DU Huishi, WANG Zongming, MAO Dehua. Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China[J]. Chinese Geographical Science, 2018, 28(4): 624-635. doi: 10.1007/s11769-018-0951-9
Citation: DU Huishi, WANG Zongming, MAO Dehua. Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China[J]. Chinese Geographical Science, 2018, 28(4): 624-635. doi: 10.1007/s11769-018-0951-9

Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China

doi: 10.1007/s11769-018-0951-9
Funds:  Under the auspices of Natural National Science Foundation of China (No. 41671002, 41401002)
More Information
  • Corresponding author: WANG Zongming.E-mail:zongmingwang@iga.ac.cn
  • Received Date: 2017-07-20
  • Rev Recd Date: 2017-11-17
  • Publish Date: 2018-08-27
  • The interaction between fluvial and aeolian processes can significantly change surface morphology of the Earth. Taking the Horqin Sandy Land as the research area and using Landsat series satellite remote sensing images, this study utilizes geomorphology and landscape ecology to monitor and analyze the aeolian geomorphology characteristics of the Horqin Sandy Land. Results show that the sand dunes of the Horqin Sandy Land are mainly distributed on alluvial plains along the banks of the mainstream and tributaries of the Western Liao River, and the sand dune types tend to simplify from west to east and from south to north. The aeolian geomorphology coverage tend to be decreasing in the past 40 years, with an average annual change rate of 0.31%. While the area of traveling dunes decreased, the area of fixed and semi-fixed dunes increased. The fractal dimensions of various types of sand dune have all remained relatively constant between 1.07 and 1.10, suggesting that they are experiencing a relatively stable evolutionary process. There is a complex interaction between fluvial and aeolian processes of the Horqin Sandy Land, which plays a central role in surface landscape molding. Sand dunes on both sides of different rivers on the Horqin Sandy Land present certain regularity and different characteristics in terms of morphology, developmental scale, and spatial pattern. There are six fluvial-aeolian interaction modes in this area:supply of sand sources by rivers for sand dune development, complete obstruction of dune migration by rivers, partial obstruction of dune migration by rivers, influence of river valleys on dune developmental types on both sides, influence of river valleys on dune developmental scale on both sides, and river diversion due to obstruction and forcing by sand dunes. This study deepens our understanding of the surface process mechanism of the interaction between fluvial and aeolian processes in semi-arid regions, and provides a basis for researches on regional landscape responses in the context of global environmental change.
  • [1] Anderson J L, Walker I J, 2006.Airflow and sand transport varia-tions within a backshore-parabolic dune plain complex:NE Graham Island, British Columbia, Canada.Geomorphology, 77 (1-2):17-34.doi: 10.1016/j.geomorph.2005.12.008
    [2] Bullard J E, McTainsh G H, 2003.Aeolian-fluvial interactions in dryland environments:examples, concepts and Australia case study.Progress in Physical Geography, 27(4):471-501.doi: 10.1191/0309133303pp386ra
    [3] Bullard J E, Nash D J, 1998.Linear dune pattern variability in the vicinity of dry valleys in the southwest Kalahari.Geomor-phology, 23(1):35-54.doi: 10.1016/S0169-555X(97)00090-1
    [4] Bullard J E, Nash D J, 2000.Valley-marginal sand dunes in the south-west Kalahari:their nature, classification and possible origins.Journal of Arid Environments, 45(4):369-383.doi: 10.1006/jare.2000.0646
    [5] Burchsted D, Daniels M, Wohl E E, 2014.Introduction to the special issue on discontinuity of fluvial systems.Geomor-phology, 205(SI):1-4.doi: 10.1016/j.geomorph.2013.04.004
    [6] Cai Yunlong, Song Changqing, Leng Shuying, 2009.Future de-velopment trends and priority areas of physical geography in China.Scientia Geographica Sinica, 29(5):619-626. (in Chi-nese)
    [7] Du Huishi, Hasi E, Yang Yi et al., 2012.Landscape pattern change and driving force of blowout distribution in the Hulun Buir Sandy Grassland.Sciences in Cold and Arid Regions, 4(5):431-438. (in Chinese)
    [8] Du Huishi, Jiang Hailing, Zhang Lifu et al., 2016.Evaluation of spectral scale effects in estimation of vegetation leaf area index using spectral indices methods.Chinese Geographical Science, 26(6):731-744.doi: 10.1007/s11769-016-0833-y
    [9] Duan Hanchen, Wang Tao, Xue Xian et al., 2013.Spatial-temporal evolution of aeolian desertification in the Horqin Sandy Land based on RS and GIS.Journal of Desert Research, 33(2):470-477. (in Chinese)
    [10] Duran O, Silva M V N, Bezerra L J C et al., 2008.Measurements and numerical simulations of the degree of activity and vege-tation cover on parabolic dunes in north-eastern Brazil.Geo-morphology, 102(3-4):460-471.doi: 10.1016/j.geomorph.2008.05.011
    [11] EBGAC (The Editorial Board of Geomorphological Atlas of the People's Republic of China), 2009.Geomorphological atlas of the People's Republic of China (1:1000000).Beijing:Science Press, 94-95. (in Chinese)
    [12] El-Baz F, Maingue M, Robinson C, 2000.Fluvio-aeolian dynamics in the north-eastern Sahara:the relationship between fluvi-al/aeolian systems and ground-water concentration.Journal of Arid Environments, 44(2):173-183.doi: 10.1006/jare.1999.0581
    [13] Ewing R C, Kocurek G, 2010.Aeolian dune-field pattern boundary conditions.Geomorphology, 114(3):175-187.doi: 10.1016/j.geomorph.2009.06.015
    [14] Ewing R C, Kocurek G, Lake L W, 2006.Pattern analysis of dune-field parameters.Earth Surface Processes and Land-forms, 31(9):1176-1191.doi: 10.1002/esp.1312
    [15] Field J P, Breshears D D, Whicker J J, 2009.Toward a more ho-listic perspective of soil erosion:why aeolian research needs to explicitly consider fluvial processes and interactions.Aeolian Research, 1(1-2):9 17.doi: 10.1016/j.aeolia.2009.04.002
    [16] Han G, Zhang G F, Dong Y X, 2007.A model for the active origin and development of source-bordering dunefields on a semiarid fluvial plain:a case study from the Xiliaohe Plain, Northeast China.Geomorphology, 86(3-4):512-524.doi: 10.1016/j.geomorph.2006.10.010
    [17] Harrison Y, 1998.Late Pleistocene Aeolian and fluvial interactions in the development of the Nizzana dune field, Negev Desert, Israel.Sedimentology, 45(3):507-518.doi: 10.1046/j.1365-3091.1998.00151.x
    [18] Havholm K G, Running IV G L, 2005.Stratigraphy, sedimentol-ogy, and environmental significance of late mid-Holocene dunes, Lauder Sand Hills, glacial lake Hind Basin, southwest-ern Manitoba.Canadian Journal of Earth Sciences, 42(5):847-863.doi: 10.1139/e05-019
    [19] Hugenholtz C H, Wolfe S A, Walker I J et al., 2009.Spatial and temporal patterns of aeolian sediment transport on an inland parabolic dune, Bigstick Sand Hills, Saskatchewan, Canada.Geomorphology, 105(1-2):158-170.doi: 10.1016/j.geomorph.2007.12.017
    [20] Jiang Chanwen, Dong Zhibao, Wen Qing, 2013.Extraction of dune crest lines and calculation of dune-field pattern parameters on remote sensing image based on Matlab platform.Journal of Desert Research, 33(6):1636-1642. (in Chinese)
    [21] Joanna E B, David J N, 1998.Linear dune pattern variability in the vicinity of dry valleys in the southwest Kalahari.Geomor-phology, 23 (1):35-54.doi: 10.1016/S0169-555X(97)00090-1
    [22] Lancaster N, 1988.Development of linear dunes in the south-western Kalahari, southern Africa.Journal of Arid Environ-ments, 14(3):233-244.doi: 0000-0003-1585-5282
    [23] Landsberg S Y, 1956.The orientation of dunes in Britain and Denmark in relation to wind.The Geographical Journal, 122(2):176-189.doi: 10.2307/1790847
    [24] Langford R P, 1989.Fluvial-aeolian interactions:Part I, modern systems.Sedimentology, 36(6):1023-1035.doi: 10.1111/j.1365-3091.1989.tb01540.x
    [25] Li Sen,Wang Yue, Hasi et al., 1997.Classification and develop-ment of aeolian sand landform in the Yurlung Zangbo Valley.Journal of Desert Research, 17(4):342-250. (in Chinese)
    [26] Liu B L, Coulthard T J, 2015.Mapping the interactions between rivers and sand dunes:Implications for fluvial and Aeolian geomorphology.Geomorphology, 231:246-257.doi: 10.1016/j.geomorph.2014.12.011
    [27] Liu Hujun, Wang Jihe, Liao Kongtai et al., 2009.Type and distri-bution of geomorphology of aeolian sediment at region of Su-osuo Vale of Kumtag Desert.Arid land geography, 32(1):87-94. (in Chinese)
    [28] Liu Yanyan, Gong Yanming, Wang Xin et al., 2013.Volume fractal dimension of soil particles and relationships with soil physical-chemical properties and plant species diversity in an alpine grassland under different disturbance degrees.Journal of Arid Land, 5(4):480-487. (in Chinese)
    [29] Ma Yufeng, 2011.The interaction of aeolian and fluvial erosion processes in upper Yellow River.Beijing:Beijing Normal University, 40-46. (in Chinese)
    [30] Marín L, Forman S L, Valdez A et al., 2005.Twentieth century dune migration at the Great Sand Dunes National Park and Preserve, Colorado, relation to drought variability.Geomor-phology, 70(1-2):163-183.doi: 10.1016/j.geomorph.2005.04.014
    [31] Muhs D R, Lancaster N, Skipp G L, 2017.A complex origin for the Kelso Dunes, Mojave National Preserve, California, USA:A case study using a simple geochemical method with global applications.Geomorphology, 276:222-243.doi: 10.1016/j.geomorph.2016.10.002
    [32] Page K J, Dare-Edwards A J, Owens J W et al., 2001.TL chro-nology and stratigraphy of riverine source bordering sand dunes near Wagga Wagga, New South Wales, Australia.Quaternary International, 83-85(1):187-193.doi:10.1016/S 1040-6182(01)00039-8
    [33] Seif E S S A, 2013.Assessing the engineering properties of con-crete made with fine dune sands:an experimental study.Ara-bian Journal of Geosciences, 6(3):857-863.doi:10.1007/s 12517-011-0376-6
    [34] Simpson E L, Hilbert-Wolf H L, Simpson W S et al., 2008.The interaction of aeolian and fluvial processes during deposition of the Upper Cretaceous capping sandstone member, Wahweap Formation, Kaiparowits Basin, Utah, U.S.A.Paleogeography, Paleoclimatology, Paleoecology, 270(1-2):19-28.doi: 10.1016/j.palaeo.2008.08.009
    [35] Smith A B, Jackson D W T, Cooper J A G, 2017.Three-dimen-sional airflow and sediment transport patterns over barch dunes.Geomorphology, 278:28-42.doi: 10.1016/j.geomorph.2016.10.025
    [36] Thomas D S G, Nash D J, Shaw P A et al., 1993.Present day lu-nette sediment cycling at Witpan in the arid southwestern Ka-lahari Desert.Catena, 20(5):515-527.doi: 10.1016/0341-8162(93)90045-Q
    [37] Walker I J, Shugar D H, 2013.Secondary flow deflection in the lee of transverse dunes with implications for dune morphody-namics and migration.Earth surface processes and landforms, 38(14):1642-1654.doi: 10.1002/esp.3398
    [38] Zuo Xiaoan, Zhao Halin, Zhao Xueyong et al., 2009.Changes on Landscape Pattern of Sand Dunes at Different Scales in Horqin Sandy Land.Journal of Desert Research, 29(5):785-795. (in Chinese)03pp386ra
    [39] Bullard J E, Nash D J, 1998. Linear dune pattern variability in the vicinity of dry valleys in the southwest Kalahari. Geomorphology, 23(1):35-54. doi: 10.1016/S0169-555X(97)00090-1
    [40] Bullard J E, Nash D J, 2000. Valley-marginal sand dunes in the south-west Kalahari:their nature, classification and possible origins. Journal of Arid Environments, 45(4):369-383. doi: 10.1006/jare.2000.0646
    [41] Burchsted D, Daniels M, Wohl E E, 2014. Introduction to the special issue on discontinuity of fluvial systems. Geomorphology, 205(SI):1-4. doi: 10.1016/j.geomorph.2013.04.004
    [42] Cai Yunlong, Song Changqing, Leng Shuying, 2009. Future development trends and priority areas of physical geography in China. Scientia Geographica Sinica, 29(5):619-626. (in Chinese)
    [43] Du Huishi, Hasi E, Yang Yi et al., 2012. Landscape pattern change and driving force of blowout distribution in the Hulun Buir Sandy Grassland. Sciences in Cold and Arid Regions, 4(5):431-438. (in Chinese)
    [44] Du Huishi, Jiang Hailing, Zhang Lifu et al., 2016. Evaluation of spectral scale effects in estimation of vegetation leaf area index using spectral indices methods. Chinese Geographical Science, 26(6):731-744. doi: 10.1007/s11769-016-0833-y
    [45] Duan Hanchen, Wang Tao, Xue Xian et al., 2013. Spatial-temporal evolution of aeolian desertification in the Horqin Sandy Land based on RS and GIS. Journal of Desert Research, 33(2):470-477. (in Chinese)
    [46] Duran O, Silva M V N, Bezerra L J C et al., 2008. Measurements and numerical simulations of the degree of activity and vegetation cover on parabolic dunes in north-eastern Brazil. Geomorphology, 102(3-4):460-471. doi:10.1016/j.geomorph. 2008.05.011
    [47] EBGAC (The Editorial Board of Geomorphological Atlas of the People's Republic of China), 2009. Geomorphological atlas of the People's Republic of China (1:1000000). Beijing:Science Press, 94-95. (in Chinese)
    [48] El-Baz F, Maingue M, Robinson C, 2000. Fluvio-aeolian dynamics in the north-eastern Sahara:the relationship between fluvial/aeolian systems and ground-water concentration. Journal of Arid Environments, 44(2):173-183. doi:10.1006/jare.1999. 0581
    [49] Ewing R C, Kocurek G, 2010. Aeolian dune-field pattern boundary conditions. Geomorphology, 114(3):175-187. doi:10. 1016/j.geomorph.2009.06.015
    [50] Ewing R C, Kocurek G, Lake L W, 2006. Pattern analysis of dune-field parameters. Earth Surface Processes and Landforms, 31(9):1176-1191. doi: 10.1002/esp.1312
    [51] Field J P, Breshears D D, Whicker J J, 2009. Toward a more holistic perspective of soil erosion:why aeolian research needs to explicitly consider fluvial processes and interactions. Aeolian Research, 1(1-2):9 17. doi: 10.1016/j.aeolia.2009.04.002
    [52] Han G, Zhang G F, Dong Y X, 2007. A model for the active origin and development of source-bordering dunefields on a semiarid fluvial plain:a case study from the Xiliaohe Plain, Northeast China. Geomorphology, 86(3-4):512-524. doi: 10.1016/j.geomorph.2006.10.010
    [53] Harrison Y, 1998. Late Pleistocene Aeolian and fluvial interactions in the development of the Nizzana dune field, Negev Desert, Israel. Sedimentology, 45(3):507-518. doi:10.1046/j. 1365-3091.1998.00151.x
    [54] Havholm K G, Running IV G L, 2005. Stratigraphy, sedimentology, and environmental significance of late mid-Holocene dunes, Lauder Sand Hills, glacial lake Hind Basin, southwestern Manitoba. Canadian Journal of Earth Sciences, 42(5):847-863. doi: 10.1139/e05-019
    [55] Hugenholtz C H, Wolfe S A, Walker I J et al., 2009.Spatial and temporal patterns of aeolian sediment transport on an inland parabolic dune, Bigstick Sand Hills, Saskatchewan, Canada. Geomorphology, 105(1-2):158-170. doi:10.1016/j.geomorph. 2007.12.017
    [56] Jiang Chanwen, Dong Zhibao, Wen Qing, 2013. Extraction of dune crest lines and calculation of dune-field pattern parameters on remote sensing image based on Matlab platform. Journal of Desert Research, 33(6):1636-1642. (in Chinese)
    [57] Joanna E B, David J N, 1998. Linear dune pattern variability in the vicinity of dry valleys in the southwest Kalahari. Geomorphology, 23 (1):35-54. doi: 10.1016/S0169-555X(97)00090-1
    [58] Lancaster N, 1988. Development of linear dunes in the southwestern Kalahari, southern Africa. Journal of Arid Environments, 14(3):233-244. doi: 0000-0003-1585-5282
    [59] Landsberg S Y, 1956. The orientation of dunes in Britain and Denmark in relation to wind. The Geographical Journal, 122(2):176-189. doi: 10.2307/1790847
    [60] Langford R P, 1989. Fluvial-aeolian interactions:Part I, modern systems. Sedimentology, 36(6):1023-1035. doi:10.1111/j. 1365-3091.1989.tb01540.x
    [61] Li Sen,Wang Yue, Hasi et al., 1997. Classification and development of aeolian sand landform in the Yurlung Zangbo Valley. Journal of Desert Research, 17(4):342-250. (in Chinese)
    [62] Liu B L, Coulthard T J, 2015. Mapping the interactions between rivers and sand dunes:Implications for fluvial and Aeolian geomorphology. Geomorphology, 231:246-257. doi: 10.1016/j.geomorph.2014.12.011
    [63] Liu Hujun, Wang Jihe, Liao Kongtai et al., 2009. Type and distribution of geomorphology of aeolian sediment at region of Suosuo Vale of Kumtag Desert. Arid land geography, 32(1):87-94. (in Chinese)
    [64] Liu Yanyan, Gong Yanming, Wang Xin et al., 2013. Volume fractal dimension of soil particles and relationships with soil physical-chemical properties and plant species diversity in an alpine grassland under different disturbance degrees. Journal of Arid Land, 5(4):480-487. (in Chinese)
    [65] Ma Yufeng, 2011. The interaction of aeolian and fluvial erosion processes in upper Yellow River. Beijing:Beijing Normal University, 40-46. (in Chinese)
    [66] Marín L, Forman S L, Valdez A et al., 2005. Twentieth century dune migration at the Great Sand Dunes National Park and Preserve, Colorado, relation to drought variability. Geomorphology, 70(1-2):163-183. doi:10.1016/j.geomorph.2005.04. 014
    [67] Muhs D R, Lancaster N, Skipp G L, 2017. A complex origin for the Kelso Dunes, Mojave National Preserve, California, USA:A case study using a simple geochemical method with global applications. Geomorphology, 276:222-243. doi: 10.1016/j.geomorph.2016.10.002
    [68] Page K J, Dare-Edwards A J, Owens J W et al., 2001. TL chronology and stratigraphy of riverine source bordering sand dunes near Wagga Wagga, New South Wales, Australia. Quaternary International, 83-85(1):187-193. doi:10.1016/S 1040-6182(01)00039-8
    [69] Seif E S S A, 2013. Assessing the engineering properties of concrete made with fine dune sands:an experimental study. Arabian Journal of Geosciences, 6(3):857-863. doi:10.1007/s 12517-011-0376-6
    [70] Simpson E L, Hilbert-Wolf H L, Simpson W S et al., 2008. The interaction of aeolian and fluvial processes during deposition of the Upper Cretaceous capping sandstone member, Wahweap Formation, Kaiparowits Basin, Utah, U.S.A. Paleogeography, Paleoclimatology, Paleoecology, 270(1-2):19-28. doi:10. 1016/j.palaeo.2008.08.009
    [71] Smith A B, Jackson D W T, Cooper J A G, 2017. Three-dimensional airflow and sediment transport patterns over barch dunes. Geomorphology, 278:28-42. doi:10.1016/j.geomorph. 2016.10.025
    [72] Thomas D S G, Nash D J, Shaw P A et al., 1993. Present day lunette sediment cycling at Witpan in the arid southwestern Kalahari Desert. Catena, 20(5):515-527. doi: 10.1016/0341-8162(93)90045-Q
    [73] Walker I J, Shugar D H, 2013. Secondary flow deflection in the lee of transverse dunes with implications for dune morphodynamics and migration. Earth surface processes and landforms, 38(14):1642-1654. doi: 10.1002/esp.3398
    [74] Zuo Xiaoan, Zhao Halin, Zhao Xueyong et al., 2009. Changes on Landscape Pattern of Sand Dunes at Different Scales in Horqin Sandy Land. Journal of Desert Research, 29(5):785-795. (in Chinese)
    [75]  
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Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China

doi: 10.1007/s11769-018-0951-9
Funds:  Under the auspices of Natural National Science Foundation of China (No. 41671002, 41401002)
    Corresponding author: WANG Zongming.E-mail:zongmingwang@iga.ac.cn

Abstract: The interaction between fluvial and aeolian processes can significantly change surface morphology of the Earth. Taking the Horqin Sandy Land as the research area and using Landsat series satellite remote sensing images, this study utilizes geomorphology and landscape ecology to monitor and analyze the aeolian geomorphology characteristics of the Horqin Sandy Land. Results show that the sand dunes of the Horqin Sandy Land are mainly distributed on alluvial plains along the banks of the mainstream and tributaries of the Western Liao River, and the sand dune types tend to simplify from west to east and from south to north. The aeolian geomorphology coverage tend to be decreasing in the past 40 years, with an average annual change rate of 0.31%. While the area of traveling dunes decreased, the area of fixed and semi-fixed dunes increased. The fractal dimensions of various types of sand dune have all remained relatively constant between 1.07 and 1.10, suggesting that they are experiencing a relatively stable evolutionary process. There is a complex interaction between fluvial and aeolian processes of the Horqin Sandy Land, which plays a central role in surface landscape molding. Sand dunes on both sides of different rivers on the Horqin Sandy Land present certain regularity and different characteristics in terms of morphology, developmental scale, and spatial pattern. There are six fluvial-aeolian interaction modes in this area:supply of sand sources by rivers for sand dune development, complete obstruction of dune migration by rivers, partial obstruction of dune migration by rivers, influence of river valleys on dune developmental types on both sides, influence of river valleys on dune developmental scale on both sides, and river diversion due to obstruction and forcing by sand dunes. This study deepens our understanding of the surface process mechanism of the interaction between fluvial and aeolian processes in semi-arid regions, and provides a basis for researches on regional landscape responses in the context of global environmental change.

DU Huishi, WANG Zongming, MAO Dehua. Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China[J]. Chinese Geographical Science, 2018, 28(4): 624-635. doi: 10.1007/s11769-018-0951-9
Citation: DU Huishi, WANG Zongming, MAO Dehua. Characteristics of Sand Dune Pattern and Fluvial-aeolian Interaction in Horqin Sandy Land, Northeast Plain of China[J]. Chinese Geographical Science, 2018, 28(4): 624-635. doi: 10.1007/s11769-018-0951-9
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