Abstract
The history of dune landform changes and dust activity at mid-latitudes is a good archive for exploring environmental changes and related landscape response. In this study, the dynamic changes, material sources, dust activity history and the influencing factors of typical sand dunes in the Hexi Corridor were comprehensively analyzed from the aspects of aeolian geomorphology, grain-size sedimentology, geochemistry and climatology. The results show that in the past half century, the typical crescent-shaped dunes and chains of crescent-shaped dunes in the study area have moved or swayed greatly, with an average speed ranging from 0.8 m/a (Dunhuang) to 6.2 m/a (Minqin). The dynamic changes of sand dunes are mainly affected by annual precipitation, annual average wind speed and annual gale days, which indicates that climate is the primary influencing factor of dune landform changes. The three-stage grain-size curve model of dune sands is obviously different from that of gobi sediments (two-stage), revealing the “immaturity” of the latter in sedimentology, while the former has experienced efficiently aeolian differentiation and non-local origin. The comprehensive evidences of paleogeography, sedimentology and geochemistry reveal that the source materials of sand dunes are mainly alluvial/proluvial and palaeo-fluvial sediments, including clastic sediments in the denudation/erosion zones of the north and south piedmonts. Indicators such as the proportion of surface fine particles, the coverage of surface salt crusts, and the content of erodible sandy materials indicate that the western gobi areas are not the main source areas of wind-blown dust in the central and eastern parts of the Hexi Corridor. The spatial distribution of the movement direction of sand dunes is similar to that of the regional dominant wind direction, which indicates that the difference in the dynamic evolution of dune landforms between the east and west of the Hexi Corridor should be controlled by the regional-scale wind system, that is, controlled by the dynamic mechanism rather than the difference in material sources. The warming and humidification of the Hexi climate is a synchronous response to the global warming and the strengthening of the Asian Summer Monsoon. It is also the main reason for the reduction of dust storms in the study area, which means that a potential inverse desertification process exists in the Hexi Corridor during the same period and it is also controlled by climate change. However, the process of desertification in the oasis areas during the period is caused by groundwater fluctuation affected by human activities.
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An F, Zhang D, Zhao J et al., 2019. Physical and chemical properties of soils in different types in the Gobi areas of the Hexi Corridor. Soil and Water Conservation in China, (6): 42–47. (in Chinese)
Bagnold R A, 1959. Physics of Sand and Dunes in Desert. Beijing: Science Press.
Chang Z, 2019. Problems and solutions to desertification combating in the Hexi, Gansu for 60 years. Journal of Arid Land Resources and Environment, 33(9): 152–159. (in Chinese)
Chang Z, Han F, Zhong S, 2005. Natural and artificial factors and their transfer on sandy desertification of lower reaches of Shiyang River Basin. Arid Land Geography, 28(2): 150–155. (in Chinese)
Chang Z, Han F, Zhong S, 2011. Response of desert climate change to global warming in Minqin, China. Journal of Desert Research, 31(2): 505–510. (in Chinese)
Chang Z, Li Y, Zhang J et al., 2017. Stability mechanisms of barchan sand dunes: A case study in the Hexi Desert in Gansu. Acta Ecologica Sinica, 37(13): 4375–4383. (in Chinese)
Chang Z, Liu H, 2003. Desertification control in Hexi inland river basins of Gansu Province (II). Protection Forest Science and Technology, (2): 28–32. (in Chinese)
Chang Z, Ma Z, Wang D, 2016a. Instability of climate change in the Minqin desert area. Arid Zone Research, 33(3): 601–608. (in Chinese)
Chang Z, Wang Q, Zhang J, 2015. Environmental conditions of barchans dune and barchans chain: A case study from the Hexi Desert area of Gansu. Animal Husbanbandry and Feed Science, 7(6): 383–388.
Chang Z, Zhu S, Shi X et al., 2016b. Comparisons between movement speed of main types of dunes: A case study of desert areas in Hexi region of Gansu Province. Journal of Landscape Research, 8(6): 36–40. (in Chinese)
Chen F, Liu Y, 2011. Secular annual movement of sand dunes in Badain Jaran Desert based on geographic analyses of remotely sensed imagery. Remote Sensing Technology and Application, 26(4): 501–507. (in Chinese)
Chen F, Zhang J, Liu J et al., 2020. Climate change, vegetation history, and landscape responses on the Tibetan Plateau during the Holocene: A comprehensive review. Quaternary Science Reviews, 243: 106444. doi: https://doi.org/10.1016/j.quascirev.2020.106444.
Chunyu X Z, Huang F, Xia Z Q et al., 2019. Assessing the ecological effects of water transport to a lake in arid regions: A case study of Qingtu lake in Shiyang river basin, Northwest China. International Journal of Environmental Research and Public Health, 16(1): 145. doi: https://doi.org/10.3390/ijerph16010145.
Ding Y, 2002a. Global climate change. World Environment, (6): 9–12.
Ding Y, 2002b. Prediction of Environmental Changes in Western China. In: Qin D (ed.). Assessment of Environmental Evolution in Western China. Beijing: Science Press. (in Chinese)
Dong Y, Huang D, 2013. Preliminary observation of movement of coastal dunes in Feicui Island in Changli, Hebei Province. Journal of Desert Research, 33(2): 486–492. (in Chinese)
Dong Z, Chen G, Yan C, 1998. Movement laws of dunes along oil transportation highway in the Tarim Desert. Journal of Desert Research, 18(4): 328–333. (in Chinese)
Dong Z, Qu J, Liu X, 2002a. Experimental investigation of the drag coefficients of gobi surfaces. Science in China Series D: Earth Sciences, 45(7): 609–615.
Dong Z, Liu X, Wang X, 2002b. Aerodynamic roughness of gravel beds. Geomorphology, 43(1/2): 17–31.
Dong Z, Su Z, Qian G, 2011. Aeolian Landforms in the Kumtag Desert. Beijing: Science Press. (in Chinese)
Feng H, Zhang M, 2015. Global land moisture trends: Drier in dry and wetter in wet over land. Scientific Reports, 5: 18018. doi: https://doi.org/10.1038/srep18018.
Ferrat M, Weiss D J, Strekopytov S, 2011. Improved provenance tracing of Asian dust sources using rare earth elements and selected trace elements for palaeomonsoon studies on the eastern Tibetan Plateau. Geochimic & Cosmochimic Acta, 75: 6374–6399.
Gillette DA, Stockton PH, 1989. The effect of nonerodible particles on wind erosion of erodible surfaces. Journal of Geophysical Research, 94(12): 885–893.
Goudie A, 2002. Great Warm Deserts of the World: Landscapes and Evolution. New York: Oxford University Press.
Greve P, Orlowsky B, Mueller B et al., 2014. Global assessment of trends in wetting and drying over land. Nature Geoscience, 7. doi: https://doi.org/10.1038/NGEO2247.
Guo Z, Peng S, Hao Q, 2004. Late Miocene-Pliocene development of Asian aridification as recorded in the red-earth formation in northern China. Global and Planetary Change, 41: 135–145.
Guo Z, Ruddiman W, Hao Q et al., 2002. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 416: 159–163.
He J, Guo J, Xing E, 2012. Structure of wind-sand flow and law of dune movement along bank of Yellow River in Ulan Buh desert. Transactions of the Chinese Society of Agricultural Engineering, 28(17): 71–77. (in Chinese)
Honda M, Shimizu H, 1998. Geochemical, mineralogical and sedimentological studies on the Taklimakan Desert sands. Sedimentology, 45: 1125–1143.
Houghton J T, Ding Y, Griggs D J, 2001. Climate Change 2001: The Scientific Basis. Cambridge: Cambridge University Press, 15–108.
Hu F, Zhang K, An Z, 2020. Composition of wind dynamic environment among desert, oasis and gobi. Journal of Desert Research, 40(4): 113–119. (in Chinese)
Hu X, Wang M, Liu Y, 2016. Analysis of movement of dunes in the Tengger Desert based on high-resolution remote sensing images. China Science and Technology Review, (2): 337. (in Chinese)
Jensen L, Eicker A, Dobslaw H, 2019. Long-term wetting and drying trends in land water storage derived from GRACE and CMIP5 models. Journal of Geophysical Research Atmosphere, 124: 9808–9823.
Jiang Q, Yang X, 2019. Sedimentological and geochemical composition of aeolian sediments in the Taklamakan Desert: Implications for provenance and sediment supply mechanisms. Journal of Geophysical Research Earth Surface, 124: 1217–1237.
Lancaster N, Wolfe S, Thomas D et al., 2016. The INQUA Dunes Atlas chronologic database. Quaternary International, 410: 3–10.
Lancaster N, Yang X, Thomas D, 2013. Spatial and temporal complexity in Quaternary desert datasets: Implications for interpreting past dryland dynamics and understanding potential future changes. Quaternary Science Reviews, 78: 301–302.
Lang L, Wang X, Zhu B et al., 2017. Nebkha formation and variations in sediment availability and wind-energy regime of the western Hexi Corridor over the past several dacades. Journal of Desert Research, 37(4): 611–620. (in Chinese)
Li B, 2007. The oasis in the lower reaches of the Shiyang River has become the “the second Loulan” before the mid-Tang Dynasty. Research and Development, (2): 153–157. (in Chinese)
Li E, 2011. Comparative study on characteristics of aeolian sediments between the Badanjilin and Tengeli deserts [D]. Xi’an: Shaanxi Normal University. (in Chinese)
Li Y, Zhang S, 2007. Review of the research on the relationship between sand-dust storm and arid in China. Advances in Earth Science, 22(11): 1169–1176. (in Chinese)
Liu T, 1985. Loess and the Environment. Beijing: China Ocean Press. (in Chinese)
Liu X, Dong Z, 2003. Aerodynamic roughness of gravel bed. Journal of Desert Research, 23(1): 40–47. (in Chinese)
Lv P, Narteau C, Dong Z, 2021. Direct validation of dune instability theory. PNAS, 118(17): e2024105118. doi: https://doi.org/10.1073/pnas.2024105118.
Lyles L, Tatarko J, 1988. Soil wind erodibility index in seven northern central states. Transactions of the ASAE, 31(5): 1396–1399.
Mao D, Lei J, Zhou J, 2016. Movement rules of different shifting dunes and semi-shifting dunes in Cele, Xinjiang Uygur Autonomous Region. Research of Soil and Water Conservation, 23(3): 278–282. (in Chinese)
MDCES (Minqin Desert Control Experiment Station), 1975. Deserts and Control in Gansu. Lanzhou: Gansu People’s Publishing House, 33–38. (in Chinese)
Micklin P, 2007. The Aral Sea disaster. Annual Review of Earth and Planetary Sciences, 35(1): 47–72.
Mischke S, Liu C L, Zhang J F, 2017. The world’s earliest Aral-Sea type disaster: The decline of the Loulan Kingdom in the Tarim Basin. Scientific Reports, 7: 43102. doi: https://doi.org/10.1038/srep43102.
Muhs D, 2004. Mineralogical maturity in dunefields of North America, Africa and Australia. Geomorphology, 59: 247–269.
Muhs D, Bush C, Cowherd S, 1995. Geomorphic and geochemical evidence for the source of sand in the Algodones dunes, Colorado Desert, southeastern California. In: Tchakerian V (ed.). Desert Aeolian Processes. London: Chapman & Hall, 37–74.
Muhs D, Stafford T, Cowherd S, 1996. Origin of the Late Quaternary dune fields of northeastern Colorado. Geomorphology, 17: 129–149.
Nottebaum V, Lehmkuhl F, Stauch G, 2015. Late Quaternary aeolian sand deposition sustained by fluvial reworking and sediment supply in the Hexi Corridor: An example from northern Chinese drylands. Geomorphology, 250: 113–127.
Pan K, Zhang Z, Dong Z, 2019. Physicochemical characteristics of surface sediments of crescent shaped sand dunes in the Hexi Corridor, Gansu, China. Journal of Desert Research, 39(1): 44–51. (in Chinese)
Pease P, Tchakerian V, 2003. Geochemistry of sediments from Quaternary sand ramps in the southeastern Mojave Desert, California. Quaternary International, 104: 19–29.
Pease P, Tchakerian V, Tindale N, 1998. Aerosols over the Arabian Sea: Geochemistry and source areas for aeolian desert dust. Journal of Arid Environments, 39: 477–496.
Pettijohn F J, Potter P E, Siever R, 1972. Sand and Sandstone. New York: Springer-Verlag.
Pu Z, 2005. For the lost oasis: A review of studies on desertification in the Hexi Corridor during the historical period. Collections of Essays on Chinese Historical Geography, 20(1): 157–158. (in Chinese)
Pye K, 1987. Aeolian Dust and Dust Storms. Gainesville: Academic Press.
Qu J, Huang N, Ta W, 2005. Structural characteristics of Gobi sanddrift and its significance. Advances in Earth Science, 20(1): 19–23. (in Chinese)
Raupach M R, Gillette D A, Leys J F, 1993. The effect of roughness elements on wind erosion threshold. Journal of Geophysical Research, 98(D2): 3023–3029.
Ren X, 2010. Element analysis of surface sediments from active dunes in the Minqin Oasis and its adjacent deserts [D]. Lanzhou: Lanzhou University. (in Chinese)
Ren X, Liu T, Wang Z, 2010. Characters of geomorphologic parameter about barchans dunes. Research of Soil and Water Conservation, 17(1): 163–166. (in Chinese)
Ren X, Wang Z, 2010. The provenance of eolian sediments in Minqin Oasis, Gansu Province. Journal of Ningxia University: Natural Science Edition, 31(1): 88–92. (in Chinese)
Ren X, Yang X, Wang Z, 2014. Geochemical evidence of the sources of aeolian sands and their transport pathways in the Minqin Oasis, northwestern China. Quaternary International, 334/335: 165–178.
Rostagno C M, Degorgue G, 2011. Desert pavements as indicators of soil erosion on aridic soils in north-east Patagonia (Argentina). Geomorphology, 134: 224–231.
Sahu BK, 1964. Depositional mechanisms from the size analysis of clastic sediments. Journal of Sedimentary Research, 34(1): 73–83.
Sha W, Shao X, Huang M, 2002. Climate warming and its impact on natural regional boundaries in China since 1980s. Science China in Series D, 32(4): 317–326.
Shi X, Li G, Liu S, 2018. Dynamic changes of barchans dunes and its relationship with meteorological factors along oasis fringe in Hexi Corridor. Journal of Gansu Agricultural University, 2: 86–93. (in Chinese)
Sun J, 2002. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau. Earth and Planetary Science Letters, 203: 845–859.
Taylor S R, McLennan S M, 1985. The Continental Crust: Its Composition and Evolution. London: Blackwell Scientific Publications.
Uno I, Wang Z, Chiba M, 2006. Dustmodel intercomparison (DMIP) study over Asia: Overview. Journal of Geophysical Research, 111: D12213. doi: https://doi.org/10.1029/2006JD006575.
Visher G, 1969. Grain size distributions and depositional processes. Journal of Sedimentary Research, 39(3): 1074–1106.
Wang J, Li W, Song D, 2002. The analysis of land desertification changing of Minqin County in recent 30 years. Journal of Remote Sensing, 8: 282–288.
Wang J, Liu L, Shen L, 2013. Research of movement laws of barchan dunes in the Mu Us Sandy Land based on Google Earth software. Remote Sensing Technology and Application, 28(6): 1094–1100.
Wang L, 2011. Surface deposits in the Hexi Corridor and its adjacent areas and implications for provenance of Asian dust [D]. Lanzhou: Lanzhou University. (in Chinese)
Wang L, Wang Q, 2013. Elemental compositions of surface deposits in the Hexi Corridor and its adjacent areas, northwestern China. Northwestern Geology, 46(2): 69–80. (in Chinese)
Wang T, 2003. Desert and Desertification in China. Shijiazhuang: Hebei Science and Technology Press. (in Chinese)
Wang X, Chen F, Dong Z, 2006. The relative role of climatic and human factors in desertification in semi-arid China. Global Environmental Change (Part A), 16: 48–57.
Wang X, Chen F, Hasi E, 2008a. Desertification in China: An assessment. Earth-Science Reviews, 88: 188–206.
Wang X, Hua T, Zhu B, 2018. Geochemical characteristics of the fine-grained component of surficial deposits from dust source areas in northwestern China. Aeolian Research, 34: 18–26.
Wang X, Lang L, Hua T, 2013. Gravel cover of Gobi desert and its significance for wind erosion: An experimental study. Journal of Desert Research, 33(2): 313–319. (in Chinese)
Wang X, Li J, Dong G, 2008b. Responses of desertification to variations in wind activity over the past five decades in arid and semiarid China. Chinese Science Bulletin, 53: 426–433.
Williams M, 2014. Climate Change in Deserts: Past, Present and Future. New York: Cambridge University Press.
Wolfe S, Muhs D, David P, 2000. Chronology and geochemistry of Late Holocene eolian deposits in the Brandon Sand Hill, Manitoba, Canada. Quaternary International, 67: 61–74.
Wolfe S A, Nickling W G, 1996. Shear stress partition in sparsely vegetated desert canopies. Earth Surface Processes and Landforms, 21: 607–619.
Xie Y, Chen F, Wang N, 2004. Spatial change of Minqin Oasis in Gansu over the last 2000 years. Acta Geographica Sinica, 59(5): 662–670. (in Chinese)
Yang X, 2006. Desert research in northwestern China: A brief review. Geomorphologie: Relief, Processus, Environment, 4: 275–284.
Yang X, Li H, Conacher A, 2012. Large-scale controls on the development of sand seas in northern China. Quaternary International, 250: 74–83.
Yang X, Liang P, Zhang D, et al., 2019. Holocene aeolian stratigraphic sequences in the eastern portion of the desert belt (sand seas and sandy lands) in northern China and their palaeoenvironmental implications. Science China Earth Sciences, 62: 1302–1315.
Yang X, Preusser F, Radtke U, 2006. Late Quaternary environmental changes in the Taklamakan Desert, western China, inferred from OSL-dated lacustrine and aeolian deposits. Quaternary Science Reviews, 25: 923–932.
Yang X, Rost KT, Lehmkuhl F, et al., 2004. The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum. Quaternary International, 118/119: 69–85.
Yang X, Scuderi L, Paillou P, 2011. Quaternary environmental changes in the drylands of China: A critical review. Quaternary Science Reviews, 30: 3219–3233.
Yang X, Zhu B, White P D, 2007. Provenance of aeolian sediment in the Taklamakan Desert of western China, inferred from REE and major-elemental data. Quaternary International, 175: 71–85.
Yin D, Qu J, Zu R, 2014. Impact of disturbing on amount of wind erosion of sandy Gobi. Journal of Desert Research, 34(1): 1–8. (in Chinese)
Zhang K, Qu J, Zu R, 2004. Wind tunnel simulation about the effects of the different underlying surfaces on the features of drifting sand current. Arid Land Geography, 37(3): 352–355. (in Chinese)
Zhang L, Ren G, 2003. Change in dust storm frequency and the climatic controls in northern China. Acta Meteorologica Sinica, 61(6): 744–750. (in Chinese)
Zhang Z, Dong Z, 2014. Dune field patterns and wind environments in the middle reaches of the Heihe Basin. Journal of Desert Research, 34(2): 332–341. (in Chinese)
Zhang Z, Dong Z, 2015. Grain size characteristics in the Hexi Corridor desert. Aeolian Research, 18: 55–67.
Zhang Z, Dong Z, Li J, 2016. Implications of surface properties for dust emission from gravel deserts (gobis) in the Hexi Corridor. Geoderma, 268: 69–77.
Zhang Z, Dong Z, Zhang C, 2017. The geochemical characteristics of dust material and dust sources identification in northwestern China. Journal of Geochemical Exploration, 175: 148–155.
Zhang Z, Pan K, Zhang C, 2020. Geochemical characteristics and the provenance of aeolian material in the Hexi Corridor Desert, China. Catena, 104483. doi: https://doi.org/10.1016/j.catena.2020.104483.
Zhu B, 2007. Geochemistry, hydrochemistry and sedimentology of the Taklamakan Desert in Tarim Basin, NW China [D]. Beijing: Institute of Geology and Geophysics, Chinese Academy of Sciences. (in Chinese)
Zhu B, 2022. Mechanisms of land degradation and their environmental implications in a middle-latitude desert area of China. Land Degradation and Development, 33: 145–178.
Zhu B, Yang X, 2009. Chemical weathering of detrital sediments in the Taklamakan Desert, northwestern China chemical weathering of detrital sediments in the Taklamakan Desert, northwestern China. Geographical Research, 47(1): 57–70.
Zhu B, Yu J, 2014. Aeolian sorting processes in the Ejina desert basin (China) and their response to depositional environment. Aeolian Research, 12: 111–120.
Zhu B, Yu J, Rioual P, 2014. Particle size variation of aeolian dune deposits in the lower reaches of the Heihe River basin, China. Sedimentary Geology, 301: 54–69.
Zhu B, Zhang J, Sun C, 2022. Potential links of gobi, dust, and desertification: A comprehensive understanding from aeolian landform evolution in a middle-latitude desert. Sedimentary Geology, 428: 106049, doi: https://doi.org/10.1016/j.sedgeo.2021.106049.
Zhu Z, 1999. Deserts, Desertification, Land Degradation and Strategies for Rehabilitation in China. Beijing: Environmental Press. (in Chinese)
Zhu Z, Chen G, 1994. Sandy Desertification in China. Beijing: Science Press. (in Chinese)
Zhu Z, Chen Z, Wu Z, 1981. Study on the Geomorphology of Wind-drift Sands in the Taklamakan Desert. Beijing: Science Press. (in Chinese)
Zhu Z, Wang T, 1992. Theory and practice on sandy desertification in China. Quaternary Sciences, 2: 97–106. (in Chinese)
Zhu Z, Wu Z, Liu S et al., 1980. An Outline of Chinese Deserts. Beijing: Science Press. (in Chinese)
Zimbelman J, Williams S, 2002. Geochemical indicators of separate sources for eolian sands in the eastern Mojave Desert, California, and western Arizona. Geological Society of America Bulletin, 114: 490–496.
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Foundation: National Natural Science Foundation of China, No.41930640, No.41771014; The Second Tibetan Plateau Scientific Expedition and Research, No.2019QZKK1003
Author: Zhu Bingqi, PhD and Professor, specialized in Quaternary geomorphology and Quaternary environmental changes.
This paper is initially published in Acta Geographica Sinica (Chinese edition), 2021, 76(11): 2710–2729.
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Zhu, B. The recent evolution of dune landforms and its environmental indications in the mid-latitude desert area (Hexi Corridor). J. Geogr. Sci. 32, 617–644 (2022). https://doi.org/10.1007/s11442-022-1964-y
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DOI: https://doi.org/10.1007/s11442-022-1964-y