Responses of Riverbed Particles to Geomorphologic Processes in Aeolian-Fluvial Action Area: A Case Study of the Heilaigou Basin in Inner Mongolia of China

  • 1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China;
    3. Hebei University of Water Resources and Electric Engineering, Cangzhou, Hebei 061000, China

Received date: 2017-09-25

  Revised date: 2017-12-19

  Online published: 2018-03-30

Supported by

National Natural Science Foundation of China (41371036;41671004)


The Heilaigou basin, located in the Inner Mongolia of China, is predominantly influenced by the aeolian-fluvial actions, with complicated sediment transport conditions on the mainstream riverbed. In order to identify the relationship between sedimentary particles and geomorphic processes, mechanisms for the formation of characteristics of grain size composition were investigated by analyzing grain size parameters and external dynamic geomorphologic features. Firstly, the grain size parameters of the riverbed, stream power, maximum grain size of the wind-blown particles and HI values of the mainstream channel were calculated and analyzed, and they were used to establish multiple regression functions of grain size parameters in order to determine the effects of wind and river actions on particles. The results show that sediments in different reaches are formed in different environments: the upper stream is controlled by fluvial and aeolian processes; the sorting properties of riverbed sediments in the middle stream are worse than those in the upper stream since they are affected mainly by fluvial processes as indicated by the larger stream power there; and the particles on the downstream riverbed are likely contributed by the Kubuqi Desert. The size of particles on the riverbed depends on the hydrodynamic conditions, but is not significantly associated with the evolution of landform. Sorting is significantly related to both the hydrodynamic conditions and wind actions. Riverbed deposits brought in by winds likely become finer from the lower to the upper reaches, which are not coarser than 0.88f. Generally speaking, the stream power has a major effect on sedimentation characteristics of the riverbed, followed by wind power.

Cite this article

GU Zhenkui, SHI Changxing, YANG Hui . Responses of Riverbed Particles to Geomorphologic Processes in Aeolian-Fluvial Action Area: A Case Study of the Heilaigou Basin in Inner Mongolia of China[J]. Journal of Resources and Ecology, 2018 , 9(2) : 191 -202 . DOI: 10.5814/j.issn.1674-764x.2018.02.009


[1] Al-Awadhi J M, Al-Helal A, Al-Enezi A.2005. Sand drift potential in the desert of Kuwait. Journal of Arid Environments, 63(2): 425-438.
[2] An Z S, Porter S C, Kutzbach J E, et al.1991. Late quaternary dust flow on the Chinese Loess Plateau. Catena, 18(2): 125-132.
[3] Avtar R, Yunus A P, Kraines S, et al.2015. Evaluation of DEM generation based on interometric SAR using TanDEM-X data in Tokyo. Physics and Chemistry of the Earth: Parts A/B/C, 83-84: 166-177.
[4] Bagnold R A.1941. The physics of blown sand and desert dunes. Nature, 18(4): 167-187.
[5] Blott S J, Pye K.2001. Gradistat: A grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth Surface Processes and Landforms, 26(11): 1237-1248.
[6] Brown K L, Pasternack B P.2004. The geomorphic dynamics and environmental history of an upper deltaic floodplain tract in the Sacramento-San Joaquin Delta, California, USA. Earth Surface Processes and Landforms, 29(10): 1235-1258.
[7] Chen Q, Liu D Y, Chen Y J, et al.2013. Comparative analysis of grade-standard deviation method and factors analysis method for environment sensitive factor analysis. Earth and Environment, 41(3): 319-324. (in Chinese)
[8] Diyabalanage S, Samarakoon K K, Adikari S B, et al.2017. Impact of soil and water conservation measures on soil erosion rate and sediment yields in a tropical watershed in the Central Highlands of Sri Lanka. Applied Geography, 79: 103-114.
[9] Dong Y S, Chang H C, Chen W T, et al.2015. Accuracy assessment of GDEM, SRTM, and DLR-SRTM in Northeastern China. Geocarto International, 30(7): 779-792.
[10] Du Y N, Feng G C, Li Z W, et al.2015. Generation of high precision DEM from TerraSAR-X/TanDEM-X. Chinese Journal of Geophysics, 58(9): 3089-3102. (in Chinese)
[11] Fan D J, Qi H Y, Sun X X, et al.2011. Annual lamination and its sedimentary implications in the Yangtze River delta inferred from high-resolution biogenic silica and sensitive grain-size records. Continental Shelf Research, 31(2): 129-137.
[12] Folk P L, Ward W D.1957. Brazos River bar: A study in the significance of grain size parameters. Journal of Sedimentary Petrology, 27(1): 3-26.
[13] Font M, Amorese D, Lagarde J L.2010. DEM and GIS analysis of the stream gradient index to evaluate effects of tectonics: The Normandy intraplate area (NW France). Geomorphology, 119: 172-180.
[14] Friedman G M.1967. Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands. Journal of Sediment Petrology, 37(2): 327-354.
[15] Fryberger S G, Dean G.1979. Dune forms and wind regime. In: Meckee E D (ed.). A Study of Global Sand Seas. Washington: U.S. Geological Survey Professional Paper, 137-169.
[16] Guan H C, Zhu C, Zhu T X, et al.2016. Grain size, magnetic susceptibility and geochemical characteristics of the loess in the Chaohu lake basin: Implications for the origin, palaeoclimatic change and provenance. Journal of Asian Earth Sciences, 117: 170-183.
[17] Guo J, Wang W, Shi J S.2015. A quantitative analysis of the stage of geomorphologic evolution in Luohe drainage basin, north of Shaanxi Province. Arid Land Geography, 38(6): 1161-1168. (in Chinese)
[18] Halls J R.1967. Significance of statistical parameters for distinguishing sedimentary environments in New South Wales, Australia. Journal of Sedimentary Petrology, 37(4): 1059-1069.
[19] Jia W, Zhang C, Li S, et al.2016. Grain size distribution at four developmental stages of crescent dunes in the hinterland of the Taklimakan Desert, China. Journal of Arid Land, 8(5): 722-733.
[20] Kanhaiya S, Singh B P, Tripathi M, et al.2017. Lithofacies and particle-size characteristics of late Quaternary floodplain deposits along the middle reaches of the Ganga river, central Gange plain, India. Geomorphology, 284: 220-228.
[21] Li B, Gao J R, Hu F B.2011. Granularity parameter of debris flow deposit in Wanghugou gully, Beijing City. Science of Soil and Water Conservation, 9(4): 7-10. (in Chinese)
[22] Li C Z and Wang Y Y.1999. Preliminary exploration on grain characteristic and discrimination of debris flow deposit, moraine and river and lake deposit. Journal of Mountain Science, 17(1): 50-54. (in Chinese)
[23] Lin X Z, Guo Y, Hou S Z.2014. Estimation of sediment discharge of ten tributaries of Yellow River in Inner-Mongolia. Journal of Sediment Research, (2): 15-20.
[24] Liu M P, Hasi E, Sun Y.2016. Variation in grain size and morphology of an inland parabolic dune during the incipient phase of stabilization in the Hobq Desert, China. Sedimentary Geology, 337: 100-112.
[25] Liu G N, Cui Z J, Wang X H.1999. Sedimentary macro-structures of debris flows and their formation mechanism. Geological Review, 41(2): 159-164. (in Chinese)
[26] Liu L Y, Skidomore E, Hasi E, et al.2005. Dune sand transport as influenced by wind directions, speed and frequencies in the Ordos Plateau, China. Geomorphology, 67(3-4): 283-297.
[27] Ma Y F, Yan P, Li S Q.2013. Dynamic process of aeolian-fluvial interaction erosion in the middle reaches of Baerdong River in Ten-Watershed, Inner Mongolia of China. Journal of Desert Research, 33(4): 990-998. (in Chinese)
[28] McManus J. 1988. Grain size determination and interpretation. In: Tucker M (ed.). Techniques in Sedimentology. Blackwell: Oxford, 63-85.
[29] Okeyode I C, Jibiri N N.2013. Grain size analysis of the sediments from Ogun River, Southwestern Nigeria. Earth Science Research, 2(1): 43-51.
[30] Opreanu G, Oaie G, Păun F.2007. The dynamic significance of the grain size of sediments transported and deposited by the Danube. Geo-Eco- Marina, 13: 111-119.
[31] Pike R J, Wilson S E.1971. Elevation-relief ratio, hypsometric integral, and geomorphic area-altitude analysis. Geological Society of America Bulletin, 82(4): 1079-1084.
[32] Prins M A, Postma G, Weltje G J.2000. Controls on the terrigenous sediment supply to the Arabian Sea during the late Quaternay: The Makran continental slope. Marine Geology, 169(3): 351-371.
[33] Qi L X, Dong F, Chen Q, et al.2001. Study on onset-wind-speed of blown sand. Mechanics in engineering, 23(4): 13-14. (in Chinese).
[34] Remo J W F, Heine R A, Ickes B S.2016. Particle size distribution of main-channel-bed sediments along the upper Mississippi River, USA. Geomorphology, 264:118-131.
[35] Rowan J S, Black S, Franks S W.2012. Sediment fingerprinting as an environmental forensics tool explaining cyanobacteria blooms in lakes. Applied Geography, 32(2): 832-843.
[36] Sharma S, Tiwari K.2009. Bootsrap based artificial neural network (BANN) analysis for hierarchical prediction of monthly runoff in Upper Damodar Valley Catchment. Journal of Hydrology, 374(3-4): 209-222.
[37] Shepard F P.1954. Nomenclature based on sand-silt-clay ratios. Journal of Sedimentary Petrology, 24(3): 151-158.
[38] Shi C X, Wang S J, Xu J X, et al.2016. Mechanisms of Flood-Riverbed-Bank Interaction in Ningxia-Inner Mongolia Reach of the Yellow River. Beijing: Science Press. (in Chinese)
[39] Singh O, Sarangi A, Sharma M C.2008. Hypsometric integral estimation methods and its relevance on erosion status of north-western lesser Himalayan watershed. Water Resources Management, 22(11): 1545-1560.
[40] Song N P, Zhang F G.2007. The changing process and mechanism of the farming-grazing transitional land use pattern in Ordos. Acta Geographica Sinica, 62(12): 1299-1308. (in Chinese)
[41] Strahler A N.1952. Hypsometric (area-altitude) analysis of erosional topography. Geological Society of America Bulletin, 63(11): 1117-1141.
[42] Strahler A N.1957. Quantitative analysis of watershed geomorphology. Transactions of the American Geophysical Union, 38(6): 913-920.
[43] Sujatha K, Singarasubramanian S R.2013. Sediment characterization and depositional processes from the pit samples of Poompuhar, Ambanar river mouth and Tarangambadi, east coast of Tamilnaduu, India. International Journal of Recent Scientific Research, 4(3): 177-184.
[44] Sun Y B, Gao S, Li J.2003. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting. Chinese Science Bulletin, 48(2): 184-187.
[45] Teng J W, Wang F Y, Zhao W Z, et al.2008. Velocity distribution of upper crust, undulation of sedimentary formation and crystalline basement beneath the Ordos basin in North China. Chinese Journal of Geophysics, 51(1): 277-291. (in Chinese)
[46] Teng J W, Wang F Y, Zhao W Z, et al.2010. Velocity structure of layered block and deep dynamic process in the lithosphere beneath the Yinshan Orogenic Belt and Ordos Basin. Chinese Journal of Geophysics, 53(6): 1753-1766. (in Chinese)
[47] Tian M Z and Chen J. 2009. Quaternary Geology and Geomorphology. Beijing: Geological Publishing House. (in Chinese)
[48] Visher G S.1969. Grain size distribution and depositional processes. Journal of Sedimentary Petrology 39(3): 1074-1016.
[49] Walling D E, Owens P N, Waterfall B D, et al.2000. The particle size characteristics of fluvial suspended sediment in the Humber and Tweed catchments, UK. The Science of the Total Environment, 251-252: 205-222.
[50] Watson E B, Pasternack G B, Gray A B, et al.2013. Particle size characterization of historic sediment deposition from a closed estuarine lagoon, Central California. Estuarine, Coastal and Shelf Science, 126: 23-33.
[51] Wu X, Hasi E, Du H S, et al.2012. Grain size distribution of parabolic dunes on the southern fringe of Hobq Desert. Act Sedimentologica Sinica, 30(5): 938-942. (in Chinese)
[52] Xiao S B and Li A C.2005. A study on environmentally sensitive grain size population in inner shelf of the East China Sea. Acta Sedmentologica Sinica, 23(1): 123-128. (in Chinese)
[53] Xiao S, Li A, Liu J P, et al.2006. Coherence between solar activity and the East Asia winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea. Palaeogeography, Palaeoclimatol, Palaeoecol, 237(2-4): 293-304.
[54] Xu S J.2007. Analysis of grain-size populations with environmentally sensitive components in aeolian deposits and their implications. Journal of Arid Land Resources and Environment, 21(3): 95-98. (in Chinese)
[55] Xu S J, Pan B T, Gao H S, et al.2006. Analysis of grain-size populations with environmentally sensitive components of loess during the last interglacial-glacial cycle and their implications. Acta Pedologica Sinica, 43(2): 183-189. (in Chinese)
[56] Yao H, Shi C, Shao W, et al.2016. Changes and influencing factors of the sediment load in the Xiliugou basin of the upper Yellow River, China. Catena, 142: 1-10.
[57] Yasir M A, Brian G J, Errol M.2015. Spatial distribution of sediment particles and trace element pollution within Gunnamatta bay, Port Hacking, NSW, Australia. Regional Studies in Marine Science, 2: 124-131.
[58] Yang H, Shi C X.The fractal characteristics of drainage networks and erosion evolution stages of ten kongduis in the upper reaches of the Yellow River, China. Journal of Resources and Ecology, 2017, 8(2): 165-173.
[59] Yin Z Q, Qin X G, Wu J S, et al.2009. The multimodal grain-size distribution characteristics of loess, desert, lake and river sediments in some areas of Northern China. Act Sedmentologica Sinica, 27(2): 343-351. (in Chinese)
[60] Zhang L, Chen S L, Pan S Q, et al.2014. Sediment variability and transport in the littoral area of the abandoned Yellow River Delta, northern Jiangsu. Journal of Geographical Sciences, 24(4): 717-730.
[61] Zhang X, Li Z B, Li P, et al.2015a. A model to study the grain size components of the sediment deposited in aeolian-fluvial interplay erosion watershed. Sedimentary Geology, 330: 132-140.
[62] Zhang X, Li P, Zhang Y, et al.2015b. The spatial analysis of sediment in Dongliugou watershed. Journal of Soil and Water Conservation, 29(1): 75-79. (in Chinese)
[63] Zheng H B, Chen G C, Xie X, et al.2008. Grain size distribution and dynamic control of late quaternary terrigenous sediments in the South China Sea and their implication for East Asian monsoon evolution. Quaternary Sciences, 28(3): 414-424. (in Chinese)