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2016 , Vol. 36 >Issue 4: 951 - 961

DOI: https://doi.org/10.7522/j.issn.1000-694X.2015.00044

沙漠与沙漠化

火星风沙地貌研究进展

  • 李继彦 ,
  • 董治宝
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  • 1. 中国科学院寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000;
    2. 太原师范学院 地理科学学院, 山西 晋中 030619;
    3. 陕西师范大学 旅游与环境学院, 陕西 西安 710062
李继彦(1984-),男,山东曹县人,博士研究生,主要从事风沙地貌研究.E-mail:jyli@lzb.ac.cn

收稿日期: 2014-12-11

  修回日期: 2015-01-26

  网络出版日期: 2016-07-20

基金资助

国家重大科学研究计划（2013CB956000）；国家自然科学基金项目（41130533，41171010）

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Research Progress of Aeolian Landforms on Mars

  • Li Jiyan ,
  • Dong Zhibao
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  • 1. Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2. School of Geography Science, Taiyuan Normal University, Jinzhong 030619, Shanxi, China;
    3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062, China

Received date: 2014-12-11

  Revised date: 2015-01-26

  Online published: 2016-07-20

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摘要

作为最活跃的地貌塑造外营力，风力作用在火星表面塑造了各种各样的地貌形态。对火星风沙活动及风沙地貌的认识是随着观测和探测技术的进步而逐渐明确的。火星沙丘在北极地区连绵成带状分布，在其他地区分布比较零散，且主要与撞击坑、河谷和山谷相伴分布。火星风沙地貌与地球上相应的地貌类型形态相似而规模更大，表明两个星球上塑造风沙地貌的动力系统具有一定的相似性。火星沙丘主要由玄武岩质（北极部分沙丘为石膏质）颗粒堆积而成，沉积物粒度比地球粗，主要是由中沙和粗纱组成。随着获取影像时空分辨率的提高和着陆器在火星近表面的观测，发现火星上部分区域的沙丘和沙波纹比较活跃。同地球一样，火星风沙地貌也可指示火星气候的变化。

关键词： 风沙地貌; 行星地貌; 沙丘; 雅丹; 火星

本文引用格式

李继彦 , 董治宝 . 火星风沙地貌研究进展[J]. 中国沙漠, 2016 , 36(4) : 951 -961 . DOI: 10.7522/j.issn.1000-694X.2015.00044

Abstract

As the most active external geomorphic agency, wind shaped a diversity of aeolian landforms on Martian surface. The understanding and knowledge to aeolian activity and landforms on Mars is gradually becoming clear with the development of techniques on observation and exploration. Aeolian dunes on the north polar form a continuous belt to be the only sand desert on Mars. Whereas dunes in the other regions are much sporadic and coexist with craters, wadies and valleys. Compared with the counterparts on Earth, the aeolian landforms on Mars are much larger in size but the external morphology is very similar, which indicates the similarity of geomorphic agencies on both planets. The Martian dunes are mainly accumulated by basaltic grains, while some dunes in the north polar are deposited by gypsum. The grain size of sand on Mars is much coarser than on Earth and the dunes are mainly composed of medium and coarse sand. With the increasing of temporal-spatial resolution of obtained remote images and the near surface observation of landers, it indicates that dunes and ripples in some region are still active. The aeolian landforms can also indicate climate change on Mars, just as on Earth.

Key words： aeolian landform; planetary landform; dune; Yardang; Mars

参考文献

[1] Glasby G P.Mars,our neighbour[J].Geology Today,2012,28(6):214-246.
[2] 倪怀玮,郑永飞.火星生命研究的进展与前景[J].地球科学进展,2002,17(4):515-520.
[3] 董治宝.中国风沙物理研究五十年(Ⅰ)[J].中国沙漠,2005,25(3):293-305.
[4] 董治宝,郑晓静.中国风沙物理研究50 a(Ⅱ)[J].中国沙漠,2005,25(6):795-815.
[5] 董治宝,王涛,屈建军.100 a来沙漠科学的发展[J].中国沙漠,2003,23(1):1-5.
[6] Antoniadi E M.The Planet Mars[M].Shaldon Devon,UK:Keith Reid Limited,1975:1-65.
[7] Cutts J A,Smith R S U.Eolian deposits and dunes on Mars[J].Journal of Geophysical Research,1973,78(20):4139-4154.
[8] McCauley J F,Carr M H,Cutts J A,et al.Preliminary mariner 9 report on the geology of Mars[J].Icarus,1972,17(2):289-327.
[9] Sagan C,Veverka J,Fox P,et al.Variable features on Mars:Preliminary mariner 9 television results[J].Icarus,1972,17(2):346-372.
[10] Smith H T U.Aeolian deposition in Martian craters[J].Nature,1972,238(83):72-74.
[11] Arvidson R E.Wind-blown streaks,splotches,and associated craters on Mars:Statistical analysis of Mariner 9 photographs[J].Icarus,1974,21(1):12-27.
[12] Barlow N.Mars:An Introduction to Its Interior,Surface and Atmosphere[M].Cambridge,UK:Cambridge University Press,2008:1-19.
[13] Carr M H,Masursky H,Baum W A,et al.Preliminary results from the Viking orbiter imaging experiment[J].Science,1976,193(4255):766-776.
[14] Ward A W,Doyle K B,Helm P J,et al.Global map of eolian features on Mars[J].Journal of Geophysical Research:Solid Earth,1985,90(B2):2038-2056.
[15] Golombek M P,Cook R A,Economou T,et al.Overview of the Mars Pathfinder mission and assessment of landing site predictions[J].Science,1997,278(5344):1743-1748.
[16] Hayward R K,Mullins K F,Fenton L K,et al.Mars global digital dune database and initial science results[J].Journal of Geophysical Research:Planets,2007,112:JE002943.
[17] Craddock R A.Aeolian processes on the terrestrial planets:Recent observations and future focus[J].Progress in Physical Geography,2012,36(1):110-124.
[18] Bridges N T,Greeley R,Haldemann A F C,et al.Ventifacts at the Pathfinder landing site[J].Journal of Geophysical Research:Planets,1999,104(E4):8595-8615.
[19] Greeley R,Kuzmin R O,Rafkin S C R,et al.Wind-related features in Gusev crater,Mars[J].Journal of Geophysical Research:Planets,2003,108:JE002006.
[20] Greeley R,Squyres S W,Arvidson R E,et al.Wind-related processes detected by the Spirit rover at Gusev Crater,Mars[J].Science,2004,305(5685):810-813.
[21] Sullivan R,Banfield D,Bell J F,et al.Aeolian processes at the Mars exploration rover Meridiani Planum landing site[J].Nature,2005,436(7047):58-61.
[22] Geissler P E,Sullivan R,Golombek M,et al.Gone with the wind:Eolian erasure of the Mars Rover tracks[J].Journal of Geophysical Research:Planets,2010,115:JE003674.
[23] Smith P H,Bell J F,Bridges N T,et al.Results from the Mars Pathfinder camera[J].Science,1997,278(5344):1758-1765.
[24] Silvestro S,Vaz D A,Ewing R C,et al.Pervasive aeolian activity along rover Curiosity's traverse in Gale Crater,Mars[J].Geology,2013,41(4):483-486.
[25] Silvestro S,Vaz D A,Fenton L K,et al.Active aeolian processes on Mars:A regional study in Arabia and Meridiani Terrae[J].Geophysical Research Letters,2011,38(20):GL048955.
[26] Berman D C,Balme M R,Rafkin S C R,et al.Transverse aeolian ridges (TARs) on Mars II:Distributions,orientations,and ages[J].Icarus,2011,213(1):116-130.
[27] Zimbelman J R,Griffin L J.HiRISE images of yardangs and sinuous ridges in the lower member of the Medusae Fossae Formation,Mars[J].Icarus,2010,205(1):198-210.
[28] Zimbelman J R.Transverse aeolian ridges on Mars:First results from HiRISE images[J].Geomorphology,2010,121(1):22-29.
[29] Bourke M C,Philippoff A,Bridges N.Studies of dune change on Mars combining MOC and HiRISE images[C]//Lunar and Planetary Science Conference,2009:1748.
[30] Greeley R,Iversen J D,Pollack J B,et al.Wind Tunnel Studies of Martian Aeolian Processes[J].Proceedings of the Royal Society.Series A,Mathematical and Physical Sciences,1974,341(1626):331-360.
[31] Greeley R,Iversen J D,Pollack J B,et al.Wind tunnel simulations of light and dark streaks on Mars[J].Science,1974,183(4127):847-849.
[32] Greeley R,Iversen J D.Wind as A Geological Processes:on Earth,Mars,Venus and Titan[M].Cambridge,UK:Cambridge University Press,1985:67-104.
[33] Greeley R.Saltation impact as a means for raising dust on Mars[J].Planetary and Space Science,2002,50(2):151-155.
[34] Anderson R S,Haff P K.Simulation of eolian saltation[J].Science,1988,241(4867):820-823.
[35] Gillies J A,Nickling W G,King J,et al.Modeling aeolian sediment transport thresholds on physically rough Martian surfaces:A shear stress partitioning approach[J].Geomorphology,2010,121(1):15-21.
[36] Sagan C,Bagnold R A.Fluid transport on Earth and aeolian transport on Mars[J].Icarus,1975,26(2):209-218.
[37] Greeley R,Bridges N T,Kuzmin R O,et al.Terrestrial analogs to wind-related features at the Viking and Pathfinder landing sites on Mars[J].Journal of Geophysical Research:Planets,2002,107: JE001481.
[38] Williams S H,Zimbelman J R,Ward A W.Large ripples on Earth and Mars[C]//Lunar and Planetary Science Conference,2002:1508.
[39] Zimbelman J R,Irwin R P,Williams S H,et al.Granule ripple on Earth and Mars:documented movement at Great Sand Dunes National Park,and implications for granule movement on Mars[CDROM]//LPSC XXVIII.Abstract,2007:1324.
[40] Laity J E,Bridges N T.Ventifacts on Earth and Mars:Analytical,field,and laboratory studies supporting sand abrasion and windward feature development[J].Geomorphology,2009,105(3):202-217.
[41] Bourke M C,Goudie A S.Varieties of barchan form in the Namib Desert and on Mars[J].Aeolian Research,2009,1(1):45-54.
[42] Steinbacher R H,Kliore A,Lorell J,et al.Mariner 9 science experiments:Preliminary results[J].Science,1972,175(4019):293-294.
[43] McCauley J F.Mariner 9 evidence for wind erosion in the equatorial and mid-latitude regions of Mars[J].Journal of Geophysical Research,1973,78(20):4123-4137.
[44] Baker V R.The geomorphology of Mars[J].Progress in Physical Geography,1981,5(4):473-513.
[45] 岳宗玉,谢红接,刘建忠,等.火星表面沙丘中冲沟的成因及对撞击坑壁冲沟成因的启发[J].地球科学,2010,35(2):291-301.
[46] Tsoar H,Greeley R,Peterfreund A R.Mars:The north polar sand sea and related wind patterns[J].Journal of Geophysical Research,1979,84(B14):8167-8180.
[47] Thomas P C,Gierasch P J.Polar margin dunes and winds on Mars[J].Journal of Geophysical Research:Planets,1995,100(E3):5397-5406.
[48] Lancaster N,Greeley R.Sediment volume in the north polar sand seas of Mars[J].Journal of Geophysical Research:Solid Earth,1990,95(B7):10921-10927.
[49] Thomas P.North-south asymmetry of eolian features in Martian polar regions:Analysis based on crater-related wind markers[J].Icarus,1981,48(1):76-90.
[50] Peterfreund A R.Visual and infrared observations of wind streaks on Mars[J].Icarus,1981,45(2):447-467.
[51] Thomas P,Weitz C.Sand dune materials and polar layered deposits on Mars[J].Icarus,1989,81(1):185-215.
[52] Hansen C J,Bourke M,Bridges,N T,et al.Seasonal erosion and restoration of Mars' northern polar dunes[J].Science,2011,331(6017):575-578.
[53] Portyankina G,Pommerol A,Aye K M,et al.Observations of the northern seasonal polar cap on Mars II:HiRISE photometric analysis of evolution of northern polar dunes in spring[J].Icarus,2012,225(2):898-910.
[54] Bourke M C,Balme M,Zimbelman J.A comparative analysis of barchan dunes in the intra-crater dune fields and the north polar sand sea[C]//Lunar and Planetary Science Conference,2004:1453.
[55] Bourke M C,Wilson S A,Zimbelman J R.The variability of transverse aeolian ridges in troughs on Mars[C]// Lunar and Planetary Science Conference,2003:2090.
[56] Balme M,Berman D C,Bourke M C,et al.Transverse aeolian ridges (TARs) on Mars[J].Geomorphology,2008,101(4):703-720.
[57] Lancaster N.Linear dunes[J].Progress in Physical Geography,1982,6(4):475-504.
[58] Edgett K S,Blumberg D G.Star and linear dunes on Mars[J].Icarus,1994,112(2):448-464.
[59] Lee P,Thomas P C.Longitudinal dunes on Mars:Relation to current wind regimes[J].Journal of Geophysical Research:Planets,1995,100(E3):5381-5395.
[60] Bourke M C.A new model for linear dune formation:Merged barchan convoys on Mars[C]//Lunar and Planetary Science Conference,2006:2432.
[61] Gardin E,Allemand P,Quantin C,et al.Dune fields on Mars:Recorders of a climate change?[J].Planetary and Space Science,2012,60(1):314-321.
[62] de Hon R A.Transitional dune forms on Mars[C]// Lunar and Planetary Science Conference,2006:1361.
[63] Lancaster N.The dynamics of star dunes:an example from the Gran Desierto,Mexico[J].Sedimentology,1989,36(2):273-289.
[64] Hedin S.Central Asia and Tibet[M].New York,USA:Charles Scribner and Sons,1903.
[65] Ward A W.Yardangs on mars:evidence of recent wind erosion[J].Journal of Geophysical Research:Solid Earth,1979,84(B14):8147-8166.
[66] Ward A W,Greeley R.Evolution of the yardangs at Rogers Lake,California[J].Geological Society of America Bulletin,1984,95(7):829-837.
[67] McCauley J F,Breed C S,El-Baz F,et al.Pitted and fluted rocks in the western desert of Egypt:Viking comparisons[J].Journal of Geophysical Research:Solid Earth,1979,84(B14):8222-8232.
[68] Greeley R,Arvidson R E,Barlett P W,et al.Gusev crater:Wind-related features and processes observed by the Mars Exploration Rover Spirit[J].Journal of Geophysical Research:Planets,2006,111(E2):JE002491.
[69] Squyres S W,Arvidson R E,Bell J F,et al.The Opportunity Rover's Athena science investigation at Meridiani Planum,Mars[J].Science,2004,306(5702):1698-1703.
[70] Ahlbrandt S.Textural parameters of eolian deposits[M]// McKee E D.A Study of Global Sand Seas.Honolulu,Hawaii,USA:Universitu Press of the Pacific,1979:21-58.
[71] Edgett K S,Christensen P R.The particle size of Martian aeolian dunes[J].Journal of Geophysical Research:Planets,1991,96(E5):22765-22776.
[72] Greeley R,Leach R N,Williams S H,et al.Rate of wind abrasion on Mars[J].Journal of Geophysical Research:Solid Earth,1982,87(B12):10009-10024.
[73] Zimbelman J R.Non-active dunes in the Acheron Fossae Region of Mars between the Viking and Mars Global Surveyor eras[J].Geophysical Research Letters,2000,27(7):1069-1072.
[74] Edgett K S,Malin M C.New views of Mars eolian activity,materials,and surface properties:three vignettes from the Mars Global Surveyor Mars Orbiter Camera[J].Journal of Geophysical Research:Planets,2000,105(E1):1623-1650.
[75] Fenton L K.Dune migration and slip face advancement in the Rabe Crater dune field,Mars[J].Geophysical Research Letters,2006,33(20): GL027133.
[76] Bourke M C,Edgett K S,Cantor B A.Recent aeolian dune change on Mars[J].Geomorphology,2008,94(1):247-255.
[77] Zimbelman J R,Irwin III R P,Williams S H,et al.The rate of granule ripple movement on Earth and Mars[J].Icarus,2009,203(1):71-76.
[78] Schofield J T,Barnes J R,Crisp D,et al.The Mars Pathfinder atmospheric structure investigation/meteorology (ASI/MET) experiment[J].Science,1997,278(5344):1752-1758.
[79] Malin M C,Edgett K S.Mars global surveyor Mars orbiter camera:interplanetary cruise through primary mission[J].Journal of Geophysical Research:Planets,2001,106(E10):23429-23570.
[80] Schatz V,Tsoar H,Edgett K S,et al.Evidence for indurated sand dunes in the Martian north polar region[J].Journal of Geophysical Research:Planets,2006,111(E4):JE002514.
[81] Sullivan R,Arvidson R,Bell J F,et al.Wind-driven particle mobility on Mars:insights from Mars exploration rover observations at "El Dorado" and surroundings at Gusev Crater[J].Journal of Geophysical Research:Planets,2008,113(E6):JE003101.
[82] Bridges N T,Geissler P E,McEwen A S,et al.Windy Mars:A dynamic planet as seen by the HiRISE camera[J].Geophysical Research Letters,2007,34(23):GL031445.
[83] Silvestro S,Fenton L K,Vaz D A,et al.Ripple migration and dune activity on Mars:evidence for dynamic wind processes[J].Geophysical Research Letters,2010,37(20):GL044743.
[84] Chojnacki M,Burr D M,Moersch J E,et al.Orbital observations of contemporary dune activity in Endeavor crater,Meridiani Planum,Mars[J].Journal of Geophysical Research:Planets,2011,116(E7):JE003675.
[85] Bridges N T,Bourke M C,Geissler P E,et al.Planet-wide sand motion on Mars[J].Geology,2012,40(1):31-34.
[86] Greeley R,Kuzmin R O,Haberle R M.Aeolian processes and their effects on understanding the chronology of Mars[J].Space Science Reviews,2001,96(1/4):393-404.
[87] Hayward R K,Titus T N,Michaels T I,et al.Aeolian dunes as ground truth for atmospheric modeling on Mars[J].Journal of Geophysical Research:Planets,2009,114(E11):JE003428.
[88] Fenton L K,Bandfield J L,Ward A.Aeolian processes in proctor crater on Mars:sedimentary history as analyzed from multiple data sets[J].Journal of Geophysical Research:Planets,2003,108(E12):JE002015.
[89] Pollack J B,Haberle R M,Schaeffer J,et al.Simulations of the general circulation of the Martian atmosphere:1.polar processes[J].Journal of Geophysical Research:Solid Earth,1990,95(B2):1447-1473.
[90] Anderson F S,Greeley R,Xu P,et al.Assessing the Martian surface distribution of aeolian sand using a Mars general circulation model[J].Journal of Geophysical Research:Planets,1999,104(E8):18991-19002.
[91] Hayward R K,Fenton L K,Tanaka K L,et al.Aeolian features as ground truth for atmospheric modeling on Mars[J].LPI Contributions,2008,1447:9033.
[92] Greeley R,Skypeck A,Pollack J B.Martian aeolian features and deposits:Comparisons with general circulation model results[J].Journal of Geophysical Research:Planets,1993,98(E2):3183-3196.
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