|本期目录/Table of Contents|

[1]王 帅,哈 斯.风蚀地貌形态与过程研究进展[J].地球科学与环境学报,2009,31(01):100-105.
 WANG Shuai,HA Si.Advances in the Study of Geomorphology and Process of Wind Erosion Landforms[J].Journal of Earth Sciences and Environment,2009,31(01):100-105.
点击复制

风蚀地貌形态与过程研究进展(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第31卷
期数:
2009年第01期
页码:
100-105
栏目:
环境地学
出版日期:
2009-03-15

文章信息/Info

Title:
Advances in the Study of Geomorphology and Process of Wind Erosion Landforms
文章编号:
1672-6561(2009)01-0100-06
作者:
王 帅12哈 斯2
(1.浙江省水利河口研究院,浙江 杭州 310020; 2.北京师范大学 中国沙漠研究中心 地表过程与资源生态国家重点实验室,北京 100875)
Author(s):
WANG Shuai12 HA Si2
(1.Zhejiang Institute of Hydraulics and Estuary, Hangzhou 310020, Zhejiang, China; 2.School of Resources Science and Technology, State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China)
关键词:
风蚀地貌地貌学发育过程综述
Keywords:
wind erosion landforms geomorphology developmental process review
分类号:
P931.3
DOI:
-
文献标志码:
A
摘要:
辨析了雅丹、风蚀坑等主要风蚀地貌的概念,雅丹是典型的风蚀正地貌形态,通过回顾雅丹地貌形态与过程的研究历史与进展,发现目前对其发育过程的认识尚不清楚,并且只关注了对残存土墩的观测和分析,没有充分重视凹槽的形态动力学过程;风蚀坑是典型的风蚀负地貌形态,特别是草原景观转变为沙地景观的临界阈现象,目前已经对独立风蚀坑的形态、气流特征、沉积物粒度以及植被演替过程等方面进行了初步研究,但由于风蚀坑形态是多因素共同作用的结果,需要由单因素观测转向综合分析其形态动力学过程。认为对风蚀过程机理及其模拟的研究中,在利用风洞模拟实验、野外观测等手段对风蚀过程微观尺度进行研究的同时,也需要加强通过遥感和GIS手段从景观尺度对风蚀地貌发展变化过程进行分析。
Abstract:
With global warming and drought enhancement, the geomorphic process of wind erosion landforms becomes one of the main surficial processes in arid and semi-arid areas. However, compared with wind accumulated landforms, less attention has been given to the wind erosion landforms. This paper reviews the processes of initiation, evolution, dynamics and geomorphology of yardangs and blowouts. Yardang and blowout are two main wind erosion landforms, one is positive and one is negative. The generation of yardangs results from complex interactions between internal factors and external factors, and they are also influenced by weathering process, fluvial erosion and mass movement. Aerodynamic system produces differential pressures giving rise to vorticity which is one of the most frequent and important wind movements responsible for the erosion. Blowout geomorphology, dynamics and evolution are also examined. Blowouts are the threshold of grasslands converting to shrublands in arid and semi-arid ecosystems. Throughout the review, the gaps in present understanding of dune processes and a range of ideas for new research possibilities are provided.

参考文献/References:

[1] David S G T.Arid Zone Geomorphology:Process,Form and Change in Drylands[M].2nd Edition.Chichester:Wiley,1998.
[2] Abrahams A D,Parsons A.Geomorphology of Desert Environments[M].London:Chapman and Hall,1994.
[3] 鲁瑞洁,哈 斯,岳兴玲,等.第四纪风沙环境证据的研究进展[J].地理科学进展,2004,23(3):82-90.
[4] Hedin S A,Bealby J T.Central Asia and Tibet Towards the Holy City of Lassa[M].New York:Greenwood Press,1970.
[5] Stein M A.Exploration in Central Asia[J].Geographical Journal,1909,34:5-36.
[6] Beadnell H J L.Lake Basins Created by Wind Erosion [J].Journal of Geology,1909,3:47-49.
[7] Melton F A.A Tentative Classification of Sand Dunes:Its Application to Dune History in the Southern High Plain [J].Journal of Geology,1940,48:113-174.
[8] Keyes C R.Rock Floor of Interment Plains of the Arid Region[J].Bulletin of the Geological Society of American,1908,19:63-92.
[9] Bryan K.Wind Erosion Near Lees Ferry,Arizona[J].American Journal of Science,1923,5(6):291-306.

[10] Mckee E D. 世界沙海的研究[M].赵兴梁,译.银川: 宁夏人民出版社,1993.

[11] Carter R W G,Hesp P A,Nordstrom K.Erosional Landforms in Coastal Dunes[C]∥ Nordstrom K,Psuty N, Carter B.Coastal Dunes:Form and Process.Chichester Sussex:Wiley,1990:217-252.

[12] Hesp P A,Hyde R.Flow Dynamics and Geomorphology of a Trough Blowout[J].Sedimentology,1996,43(3):505-525.

[13] 张德平,王效科,哈 斯,等.呼伦贝尔沙质草原风蚀坑研究(1)—形态、分类、研究意义[J].中国沙漠,2006,26(6):894-902.

[14] Zhang A M,Feng Z W,Wang X K,et al.Sandy Grassland Blowouts in Hulunbuir,Northeast China:Geomorphology,Distribution,and Causes[J].Progress in Natural Science,2007,17(1):68-73.

[15] 吴 正.风沙地貌与治沙工程学[M].北京:科学出版社, 2003.

[16] 郑本兴,张林源,胡孝宏.玉门关西雅丹地貌的分布和特征及形成时代问题[J].中国沙漠, 2002,22(1):40-46.

[17] Bosworth T O.Geology and Palaeontology of Northwest Peru[M].London: Macmillan,1922.

[18] Grolier M J,Mccauley J F,Breed C S,et al.Yardangs of the Western Desert[J].Geographical Journal,1980,146(1):86-87.

[19] Ward A W,Greeley R.Evolution of the Yardangs at Rogers Lake,California[J].Bulletin of the Geological Society of America,1984,95(7):829-837.
[20] Whitney M I.The Role of Vorticity in Developing Lineation by Wind Erosion[J].Bulletin of the Geological Society of America,1978,89(1):1-18.
[21] McCauley J F,Ward A W,Breed C S,et al.The Yardangs at Rogers Dry Lake,California[J].Geological Society of America,1977,9(7):150-152.
[22] Embabi N S.Playas of the Western Desert,Egypt [J].Ann Acad Sci Fenn Geol-Geog,1999,160:5-47.
[23] Brookes I A.Aeolian Erosional Lineations in the Libyan Desert,Dakhla Region,Egypt[J].Geomorphology,2001,39(3):189-209.
[24] 屈建军,郑本兴,俞祁浩,等.罗布泊东阿奇克谷地雅丹地貌与库姆塔格沙漠形成的关系[J].中国沙漠, 2004,24(3):294-300.
[25] 夏训诚.重返罗布泊[J].大自然探索,2003(4):4-9.
[26] Hesp P A.Foredunes and Blowouts:Initiation,Geomorphology and Dynamics[J].Geomorphology, 2002,48(1):245-268.
[27] Livingstone I,Warren A.Aeolian Geomorphology:An Introduction[M].New Jersey:Prentice Hall,1996.
[28] 朱震达,吴 正,刘 恕,等.中国沙漠概论[M].北京:科学出版社, 1980.
[29] Smith H T U.Physiography and Photo Interpretation of Coastal Sand Dunes[R].Washington:Office of Naval Research,Geographical Branch,1960.
[30] Cooper W S.Coastal Sand Dunes of California[M].Boulder:Geological Society of America,1967.
[31] 王 帅.沙质草原风蚀坑表面气流与粒度响应[D]. 北京: 北京师范大学,2007.
[32] 王 帅,哈 斯.呼伦贝尔沙质草原区域风况与风蚀坑形态特征[J].水土保持研究,2008,15(3):74-76.
[33] 张德平,王效科,孙宏伟,等.呼伦贝尔沙质草原风蚀坑研究(Ⅳ):人类活动的影响[J].中国沙漠,2007,27(2):214-220.
[34] 张德平,王效科,胡日乐,等.呼伦贝尔沙质草原风蚀坑研究(Ⅲ):微地貌和土层的影响[J].中国沙漠,2007,27(1):25-31.
[35] Gares P A.Eolian Sediment Transport and Dune Formation on Undeveloped and Developed Shorelines[D].New Brunswick:The State University of New Jersey,1987.
[36] Eriksson P G,Nixon N,Snyman C P,et al.Ellipsoidal Parabolic Dune Patches in the Southern Kalahari Desert[J].Journal of Arid Environments,1989,16(2):111 -124.
[37] 张德平,孙宏伟,王效科,等.呼伦贝尔沙质草原风蚀坑研究(Ⅱ):发育过程[J].中国沙漠,2007,27(1):20-24.
[38] Gutierrez-Elorza M,Desir G,Gutierrez-Santolalla F,et al.Origin and Evolution of Playas and Blowouts in the Semiarid Zone of Tierra de Pinares(Duero Basin, Spain)[J].Geomorphology,2005,72(1/4):177-192.
[39] 史培军.试论科尔沁南部大青沟地区沙漠化土地的地表形态特征及其发育过程[J].内蒙古师范大学学报:自然科学版, 1986(1):43-54.
[40] 张 萍,哈 斯,王 帅,等.呼伦贝尔沙质草原风蚀坑积沙区的植被分带性[J].自然资源学报,2008,23(2):237-244.
[41] Thomas D S G,Knight M,Wiggs G F S.Remobilization of Southern African Desert Dune Systems by Twenty-first Century Global Warming[J].Nature,2005,435:1218-1221.
[42] Jungerius P D,Witter J V,Vanboxel J H.The Effects of Changing Wind Regimes on the Development of Blowouts in the Coastal Dunes of the Netherlands[J].Landscape Ecology,1991,6(1/2):41-48.
[43] Jungerius P D,Meulen F.The Development of Dune Blowouts,as Measured with Erosion Pins and Sequential Air Photos[J].Catena,1989,16(4/5):369-376.
[44] Lancaster N.Dynamics of Deflation Hollows in the Elands Bay Area,Cape Province,South Africa[J].Catena,1986,13(1/2):139-153.
[45] Hesp P A.Flow Dynamics in a Trough Blowout[J].Boundary-Layer Meteorology,1996,77(3/4):305-330.
[46] 王 帅,哈 斯,张 军,等.呼伦贝尔沙质草原碟形风蚀坑表面气流及其意义[J].中国沙漠, 2007,27(5):745-749.
[47] 任朝霞,杨达源.西北干旱区近50年气候变化特征与趋势[J].地球科学与环境学报,2007,29(1):99-102.
[48] Okin G S,Gillette D A,Herrick J E.Multi-scale Controls on and Consequences of Aeolian Processes in Landscape Change in Arid and Semi-arid Environments[J].Journal of Arid Environments,2006,65(2):253-275.
[49] Peters D P C,Havstad K M.Nonlinear Dynamics in Arid and Semi-arid Systems:Interactions Among Drivers and Processes Across Scales[J].Journal of Arid Environments,2006,65(2):196-206.
[50] 王 涛,赵哈林.中国沙漠科学五十年[J].中国沙漠,2005,25(2):145-165.

相似文献/References:

备注/Memo

备注/Memo:
收稿日期:2008-05-20
基金项目: 国家自然科学基金项目(40471013); 十一五国家科技支撑计划项目(2006BAD26B07)
作者简介: 王 帅(1982-),男,内蒙古鄂尔多斯人,工程师,农学硕士,从事水土资源保护及荒漠化过程与防治研究。 E-mail:shuaiwang@ires.cn

更新日期/Last Update: 2009-03-20