• Journal of Geographical Sciences
  • Vol. 30, Issue 3, 468 (2020)
Yanjun WANG, Baosheng WU*, and Deyu ZHONG
Author Affiliations
  • State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084, China
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    DOI: 10.1007/s11442-020-1738-3 Cite this Article
    Yanjun WANG, Baosheng WU, Deyu ZHONG. Adjustment in the main-channel geometry of the lower Yellow River before and after the operation of the Xiaolangdi Reservoir from 1986 to 2015[J]. Journal of Geographical Sciences, 2020, 30(3): 468 Copy Citation Text show less
    References

    [1] Z X Chu. The dramatic changes and anthropogenic causes of erosion and deposition in the lower Yellow (Huanghe) River since 1952. Geomorphology, 216, 171-179(2014).

    [2] B L Cui, X L Chang, W Y Shi. Abrupt changes of runoff and sediment load in the lower reaches of the Yellow River, China. Water Resources, 41, 252-260(2014).

    [3] S V M Dirk, M Yang, Z B Wang. Predicting the morphodynamic response of silt-laden rivers to water and sediment release from reservoirs: Lower Yellow River, China. Journal of Hydraulic Engineering, 137, 90-99(2011).

    [4] D X Kong, C Y Miao, J W Wu et al. Bi-objective analysis of water-sediment regulation for channel scouring and delta maintenance: A study of the Lower Yellow River. Global and Planetary Change, 133, 27-34(2015).

    [5] D X Kong, C Y Miao, J W Wu et al. The hydro-environmental response on the lower Yellow River to the water-sediment regulation scheme. Ecological Engineering, 79, 69-79(2015).

    [6] J Li, J Q Xia, M L Zhou et al. Variation in reach-scale thalweg-migration intensity in a braided reach of the Lower Yellow River in 1986-2015. Earth Surface Processes and Landforms, 42, 1952-1962(2017).

    [7] Z C Lu, S F Chen, H Chen. The evolutionary tendency forecast of channel morphology and river state of the wandering braided rivers in the Lower Yellow River. Acta Geographica Sinica, 55, 729-736(2000).

    [8] Y X Ma, H Q Huang, G C Nanson et al. Channel adjustments in response to the operation of large dams: The upper reach of the Lower Yellow River. Geomorphology, 147/148, 35-48(2012).

    [9] C Y Miao, D X Kong, J W Wu et al. Functional degradation of the water-sediment regulation scheme in the Lower Yellow River: Spatial and temporal analyses. The Science of the Total Environment, 551/552, 16-22(2016).

    [10] J Peng, S L Chen, P Dong. Temporal variation of sediment load in the Yellow River basin, China, and its impacts on the lower reaches and the river delta. Catena, 83, 135-147(2010).

    [11] J Peng, S L Chen, F Liu et al. Erosion and siltation processes in the Lower Yellow River during different river courses into the sea. Acta Geographica Sinica, 65, 613-622(2010).

    [12] Z Y Sun, W Z Wang, Y Li et al. Can the narrowing of the Lower Yellow River by regulation result in non-siltation and even channel scouring?. Journal of Geographical Sciences, 26, 1337-1348(2016).

    [13] S M Tian, W H Wang, B F Xie et al. Fluvial processes of the downstream reaches of the reservoirs in the Lower Yellow River. Journal of Geographical Sciences, 26, 1321-1336(2016).

    [14] H J Wang, N S Bi, Y Saito et al. Recent changes in sediment delivery by the Huanghe (Yellow River) to the sea: Causes and environmental implications in its estuary. Journal of Hydrology, 391, 302-313(2010).

    [15] H J Wang, X Wu, N S Bi et al. Impacts of the dam-orientated water-sediment regulation scheme on the lower reaches and delta of the Yellow River (Huanghe): A review. Global and Planetary Change, 157, 93-113(2017).

    [16] H J Wang, Z S Yang, Y Saito et al. Stepwise decreases of the Huanghe (Yellow River) sediment load (1950-2005): Impacts of climate change and human activities. Global and Planetary Change, 57, 331-354(2007).

    [17] S J Wang, Y K Li. Channel variations of the different channel pattern reaches in the Lower Yellow River from 1950 to 1999. Quaternary International, 244, 238-247(2011).

    [18] B S Wu, J Q Xia, X D Fu et al. Effect of altered flow regime on bankfull area of the Lower Yellow River, China. Earth Surface Processes and Landforms, 33, 1585-1601(2010).

    [19] B S Wu, L Y Li. Characteristics of cross-section in the lower channel of the Yellow River. Yellow River, 30, 15-16, 79(2008).

    [20] B S Wu, G Q Wang, J Q Xia et al. Response of bankfull discharge to discharge and sediment load in the Lower Yellow River. Geomorphology, 100, 366-376(2008).

    [21] B S Wu, J Q Xia, Y F Zhang. Response of bankfull discharge to variation of flow discharge and sediment load in lower reaches of Yellow River. Journal of Hydraulic Engineering, 38, 886-892(2007).

    [22] J Q Xia, X J Li, X L Zhang et al. Recent variation in reach-scale bankfull discharge in the Lower Yellow River. Earth Surface Processes and Landforms, 39, 723-734(2014).

    [23] J Q Xia, X L Zhang, Z H Wang et al. Modelling of hyper-concentrated flood and channel evolution in a braided reach using a dynamically coupled one-dimensional approach. Journal of Hydrology, 561, 622-635(2018).

    [24] X H Xia, J W Dong, M H Wang et al. Effect of water-sediment regulation of the Xiaolangdi Reservoir on the concentrations, characteristics, and fluxes of suspended sediment and organic carbon in the Yellow River. The Science of the Total Environment, 571, 487-497(2016).

    [25] J X Xu, O Y Zhang. Complicated fill-scour behaviors of the Huanghe River and the channel forming processes. Acta Geographica Sinica, 55, 274-280(2000).

    [26] T Yang, Q Zhang, Y D Chen et al. A spatial assessment of hydrologic alteration caused by dam construction in the middle and lower Yellow River, China. Hydrological Processes, 22, 3829-3843(2010).

    [27] W Y Yao, H X Zhang, Z J Hou et al. Discussion on the reversibility of the river channel shrinking in the Lower Yellow River. Proceedings of the 2nd International Yellow River Forum on Keeping Healthy Life of the River, 4, 197-204(2015).

    [28] . Yellow River Sediment Bulletin(20002015).

    [29] M Zhang, H Q Huang, P A Carling et al. Sedimentation of overbank floods in the confined complex channel-floodplain system of the Lower Yellow River, China. Hydrological Processes, 31, 3472-3488(2017).

    [30] O Y Zhang, J X Xu, H W Zhang. The response of the channel form adjustment at the wandering-braided reaches of the Lower Yellow River to flood events. Journal of Sediment Research, 1-7(2002).

    [31] Y F Zhang, G Q Shen. Regulation indices of hyperconcentrated floods in the Lower Yellow River. Journal of Sediment Research, 42, 25-30(2017).

    [32] S Zheng. Study on the simulation of non-equilibrium fluvial processes. Beijing: Tsinghua University(2013).

    [33] S Zheng, S S Han, G M Tan et al. Morphological adjustment of the Qingshuigou channel on the Yellow River Delta and factors controlling its avulsion. Catena, 166, 44-55(2018).

    Yanjun WANG, Baosheng WU, Deyu ZHONG. Adjustment in the main-channel geometry of the lower Yellow River before and after the operation of the Xiaolangdi Reservoir from 1986 to 2015[J]. Journal of Geographical Sciences, 2020, 30(3): 468
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