实时水沙运动方面的论文
1.陈波,范念念*,范晓玥,等.龙兴H11-M9水文测验无人船的研发及多场景应用.水利部防洪抗旱减灾工程技术研究中心（水旱灾害防御中心）,中国水利企业协会防灾与抢险装备技术分会.第四届防汛抗旱抢险新技术、新产品应用研讨会论文集.,2025:182-188.DOI:10.26914/c.cnkihy.2025.007440.
2.Niannian Fan, Qiang Zhong, Ruihua Nie, and Xingnian Liu. Interaction of various-sized particles in river flow. Scientific Reports 13, 10503 (2023).
3.Niannian Fan, Yushu Xie and Ruihua Nie. Bed load transport for a mixture of particle sizes: Downstream sorting rather than anomalous diffusion.Journal of Hydrology. 2017, 553: 26-34
4.Niannian Fan, Arvind Singh, Michele Guala, Efi Foufoula-Georgiou and Baosheng Wu. Exploring a semi-mechanistic Episodic Langevin model for bed load transport: emergence of normal and anomalous advection and diffusion regimes. Water Resources Research. 2016, 52: 2789-2801
5.Niannian Fan, Deyu Zhong, Baosheng Wu, Efi Foufoula-Georgiou, and Michele Guala. A mechanistic-stochastic formulation of bed load particle motions: from individual particle forces to the Fokker-Planck equation under low transport rates.Journal of Geophysical Research-Earth Surface, 2014, 119 (3): 464-482.
6.谢玉姝,范念念*,刘兴年.非均匀推移质颗粒的扩散与分选试验研究[J].四川大学学报(工程科学版), 2016,(05):58-65.
7.范念念,聂锐华,杨克君,刘兴年,陈日东.基于单颗粒受力的均匀推移质颗粒对流和扩散特征[J].水科学进展, 2016,(02):249-255.
8.王强,聂锐华,范念念,刘兴年.来沙条件变化对河床形态及推移质运动的影响研究，四川大学学报（工程科学版）, 2016, 48(增1), 20-24.
9.范念念,吴保生.基于随机-动力学模型的非均匀推移质扩散.浙江大学学报（工程科学版）, 2015, 49(02): 204-208
河流发育演化方面的论文
1.Yuqi Zhao, Niannian Fan *, Junshen Nie, Jordan T. Abell, Yu An, Zhangdong Jin, Chengshan Wang, Jiafu Zhang, Xingnian Liu and Ruihua Nie. From desiccation to re-integration of the Yellow River since the last glaciation. Geophysical Research Letters, 2023, 50, e2023GL103632. (自然指数期刊，https://doi. org/10.1029/2023GL103632)黄河流域水资源短缺，上世纪70至90年代多有断流，但在更长的时间尺度上，特别是末次冰盛期黄河是否有长期断流少有研究。带着该问题，本人自学跨学科知识和技能，全面构思，指导研究生开展该研究，通过野外考察取样，分析测试和数值模拟，得出2万年前黄河上游变为内流河，吉兰泰古湖为尾闾湖，水资源量仅为当今的三分之一。
2.NiannianFan,GuoxuanMa, YuAn, et al. The impact of natural and anthropogenic factors on erosion in the Northeastern loess Plateau, China, during the past 10,000 years. Catena, 2025,258(109292).黄土高原强烈的侵蚀，有多少是自然背景值，另外有多少是人类活动增加值？带着这个疑问，本人自学了跨学科知识，关注万年来黄土高原侵蚀的变化特征，全面构思设计，通过文献调研，野外考察采样，数值模拟等手段，得出人类活动使黄土高原侵蚀率增加了三倍。
3.NiannianFan,XingguoYang,M J Storozum, et al. Geoarchaeological evidence of an ancient landslide dam (13-4.7 ka) and consequent outburst flood on the Minjiang River near Wenchuan, China. Catena, 2024,242(108137).岷江上游地质灾害多发，且是新石器时代晚期以来重要的文明通道。研究表明13-4.7千年间汶川上游岷江干流被堵塞形成堰塞湖，促进了湖周围营盘山文化的发展，4.7千年堰塞湖消失，推动岷江上游文明向成都平原迁移。接受成都电视台采访并制作节目（https://www.zhihu.com/zvideo/1840923054722654208）。
4.GuoxuanMa,NiannianFan*, M J Storozum, et al. Late holocene overflow floods of the lower Yellow River led to the shrinkage of downstream lakes. Scientific Reports, 2025,15(402411).黄河下游多有两千多年来的决口改道历史记录，是否能找到对应的沉积证据？本文对古大野泽及周围展开实地调研，找到汉武帝时期瓠子决口，五代滑州决口的沉积证据，并表明东汉王景治河后黄河八百年安澜的历史推断是可靠的。
5.NiannianFan, Zhongxin Chu, Luguang Jiang, Hassan Marwan, Micheal P. Lamb and Xingnian Liu. Abrupt drainage basin reorganization following a Pleistocene river capture.Nature Communications. 2018.9,3756（Nature子刊）老家的河流上游能沿伸到哪里，是什么样子？这是不少人在儿童时期想过的问题。本人带着儿时的疑问，到中学时骑自行车沿途探索，发现老家的母亲河柴汶河上游有特殊的河流地貌特点。本人工作后采用专业方法，寻求合作，报道了证据确凿的河流袭夺，当地已进行开发。
6.Yuqi Zhao, Niannian Fan*, YuAn, et al. Co-evolution of palaeolakes in the Hetao Basin and the Yellow River over the last 500 ka. Palaeogeography Palaeoclimatology Palaeoecology, 2025,674(113038).
7.NiannianFan,XiaonanYan, HaoXie, et al. The largest outburst flood from the Paleo Hutiao Gorge landslide dam, Yangtze River since Late Pleistocene. Palaeogeography Palaeoclimatology Palaeoecology, 2025,678(113234).
8.Niannian Fan, Ping Kong, Jörg Christian Robl, Hongwei Zhou, Xianyan Wang, Zhangdong Jin, Xingnian Liu. Timing of river capture in major Yangtze River tributaries: Insights from sediment provenance and morphometric indices. Geomorphology. Volume 392, 2021, 107915
9.Niannian Fan, Ruihua Nie, Qiang Wang, and Xingnian Liu. Dramatic undercutting of piedmont rivers after the 2008 Wenchuan Ms 8.0 Earthquake,Scientific Reports. 2016, 6, 37108.
10.Shan Zheng*, Songyi Li, Xiongdong Zhou, Niannian Fan*, Huiqun Cao, Ruihua Nie, Yuhong Zeng. Relationships between morphological quality and macroinvertebrate diversity in a degrading gravel-bed river following the magnitude 8.0 Wenchuan earthquake, China, Geomorphology, 2023, 108821
11.Qiuyue Zhao, Shuzhen Peng, Niannian Fan, et al. Luminescence chronology of loess-palaeosol deposits in the Central Shandong Mountains region: Provenances and paleoclimate implications. QUATERNARY GEOCHRONOLOGY, 2022,70(101296).
12.安宇，范念念*，徐志伟，刘兴年.基于碎屑锆石的黄土高原—毛乌素交界区石峁黄土粉尘物源估算.古地理学报. 2022(04): 802-812.
13.程雪峰，范念念*，刘维明，杨兴国，刘兴年.两万年来岷江汶川古堰塞湖事件研究.山地学报, 2020, 38(4):1-10.
14.聂锐华,王小凡,刘发明,王强,范念念*,刘兴年.强震受损山前河流河床演变研究.工程科学与技术,2018,(5):105-111.
15.顾继一,范念念*,刘兴年.山区河流河床基岩暴露与沙卵石覆盖反常关系研究——以陇西河为例[J].工程科学与技术,2017,(S1):44-49.
16.赵秋月，臧凯旋，彭淑贞，周锐，范念念，丁敏，方慜，吉春雯.2022.末次冰期以来青州黄土光释光测年及其对古气候的指示[J].地球环境学报,13(3):281-295
17.赵秋月,张文琪,丁敏,赖忠平,方慜,彭淑贞，刘宁，臧凯旋，宋波，范念念. (2022).倒数第二次间冰期以来黄河下游冲洪积物释光年代及其古气候意义.第四纪研究(005), 042.
18.范念念,吴保生,田富强.沙地地区水文过程及模拟——以秃尾河流域为例.水文, 2013, 01: 12-17.
19.范念念,吴保生,刘乐.地震导致河流改道与古蜀文明的变迁.山地学报, 2010, 04: 453-462
20.范念念,薛小妮.窟野河泥沙输移与冲淤特征分析.泥沙研究,2010,(02): 75-80.
21.范念念,李慧奇,田苏茂,马宇.黄河河潼区间泥沙与洪水复杂响应分析.水土保持通报,2009,(03): 216-219.
22.范念念.秃尾河水沙冲淤特征与变化趋势分析.西北水电,2008,(03): 1-3.
23.Daljit Sandhu, Singh Arvind, Fan Niannian, Wang Dingbao and Steven J. Duranceaua. Hydro-geomorphic response of Everglades to changing climate and anthropogenic activities.Journal of Hydrology. 2016, 543: 861–872
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