[1] HU Sheng,QIU Haijun,WANG Ninglian,et al.The influence of loess cave development upon landslides and geomorphologic evolution:a case study from the northwest Loess Plateau,China[J].Geomorphology,2020,359:107167. [2] 张卜平,朱兴华,成玉祥,等.黄土潜蚀机理及其致灾效应研究综述[J].中国地质灾害与防治学报,2021,32(6):41-52. [3] 彭建兵,李喜安,孙萍,等.黄土洞穴的环境灾害效应[J].地球与环境,2005,33(4):5-11. [4] 雒林林,张超.黄土陷穴对长输管道建设的危害与防治[J].油气田地面工程,2013,32(9):137. [5] 李喜安,彭建兵,马润勇,等.黄土洞穴危害及其形成演化机制[J].西安科技大学学报,2009,29(6):737-741. [6] 李喜安,彭建兵,郑书彦,等.公路黄土洞穴灾害与水土流失研究[J].公路,2004,(12):70-73. [7] 李喜安,彭建兵,郑书彦,等.湿陷性黄土地区土壤洞穴侵蚀模式研究[J].水土保持研究,2005,12(6):25-27. [8] PENG Jianbing,SUN Ping,IGWE O,et al.Loess caves,a special kind of geo-hazard on Loess Plateau,Northwestern China[J].Engineering Geology,2018,236:79-88. [9] FULLER M L.Some unusual erosion features in the loess of China[J].Geographical Review,1922,12(4):570. [10] 王斌科.土壤的洞穴侵蚀研究综述[J].土壤学进展,1989,17(1):9-14. [11] 朱显谟.黄土区的洞穴侵蚀[J].黄河建设,1958(3):43-44. [12] 陈传康.陇东东南部黄土地形类型及其发育规律[J].地理学报,1956,11(3):223-231. [13] VAN DEN EECKHAUT M,POESEN J,DUSAR M,et al.Sinkhole formation above underground limestone Quarries:a case study in South Limburg (Belgium)[J].Geomorphology,2007,91(1/2):19-37. [14] JOUVES J,VISEUR S,ARFIB B,et al.Speleogenesis,geometry,and topology of caves:a quantitative study of 3D Karst conduits[J].Geomorphology,2017,298:86-106. [15] SZCZYGIEŁ J,GOLICZ M,HERCMAN H,et al.Geological constraints on cave development in the plateau-gorge Karst of South China(Wulong,Chongqing)[J].Geomorphology,2018,304:50-63. [16] BALLESTEROS D,GIRALT S,GARCÍA-SANSEGUNDO J,et al.Quaternary regional evolution based on Karst cave geomorphology in Picos de Europa (Atlantic Margin of the Iberian Peninsula)[J].Geomorphology,2019,336:133-151. [17] 彭建兵,李庆春,陈志新,等.黄土洞穴灾害[M].北京:科学出版社,2008. [18] 郑炜珊,耿豪鹏,潘保田.兰州青水村黄土陷穴的侵蚀临界研究[J].兰州大学学报(自然科学版),2020,56(3):326-332. [19] 齐威.黄土陷穴的自动提取与分析研究:以定西市典型样区为例[D].南京:南京信息工程大学,2017. [20] 丁浒.融合地形特征的影像深度分割方法研究:以黄土微地貌为例[D].南京:南京师范大学,2019. [21] 王毅,方志策,牛瑞卿,等.基于深度学习的滑坡灾害易发性分析[J].地球信息科学学报,2021,23(12):2244-2260. [22] 王世宝,庄建琦,郑佳,等.基于深度学习的CZ铁路康定—理塘段滑坡易发性评价[J].工程地质学报,2022,30(3):908-919. [23] 李辉山,白莲,刘平.基于DNN神经网络的地铁洪涝灾害评估研究[J].铁道标准设计,2022,66(12):131-136. [24] SONG Xiaodong,BRUS D J,LIU Feng,et al.Mapping soil organic carbon content by geographically weighted regression:a case study in the Heihe River Basin,China[J].Geoderma,2016,261:11-22. [25] 胡永占.陇西地区黄土陷穴成因分析及形成机理[J].铁道工程学报,2013,30(3):1-4. [26] 李喜安,彭建兵,郑书彦,等.黄土高原地区黄土洞穴的成因研究[J].公路,2005(11):147-151. [27] 郑炜珊.黄土高原洞穴的发育特征及其影响因素研究[D].兰州:兰州大学,2021. [28] 武翠翠,王世杰.黄河流域兰州段土壤侵蚀敏感性评价[J].科学技术与工程,2021,21(29):12390-12397. [29] WISCHMEIER W H.Predicting rainfall-erosion losses from cropland east of the Rocky Mountains,guide for selection of practices for soil and water conservation[J].United States Government Printing Office,1965:282. [30] 刘宝元,毕小刚,符素华,等.北京土壤流失方程[M].北京:科学出版社,2010. [31] WISCHMEIER W H,SMITH D D.Rainfall energy and its relationship to soil loss[J].Transactions,American Geophysical Union,1958,39(2):285-291. [32] WILLIAMS J R,DYKE P T,JONES C A.Epic-a model for assessing the effects of erosion on soil productivity[M]//Developments in Environmental Modelling.Amsterdam:Elsevier,1983:553-572. [33] 蔡崇法,丁树文,史志华,等.应用USLE模型与地理信息系统IDRISI预测小流域土壤侵蚀量的研究[J].水土保持学报,2000,14(2):19-24. [34] 郭达,宋小宁,董震,等.基于RUSLE与GIS的黄土高原水土流失评价研究:以宁夏中卫地区为例[J].泥沙研究,2020,45(5):55-60. [35] 胡克志.黄土高原不同生物气候区土壤侵蚀动态变化研究[J].人民长江,2016,47(13):16-23. [36] 周飞燕,金林鹏,董军.卷积神经网络研究综述[J].计算机学报,2017,40(6):1229-1251. [37] GU Jiuxiang,WANG Zhenhua,KUEN J,et al.Recent advances in convolutional neural networks[J].Pattern Recognition,2018,77:354-377. [38] 袁群勇.深度神经网络的训练优化方法研究[D].广州:华南理工大学,2020. [39] 郑炜珊,耿豪鹏,顾国强,等.定西于家山黄土洞穴的分布特征与侵蚀临界研究[J].水土保持学报,2020,34(4):112-117. [40] 杨昕,汤国安,袁宝印,等.黄土高原勺状沟壑特征及发育过程[J].地理研究,2021,40(7):1870-1886. |