北黄土高原区地质灾害与降水关系[J].干旱区研究,2009,26(4):599-606.
Li M, Du J W, Gao W Y. Study on the relationship between geological disasters and precipitation in the Loess Plateau in North Shaanxi Province[J]. Arid Zone Research, 2009,26(4):599-606.
[23]严桥.多种降雨条件下沟坡重力侵蚀过程模型试验[D].辽宁大连:大连理工大学,2013.
Yan Q. Simulation of gravitational erosion in the loess gully wall based on various rainfall condition[D]. Dalian, Liaoning:Dalian University of Technology, 2013.
[24]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(6):21-27,35.
Zhang R X, Qin F C, Li L, et al. Responses of slope microgeomorphology to erosion and sediment yield in arsenic sandstone area[J]. Research of Soil and Water Conservation, 2022,29(6):21-27,35.
[25]梁心蓝.水蚀过程中地表糙度变化及侵蚀响应[D].陕西杨凌:西北农林科技大学,2015.
Liang X L. Soil surface roughness change and erosion response in the process of water erosion[D]. Yangling, Shaanxi:Northwest A & F University, 2015.
[26]唐辉,李占斌,李鹏,等.模拟降雨下坡面微地形量化及其与产流产沙的关系[J].农业工程学报,2015,31(24):127-133.
Tang H, Li Z B, Li P, et al. Surface micro topography quantification and its relationship with runoff and sediment under simulated rainfall[J]. Transactions of the Chinese Society of Agricultural Engineering, 2015,31(24):127-133.
[27]张文博.土壤结构体对工程堆积体坡面侵蚀产沙及微地形的影响[D].陕西杨凌:西北农林科技大学,2020.
Zhang W B. Effects of soil structure on erosion sediment yield and surface roughness of engineering piles[D]. Yangling,Shaanxi:Northwest A&F University, 2020.
[28]李清溪,丁文峰,朱秀迪,等.雨强和地表糙度对坡面微地形及侵蚀的影响[J].长江科学院院报,2019,36(1):41-47.
Li Q X, Ding W F, Zhu X D, et al. Effects of rainfall intensity and land surface roughness on microtopography and runoff and sediment yield of slope[J]. Journal of Changjiang River Scientific Research Institute, 2019,36(1):41-47.
[29]赵斯琦,王晓红,舒天竹,等.喀斯特地区区域尺度土壤侵蚀地形因子研究[J].干旱区资源与环境,2018,32(5):97-103.
Zhao S Q, Wang X H, Shu T Z, et al. Research on topographic factors in relation to regional soil erosion in Karst Region[J]. Journal of Arid Land Resources and Environment, 2018,32(5):97-103.
[30]乔荣荣,季树新,白雪莲,等.流域沟壑数量特征与侵蚀量关系[J].中国水土保持科学(中英文),2020,18(6):9-14.
Qiao R R, Ji S X, Bai X L, et al. Relationship between gully quantitative characteristics and soil erosion amount[J]. Science of Soil and Water Conservation, 2020,18(6):9-14.
Similar References:

Memo

-

Last Update: 2024-08-10

Online:276       Total Traffic Statistics:27135006

Website Copyright: Research of Soil and Water Conservation Shaanxi ICP No.11014090-10
Tel: 029-87012705 Address: Editorial Department of Research of Soil and Water Conservation, No. 26, Xinong Road, Yangling, Shaanxi Postcode: 712100