Composition and Micro-morphological Characteristics of Aeolian Sand in the Middle of the Mu Us Sandy Land

Chen Guoxiang; Dong Zhibao; Cui Xujia; Xiao Weiqiang; Li Lulu; Yang Junhuai; Shi Weikang

doi:10.7522/j.issn.1000-694X.2017.00066

Journal of Desert Research >

2018 , Vol. 38 >Issue 3: 473 - 483

DOI: https://doi.org/10.7522/j.issn.1000-694X.2017.00066

Composition and Micro-morphological Characteristics of Aeolian Sand in the Middle of the Mu Us Sandy Land

Chen Guoxiang ,
Dong Zhibao ,
Cui Xujia ,
Xiao Weiqiang ,
Li Lulu ,
Yang Junhuai ,
Shi Weikang

Expand

1. School of Geography and Tourism, Shaanxi Normal University, Xi'an 710062, China;
2. National Demonstration Center for Experimental Geography Education, Shaanxi Normal University, Xi'an 710062, China;
3. Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China

Received date: 2017-08-11

Revised date: 2017-08-29

Online published: 2018-11-06

Fold

Abstract

In this paper, the grain size, element and micro-morphological characteristics of mobile dune and fixed/semi-fixed dune in the middle of the Mu Us Sandy Land are analyzed. The results show that both the mobile dune and the fixed/semi-fixed dune are composed of fine sand and medium sand, while the sorting of mobile dune is better, and the sorting of fixed/semi-fixed dune is poor. The transport style of dunes is saltation in a frequent and strong wind activity environment, and the way of transportation is fixed and the power of transportation is stable. Compared with UCC, SiO₂ and Na₂O are rich in major elements, others are loss, and Co is enriched obviously for trace element. Values of CIA of dunes are close to the average of the upper continental crust, indicating that the dune has experienced a low degree of chemical weathering. The roundness of mobile dune and fixed/semi-fixed dune is poor, and most of them are angular shape or sub-angular shape, and the real round shape is less; The typical mark of the windy environment is dish-shaped pits accounted for a large proportion, and it is inferred that the climate of the Mu Us Sandy Land is relatively dry, the mechanical action occupies a dominant position while the chemical weathering plays a small role.

Key words： micro-morphology; sediment; grain size; geochemical elements; Mu Us Sandy Land

Cite this article

Chen Guoxiang , Dong Zhibao , Cui Xujia , Xiao Weiqiang , Li Lulu , Yang Junhuai , Shi Weikang . Composition and Micro-morphological Characteristics of Aeolian Sand in the Middle of the Mu Us Sandy Land[J]. Journal of Desert Research, 2018 , 38(3) : 473 -483 . DOI: 10.7522/j.issn.1000-694X.2017.00066

References

[1] 朱震达,吴正,刘恕,等.中国沙漠概论[M].北京:科学出版社,1980.
[2] 吴正,等.风沙地貌与治沙工程学[M].北京:科学出版社,2003.
[3] Livingstone I.Grain-size variation on a ‘complex’ linear dune in Namib Desert[C]//Frostick L E,Reid I.Desert Sediments:Ancient and Modern.Oxford,UK:Blackwell,1987:281-291.
[4] Wang X M,Dong Z B,Zhang J W,et al.Grain size characteristics of dune sands in the central Taklimakan Sand Sea[J].Sedimentary Geology,2003,161:1-14.
[5] Friedman G.Distinction between dune,beach,and river sands from their textural characteristics[J].Journal of Sedimentary Petrology,1961,31:514-529.
[6] Ahlbrandt T S.Textural parameters of eolian deposites[C]//McKee E.A Study of Global Sand Seas.Washington,USA,1979:21-51.
[7] Visher G S.Grain-size distributions and depositional processes[J].Journal of Sedimentary Petrology,1969,39(3):1074-1106.
[8] 龙黎,董玉祥,孙忠.海岸沙丘表面现代风成沙地球化学元素分异的典型研究——以河北昌黎黄金海岸横向沙脊为例[J].沉积学报,2012,30(4):724-730.
[9] 陈丽华,等.扫描电镜在石油地质上的应用[M].北京:石油工业出版社,1990:51-57.
[10] 戴枫年.石英砂粒表面微结构特征的研究[J].中国沙漠,1986,6(3):20-23.
[11] Krinsley D H,Doornkamp J C.Atlas of quartz sand surface textures[M].New York,USA:Cambridge University Press,1973:5-102.
[12] 谢又予,崔之久,李洪云,等.中国石英砂表面结构特征图谱[M].北京:海洋出版社,1984.
[13] 孙有斌,安芷生.风尘堆积物中石英颗粒表面结构特征及其沉积学指示[J].沉积学报,2000,18(4):506-510.
[14] 黄杏珍,潘中海.应用粒度资料探讨毛乌素沙漠西南部的风沙特征[J].地理学报,1981,36(1):70-78.
[15] 曹红霞,张云翔,岳乐平,等.毛乌素沙地全新世地层粒度组成特征及古气候意义[J].沉积学报,2003,21(3):482-486.
[16] 李智佩,岳乐平,薛祥煦,等.毛乌素沙地东南部边缘不同地质成因类型土地沙漠化粒度特征及其地质意义[J].沉积学报,2006,24(2):267-275.
[17] 隆浩,王乃昂,李煜育,等.毛乌素沙地北缘泊江海子剖面粒度特征及环境意义[J].中国沙漠,2007,27(2):197-193.
[18] 刘海霞,李晋昌,苏志珠,等.毛乌素沙地西南缘灌丛沙丘沉积物的粒度和元素特征[J].中国沙漠,2015,35(1):27-28.
[19] 舒培仙,牛东风,李保生,等.毛乌素沙地现代沙丘沙的粒度特征及其意义[J].中国沙漠,2016,36(1):158-166.
[20] 陈渭南,高尚玉,孙忠.毛乌素沙地全新世地层化学元素特点及其古气候意义[J].中国沙漠,1994,3(1):22-30.
[21] 陈渭南,宋锦熙,高尚玉.从沉积重矿物与土壤养分特点看毛乌素沙地全新世环境变迁[J].中国沙漠,1994,14(3):1-9.
[22] 苏志珠,董光荣,李小强,等.晚冰期以来毛乌素沙漠环境特征的湖沼相沉积记录[J].中国沙漠,1999,19(2):104-109.
[23] 吴利杰,石建省,郭娇,等.沙漠/黄土过渡带杨桥畔全新世地层微量元素特征及其所揭示的古气候变化[J].矿物岩石地球化学通报,2015,34(2):323-329.
[24] 谢又予,崔之久.电子扫描镜下我国若干冰碛石英砂的表面特征[J].冰川冻土,1981,3(2):52-55.
[25] 谢又予,崔之久,李洪云.扫描电镜下石英砂的表面结构特征及其地质解译[J].石油与天然气地质,1981,2(1):66-74.
[26] 王颖,迪纳瑞尔B.石英砂表面结构模式图集[M].北京:科学出版社,1985.
[27] 克林斯雷D H,杜尔坎普J C.石英颗粒表面结构图册[M].陈瑞君,译.石油工业出版社,1980:1-149.
[28] 任明达,缪昕.石英砂表面的微结构-种沉积环境标志[J].地质评论,1984,30(1):36-41.
[29] 吴正.我国内陆沙漠与海岸沙丘石英颗粒表面结构的对比研究[J].中国沙漠,1995,15(3):201-206.
[30] 陈秀英,李萍,李从先.我国南北方海岸风成沙丘石英颗粒表面结构的对比研究[J].海洋科学,1987(5):20-22.
[31] 戴枫年.我国北方沙漠地区沙丘石英砂的表面特征与沉积环境的关系[J].干旱区资源与环境,1988,2(2):25-35.
[32] 吴正.中国沙漠及其治理[M].北京:科学出版社,2009.
[33] 成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1978.
[34] 任明达,王乃梁.现代沉积环境概论[M].北京:科学出版社,1985:8-9,14-16.
[35] Folk P L,Ward W D.Brazos reviver bar:a study in the significance of grain size parameters[J].Journal of Sedimentary Petrology,1957,27(1):3-26.
[36] 董治宝,苏志珠,钱广强,等.库姆塔格沙漠风沙地貌[M].北京:科学出版社,2011.
[37] Lancaster N.Grain size characteristics of Namib Desert linear dunes[J].Sedimentology,1981,28(1):115-122.
[38] 郑海飞,郝瑞霞.普通地球化学[M].北京:北京大学出版社,2007:147-149.
[39] Nesbitt H W,Yong G M.Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J].Geochimica et Cosmochimica Acta,1984,48(7):1523-1534.
[40] 冯连君,储雪蕾,张启锐,等.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,2003,10(4):539-544.
[41] 罗万银,董治宝,钱广强,等.戈壁表层沉积物地球化学元素组成及其沉积意义[J].中国沙漠,2014,34(6):1-13.
[42] Nesbitt H W,Yong G M.Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J].Nature,1982,229:715-717.
[43] Nesbitt,Yong G M.Formation and diagenesis of weathering profiles[J].The Journal of Geology,1989,97:129-147.
[44] 董治宝,苏志珠,钱广强,等.库姆塔格沙漠风沙地貌[M].北京:科学出版社,2011:116-117.
[45] 崔徐甲,孙虎,董治宝,等.巴丹吉林沙漠高大沙山沉积物地球化学元素组成及其环境意义[J].中国沙漠,2017,37(1):17-25.
[46] Mahaney W C,Dirszowsky R W,Milner M W,et al.Quartz microtextures and microstructures owing to deformation of glaciolacustrine sediments in the northern Venezuelan Andes[J].Journal of Quaternary Science,2004,19(1):23-33.
[47] Cardona J P M,Gutiecrrez Mas J M,Bellocn A S,et al.Surface textures of heavy-mineral grains:a new contribution to provenance studies[J].Sedimentary Geology,2005,174:223-235.
[48] Strand K,Psaachier S,Nasi J.Implications of quartz grain microtextures for onset Eocene/Oligocene glaciation in Prydz Bay,ODP Site 1166,Autarctica[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2003,198:101-111.

Options

Outlines

模态框（Modal）标题

Abstract

Cite this article

References