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  • CN 62-1070/P
  • ISSN 1000-694X
  • 双月刊 创刊于1981年
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沙漠与沙漠化

不同气候带的河道与沙丘分布格局及其类型划分

  • 李小妹 ,
  • 严平 ,
  • 钱瑶 ,
  • 吴伟
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  • 1. 陕西师范大学 地理科学与旅游学院, 陕西 西安 710119;
    2. 北京师范大学 减灾与应急管理研究院/地表过程与资源生态国家重点实验室, 北京 100875
李小妹(1979-),女,安徽宿州人,博士,研究方向为干旱区地貌。E-mail:lixiaomei8477@sina.com

收稿日期: 2016-02-02

  修回日期: 2016-04-06

  网络出版日期: 2017-09-20

基金资助

国家重大科学研究计划项目(2013CB956001);国家自然科学基金项目(41171003);中央高校基本科研业务费项目(GK201703047)

Distribution Patterns and Its Classification at the Scale of Channel-Sand Dune in Different Climate Zones

  • Li Xiaomei ,
  • Yan Ping ,
  • Qian Yao ,
  • Wu Wei
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  • 1. School of Geogrophy and Tourism, Shaanxi Normal University, Xi'an 710119, China;
    2. Academy of Disaster Reduction and Emergency Management/State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China

Received date: 2016-02-02

  Revised date: 2016-04-06

  Online published: 2017-09-20

摘要

风水交互作用是干旱区常见的地貌现象和重要的地表过程,干旱区河流通过提供物源和场所控制沙漠分布的格局,沙漠分布与风沙活动制约河道发育和泥沙输移,在不同时空尺度表现不一,但关于二者交互作用的分类处于探索阶段,尚未形成分类体系,尤其在地貌格局分类上多为定性描述。因此,自西向东选择位于3个气候带的中国西部克里雅河、中部毛不拉格孔兑以及东部西拉木伦河,利用遥感影像解译获取河道与沙丘信息,探讨近源沙丘的分布与河型之间的组合关系。结果表明:河型、河流流向与风向之间的关系、水文以及距离河道的远近影响河道与沙丘组合的地貌格局;在河道-沙丘尺度上,划分为弯曲河道-对称式边滩沙丘、顺直河道-边滩沙丘、分汊河道-心滩式沙丘、网状河道-格状镶嵌式沙丘4种类型。

本文引用格式

李小妹 , 严平 , 钱瑶 , 吴伟 . 不同气候带的河道与沙丘分布格局及其类型划分[J]. 中国沙漠, 2017 , 37(5) : 821 -829 . DOI: 10.7522/j.issn.1000-694X.2016.00044

Abstract

Aeolian-fluvial interaction is a common landform phenomenon and an important earth surface process in the arid regions. The rivers in the arid regions significantly influence the form and distribution of the sand dunes by providing sediments and accommodation. In return, the distributions of the sand dunes and the sand activities have restricted the growth of the river channel and the transportation of the sediment in different temporal-spatial scale. However, the research on the classification system of aeolian-fluvial interaction has not been formed in the exploration stage, especially in the landscape pattern classification on qualitative description. This research selected the main river basins and deserts in the northern China, including the three typical river basins, the Keriya River in the west, the Mu Bulag River in the middle and the Xar Moron River in the east of the northern China to observe such interactions between fluvial and aeolian system. By employing the knowledge and methods of geomorphology and landscape ecology based on the data of remote sensing, this thesis provides a comprehensive understanding of the landscape distribution pattern between river channel and sand dunes. Furthermore, the types of the interactions between sand dunes and rivers are classified. The main results show that at the scale of channel-sand dune, the distribution patterns of sand dunes and rivers was divide as four types, meandering channel-symmetrical interleaving dunes, straight channel-riverside dunes, anabranches channel-river-island dunes and anastomosing channel-grid-like dunes.

参考文献

[1] 董治宝,屈建军,钱广强,等.库姆塔格沙漠风沙地貌区划[J].中国沙漠,2010,31(4):805-814.
[2] 师长兴,许炯心,蔡强国,等.地貌过程研究回顾与展望[J].地理研究,2010,29(9):1546-1560.
[3] 许炯心.黄河中游多沙粗沙区的风水两相侵蚀产沙过程[J].中国科学:D辑,2000,30(5):540-548.
[4] Kirkby M J.The stream head as a significant geomorphic threshold[D].Leeds,UK:University of Leeds,1978.
[5] 史培军,王静爱.论风水两相作用地貌的特征及其发育过程[J].内蒙古林学院学报,1986,8(2):88-97.
[6] Liu B L,Coulthard T J.Mapping the interactions between rivers and sand dunes:implications for fluvial and aeolian geomorphology[J].Geomorphology,2015,231:246-257.
[7] Al-Masrahy M A,Mountney N P.A classification scheme for fluvial-aeolian system interaction in desert-margin settings[J].Aeolian Research,2015,17:67-88.
[8] Langford R P,Chan M A.Fluvial-aeolian interactions:part Ⅱ,ancient systems[J].Sedimentology,1989,36:1037-1051.
[9] Bullard J E,Nash D J.Valley-marginal sand dunes in the south-west Kalahari:their nature,classification and possible origins[J].Journal of Arid Environment,2000,45:369-38.
[10] 李森,董光荣,申建友,等.雅鲁藏布江河谷风沙地貌形成机制与发育模式[J].中国科学:D辑,1999,29(1):91-95.
[11] 马玉凤,严平,张登山.基于GIS的青海共和盆地风水交互侵蚀格局初析[J].干旱区资源与环境,2011,25(1):152-156.
[12] 李小妹,严平.中国北方地区沙漠与河流景观格局[J].地理科学进展,2014,33(9):1198-1208.
[13] 李小妹.中国北方典型流域沙漠与河流交互关系及其表现[D].北京:北京师范大学,2015.
[14] Page K J.Australian landform example No.20.Riverine source bordering sand dune[J].Australian Geographer,1971,11:603-605.
[15] Page K J,Dare-Edwards A J,Owens J W,et al.TL chronology and stratigraphy of riverine source bordering sand dunes near Wagga Wagga,New South Wales,Australia[J].Quaternary International,2001,85:187-193.
[16] Bullard J E,McTainsh,G H.Aeolian-fluvial interactions in dryland environments:examples,concepts and Australia case study[J].Progress in Physical Geography,2003,27:471-501.
[17] Ivester A H,Leigh D S.Riverine dunes on the coastal plain of Georgia,USA[J].Geomorphology,2003,51:289-311.
[18] Wasson R J,Hyde R.Factors determining desert dune type[J].Nature,1983,304:337-339.
[19] Livingstone I,Warren A.Aeolian Geomorphology:An Introduction[M].Essex,UK:Addison Wesley Longman Limited,1996.
[20] 吴正.风沙地貌与治沙工程学[M].北京:科学出版社,2009:17-24.
[21] Wopfner H,Twidale C R.Formation and age of desert dunes in the Lake Eyre depocentres in central Australia[J].Geologische Rundschau,1988,77:815-834.
[22] Goudie A S.Encyclopedia of Geomorphology (Volume 1)[M].London,UK:Routledge Ltd,2004.
[23] Maroulis J C,Nanson G C,Price D M,et al.Aeolian-fluvial interaction and climate change:source-bordering dune development over the past~100 ka on Cooper Creek,central Au stralia[J].Quaternary Science Reviews,2007,26:386-404.
[24] 新疆克里雅河及塔克拉玛干科学探险考察队.克里雅河及塔克拉玛干科学探险考察报告[M].北京:中国科学技术出版社,1991.
[25] Yang X P,Zhu Z D,Jaekel D.Quaternary palaeoenvironment change and landscape evolution along the Keriya River,Xinjiang,China:the relationship between high mountain glaciation and landscape evolution in foreland desert regions[J].Quaternary International,2002,97/98:155-166.
[26] 许林军,杨亚娟,朱莉莉,等.毛不拉孔兑水土流失特征与防治布局[J].水土保持应用技术,2011(6):32-34.
[27] 许炯心.黄河内蒙古段支流"十大孔兑"侵蚀产沙的时空变化及其成因[J].中国沙漠,2014,34(6):1641-1649.
[28] 杨文斌,林凤友,樊忠成.西拉木伦河流域防洪治理工程水土保持措施探讨[J].内蒙古水利,2014(2):79-80.
[29] Han G,Zhang G F,Dong Y X.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[J].Geomorphology,2007,86:512-524.
[30] Rust B R.A classification of alluvial channel systems[M]//Miall A D.Fluvial Sedimentology.Eenver,USA:Stacs Data Service Ltd,1978:187-198.
[31] Nanson G C,Chen X Y,Price D M.Aeolian and fluvial evidence of changing climate and wind patterns during the past 100 ka in the western Simpson Desert,Australia[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1995,113:87-102.
[32] Lancaster N.Control of eolian dune Size and spacing[J].Geology,1988,16:972-997.
[33] Twidale C R,Wopfner H.Dune fields[M]//Tyler M J,Twidale C R,Davies M,et al.Natural History of the North East Deserts.Adelaide,Australia:Royal Society of South Australia,1990:45-60.
[34] Bullard J E,Nash D J.Linear dune pattern variability in the vicinity of dry valleys in the southwest Kalahari[J].Geomorphology,1998,23(1):35-54.
[35] Han G,Zhang G F,You,Li,et al.Deflated rims along the Xiangshui River on the Xiliaohe Plain,Northeast China:a case of active fluvial-aeolian interactions[J].Geomorphology,2016,257:47-56.
[36] 王勇,韩广,杨林,等.响水河中游右岸沙丘群粒度分布特征[J].中国沙漠,2017,37(1):26-32.
[37] 韩广,张桂芳.河流演变在科尔沁沙地形成和演化中的作用初探——以科尔沁沙地南部教来河中游沙地为例[J].中国沙漠,2001,21(2):130-133.
[38] 秦小光,刘嘉麒,裘善文,等.科尔沁沙地及其古水文网的演化变迁[J].第四纪研究,2010,31(1):80-95.
[39] 倪晋仁,王随继.论顺直河流[J].水利学报,2000(12):14-20.
[40] Begin Z B.The relationship between flow-shear stress and stream pattern[J].Journal of Hydrology,1981,52:307-319.
[41] 王随继,倪晋仁,王光谦.古河型演化模式及其影响因素的沉积体系分析[J].石油勘探与开发,2000,27(5):102-105.
[42] 王随继.两类多河道河流的形成模式及河道稳定性比较[J].地球学报,2002,23(1):89-93.
[43] Zhou N,Zhang C L,Wu X X,et al.The geomorphology and evolution of aeolian landforms within a river valley in a semi-humid environment:a case study from Mainling Valley,Qinghai-Tibet Plateau[J].Geomorphology,2014,224:27-38.
[44] Smith D G,Smith N D.Sedimentation in anastomosed river systems:examples from alluvial valleys near Banff,Al-berta[J].Journal of Sedimentary Petrology,1980,50:157-164.
[45] Knighton A D,Nanson G C.Anastomosis and the continuum of channel pattern[J].Earth Surface and Processes Landforms,1993,18:613-625.
[46] Yan P,Li X M,Ma Y F,et al.Morphological characteristics of interactions between deserts and rivers in northern China[J].Aeolian Research,2015,19:225-233.
[47] Breed C S,Fryberger S G,Andrews S,et al.Regional studies of sand seas using Landsat (ERTS) imagery[M]//Mckee E D.A Study of Global Sand Seas,1979:305-397.
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