陕西靖边统万城建城时期地表物质成因与自然环境

doi:10.31497/zrzyxb.20200620

自然资源学报 ›› 2020, Vol. 35 ›› Issue (6): 1499-1510.doi: 10.31497/zrzyxb.20200620

• 其他研究论文 • 上一篇

陕西靖边统万城建城时期地表物质成因与自然环境

黄小刚^{1, 2}, 赵景波^{2, 3}, 马延东², 岳大鹏², 罗小庆²

1. 山西师范大学地理科学学院,临汾 041004;
2. 陕西师范大学地理科学与旅游学院,西安 710119;
3. 中国科学院地球环境研究所气溶胶化学与物理重点实验室,西安 710061

收稿日期:2019-04-11 修回日期:2019-09-02 出版日期:2020-06-28 发布日期:2020-06-28
通讯作者: 赵景波（1953-）, 男, 山东滕州人, 博士, 教授, 博士生导师, 主要从事自然地理与第四纪研究。E-mail:zhaojb@snnu.edu.cn
作者简介:黄小刚（1978-）, 男, 广西桂林人, 博士研究生, 主要从事生态环境评价与治理研究。 E-mail:huangxg@sxnu.edu.cn
基金资助:
国家社会科学基金重大项目（11&ZD097）；中国科学院气溶胶化学与物理重点实验室项目（KLACP1904）

Causes of surface sediments and natural environment of Tongwan city in Jingbian county of Shaanxi province during its construction period

HUANG Xiao-gang^{1, 2}, ZHAO Jing-bo^{2, 3}, MA Yan-dong², YUE Da-peng², LUO Xiao-qing²

1. College of Geographical Sciences, Shanxi Normal University, Linfen 041004, Shanxi, China;
2. School of Geography and Tourism, Shaanxi Normal University, Xi'an 710119, China;
3. Key Laboratory of Aerosol Chemistry and Physics, Institute of Earth Environment, CAS, Xi'an 710061, China

Received:2019-04-11 Revised:2019-09-02 Online:2020-06-28 Published:2020-06-28

摘要/Abstract

摘要： 为查明距今约1600年的统万城建城时期的自然环境和该古城是否建在风沙沉积之上这一长期争议的问题,对6个钻孔剖面样品进行粒度和X-射线衍射等分析。结果表明：城墙内外地表之下均为湖泊沉积,沉积物特点与风沙沉积物显著不同,主要表现为以下五个方面：（1）沙层含有褐黄色针铁矿;（2）有多个深灰色沉积层;（3）沙层中粗砂含量显著大于风积沙层;（4）沙层中粒度成分的分选性比风积沙层明显差;（5）细粒斑点中Fe₂O₃与Al₂O₃含量比风沙沉积物高。本文获得的证据充分表明,在统万城建城前后,该区自然环境较好,普遍分布的是由湖积物组成的高平地,统万城建在湖积沙层之上。统万城建城时期基本没有发生沙漠化,沙漠化发生在建城之后的一定时期。

关键词: 湖泊沉积, 沙漠化, 统万城, 粒度组成, 自然环境

Abstract: In order to figure out the natural environment during the construction period (around 1600 years ago) of Tongwan city and a long-standing controversy of whether the city is built on sand deposits, research is done on six profiles of sample bore holes by grain size analysis, X-Ray diffraction, etc. This study indicates that lacustrine deposits are identified under the surface of ground both inside and outside of the city wall, and their features are totally different from wind deposit. The differences are shown as follows: (1) There is yellowish-brown goethite in targeted sand layers. (2) Several dark gray deposited layers are identified. (3) The content of coarse sand in the targeted sand layers is much higher than that in wind deposits. (4) The grain content showed a mixture of coarse and fine sand with a higher degree of separation. (5) The contents of Fe₂O₃ and A1₂O₃ in fine-sand spots in lacustrine deposits are higher than those in sand deposits. Supported by concrete evidences collected, it is shown that the natural environment of the city was good during the construction period. And the basic landscape is plateau generated owing to the accumulation of lacustrine deposits, on which the ancient city was built. Desertification did not occur during the construction period, but did during a period after its construction.

Key words: content of grain size, desertification, natural environment, lacustrine deposit, Tongwan city

黄小刚, 赵景波, 马延东, 岳大鹏, 罗小庆. 陕西靖边统万城建城时期地表物质成因与自然环境[J]. 自然资源学报, 2020, 35(6): 1499-1510.

HUANG Xiao-gang, ZHAO Jing-bo, MA Yan-dong, YUE Da-peng, LUO Xiao-qing. Causes of surface sediments and natural environment of Tongwan city in Jingbian county of Shaanxi province during its construction period[J]. JOURNAL OF NATURAL RESOURCES, 2020, 35(6): 1499-1510.

参考文献

[1] 董光荣, 李保生, 高尚玉, 等. 鄂尔多斯高原第四纪古风成沙的发现及其意义. 科学通报, 1983, 28(16): 998-1001.
[DONG G R, LI B S, GAO S Y, et al.Significances of the Quaternary ancient eolian sands in the Ordos Plateau. Chinese Science Bulletin, 1983, 28(16): 998-1001.]
[2] SUN J M, DING Z L, LIU T S, et al.580000-year environmental reconstruction from aeolian deposits at the Mu Us Desert margin, China. Quaternary Science Reviews, 1999, 18(12): 1351-1364.
[3] 邓辉, 舒时光, 宋豫秦, 等. 明代以来毛乌素沙地流沙分布南界的变化. 科学通报, 2007, 52(21): 2556-2563.
[DENG H, SHU S G, SONG Y Q, et al.The change of southern border of quicksand in Mu Us Desert since the time of Ming Dynasty. Chinese Science Bulletin, 2007, 52(21): 2556-2563.]
[4] DONG G R, GAO S Y, JIN J, et al.The formation, evolution and cause of the Mu Us Desert in China. Science in China: Series B, 1989, 32(7): 859-872.
[5] ZHOU Y L, LU H Y, ZHANG J F, et al.Luminescence dating of sand-loess sequences and response of Mu Us and Otindag sand fields (North China) to climatic changes. Journal of Quaternary Science, 2009, 24(4): 336-344.
[6] LU H Y, MIAO X D, ZHOU Y L, et al.Late Quaternary aeolian activity in the Mu Us and Otindag dune fields (North China) and lagged response to insolation forcing. Geophysical Research Letters, 2005, 32(21): L21716.
[7] LI B S, JIN H L, LYU H, Y, et al. Processes of the deposition and vicissitude of Mu Us Desert, China since 150 ka BP. Science in China: Series D, 1998, 41(3): 248-254.
[8] HO P.The myth of desertification at China's northwestern frontier: The case of Ningxia, 1929-1958. Modern China, 2000, 26(3): 348-395.
[9] 韩昭庆. 明代毛乌素沙地变迁及其与周边地区垦殖的关系. 中国社会科学, 2003, (5): 191-204.
[HAN Z Q.The evolution of the Maowusu Desert and the reclamation in the adjacent areas in the Ming Dynasty. Social Sciences in China, 2003, (5): 191-204.]
[10] 邓辉, 夏正楷, 王琫瑜. 从统万城的兴废看人类活动对生态环境脆弱地区的影响. 中国历史地理论丛, 2001, 16(2): 104-113.
[DENG H, XIA Z K, WANG B Y.Human activities' influence on the areas of weak ecological environment in terms of the rise and fall of Tongwan city. Collections of Essays on Chinese Historical Geography, 2001, 16(2): 104-113.]
[11] 王乃昂, 黄银洲, 何彤慧, 等. 鄂尔多斯高原古城夯层沙的环境解释. 地理学报, 2006, 61(9): 937-945.
[WANG N A, HUANG Y Z, HE T H, et al.The environmental significance of tamping sandy layer in ancient city ramparts on Erdos Plateau. Acta Geographica Sinica, 2006, 61(9): 937-945.]
[12] 黄银洲, 王乃昂, 何彤慧, 等. 毛乌素沙地历史沙漠化过程与人地关系. 地理科学, 2009, 29(2): 206-211.
[HUANG Y Z, WANG N A, HE T H, et al.Process of historical desertification of Mu Us desert and relationship between nature and human beings. Scientia Geographica Sinica, 2009, 29(2): 206-211.]
[13] 戴应新. 统万城城址勘测记. 考古, 1981, (3): 225-232.
[DAI Y X.Survey on the site of Tongwan city. Archaeology, 1981, (3): 225-232.]
[14] 王尚义, 董靖保. 统万城的兴废与毛乌素沙地之变迁. 地理研究, 2001, 20(3): 347-353.
[WANG S Y, DONG J B.The rise and fall of Tongwan city with the environmental change of Mu Us Sandy Land. Geographical Research, 2001, 20(3): 347-353.]
[15] 侯仁之. 从红柳河上的古城废墟看毛乌素沙漠的变迁. 文物, 1973, (1): 35-41.
[HOU R Z.A research on the changes of the Maowusu Desert through the ruins of ancient towns in Hongliu River valley. Cultural Relics, 1973, (1): 35-41.]
[16] 史念海. 两千三百年来鄂尔多斯高原和河套平原农林牧地区的分布及其变迁. 北京师范大学学报: 社会科学版, 1980, (6): 1-14.
[SHI N H.Distribution and changes of the farming, forestry and animal husbandry area in Ordos Plateau and Hetao Plain during the past 2300 years. Journal of Beijing Normal University: Social Sciences, 1980, (6): 1-14.]
[17] 李恩菊, 谢春林. 统万城废弃的原因分析. 中国沙漠, 2010, 30(5): 1047-1052.
[LI E J, XIE C L.Discuss on causes of abandonment of Tongwan city in south of Mu Us Sand Land. Journal of Desert Research, 2010, 30(5): 1047-1052.]
[18] 杨屹, 胡蝶. 生态脆弱区榆林三维生态足迹动态变化及其驱动因素. 自然资源学报, 2018, 33(7): 1204-1217.
[YANG Y, HU D.Dynamic changes and driving factors of three dimensional ecological footprint in Yulin. Journal of Natural Resources, 2018, 33(7): 1204-1217.]
[19] 榆林市编纂委员会. 榆林市志. 西安: 三秦出版社, 1996: 85-116.
[Yulin City Codification Committee. Yulin City Annals. Xi'an: Sanqin Press, 1996: 85-116.]
[20] 赵景波, 张冲, 董治宝, 等. 巴丹吉林沙漠高大沙山粒度成分与沙山形成. 地质学报, 2011, 85(8): 1389-1398.
[ZHAO J B, ZHANG C, DONG Z B, et al.Particle size composition and formation of the mega-dune in the Badain Jaran Desert. Acta Geologica Sinica, 2011, 85(8): 1389-1398.]
[21] 哈斯, 王贵勇. 腾格里沙漠东南缘横向沙丘粒度变化及其与坡面形态的关系. 中国沙漠, 1996, 16(2): 216-221.
[HA S, WANG G Y.Grain-size variation on transverse dune in connection with slope morphology at southeastern fringe of Tengger Desert. Journal of Desert Research, 1996, 16(2): 216-221.]
[22] 李智佩, 岳乐平, 薛祥煦, 等. 毛乌素沙地沉积物粒度特征与土地沙漠化. 吉林大学学报: 地球科学版, 2007, 37(3): 578-586.
[LI Z P, YUE L P, XUE X X, et al.Grain-size distribution characteristics of different geo-genetic type sediments and land desertification in Mo Us Desert. Journal of Jilin University: Earth Science Edition, 2007, 37(3): 578-586.]
[23] 黄银洲, 王乃昂, 冯起, 等. 统万城筑城的环境背景: 河流、湖泊及沙漠化程度. 中国沙漠, 2012, 32(5): 1233-1239.
[HUANG Y Z, WANG N A, FENG Q, et al.Environmental background of building the Tongwancity: Rivers, lakes and desertification degree. Journal of Desert Research, 2012, 32(5): 1233-1239.]
[24] 苏春田, 唐健生, 单海平, 等. 黎塘岩溶区土壤铁锰结核的地球化学特征研究. 中国岩溶, 2008, 27(1): 43-49.
[SU C T, TANG J S, SHAN H P, et al.Study on the geochemical properties of Fe-Mn nodule in Litang karst area. Carsologica Sinica, 2008, 27(1): 43-49.]
[25] ZHAO J B, MA Y D, LUI R, et al.Palaeoclimatic and hydrological environments inferred by moisture indexes from the S₄ palaeosol section in the Xi'an region, China. Quaternary International, 2018, 493: 127-136.
[26] 钱亦兵, 吴兆宁, 石井武政, 等. 塔克拉玛干沙漠沙物质成分特征及其来源. 中国沙漠, 1993, 13(4): 32-38.
[QIAN Y B, WU Z N, ISHII T, et al.The constituent cheracteristics of sand materials and sand sources of the Taklamakan Desert. Journal of Desert Research, 1993, 13(4): 32-38.]
[27] 张宝政, 陈琦. 地质学原理. 北京: 地质出版社, 1983: 156-159.
[ZHANG B Z, CHEN Q.Principles of Geology. Beijing: Geological Publishing House, 1983: 156-159.]
[28] 艾冲. 论毛乌素沙漠形成与唐代六胡州土地利用的关系. 陕西师范大学学报: 哲学社会科学版, 2004, 33(3): 99-105.
[AI C.The relationship between the shaping of the Maowusu Desert and utility of land in the Six Barbarous States in the Tang Dynasty. Journal of Shaanxi Normal University: Philosophy and Social Sciences Edition, 2004, 33(3): 99-105.]
[29] 李保生, 董光荣, 高尚玉, 等. 陕西北部榆林第四纪地层剖面的粒度分析与讨论. 地理学报, 1988, 43(2): 127-133.
[LI B S, DONG G R, GAO S Y, et al.Analysis and discussion on the grain size of the Quaternary Strata profile in Yulin area of the Northern, Shaanxi. Acta Geographica Sinica, 1988, 43(2): 127-133.]
[30] 孙继敏, 刘东生, 丁仲礼, 等. 五十万年来毛乌素沙漠的变迁. 第四纪研究, 1996, 16(4): 359-367.
[SUN J M, LIU D S, DING Z L, et al.The Mu Us Desert evolution in the last 0.5 Ma. Quaternary Sciences, 1996, 16(4): 359-367.]
[31] 郭兵, 孔维华, 姜琳. 西北干旱荒漠生态区脆弱性动态监测及驱动因子定量分析. 自然资源学报, 2018, 33(3): 412-424.
[GUO B, KONG W H, JIANG L.Dynamic monitoring of ecological vulnerability in arid desert ecological region of Northwest China and the quantitative analysis of its driving forces. Journal of Natural Resources, 2018, 33(3): 412-424.]
[32] 李文龙, 石育中, 鲁大铭, 等. 北方农牧交错带干旱脆弱性时空格局演变. 自然资源学报, 2018, 33(9): 1599-1612.
[LI W L, SHI Y Z, LU D M, et al.The spatio-temporal evolution of drought vulnerability in the ecotone between agriculture and animal husbandry in the north of China. Journal of Natural Resources, 2018, 33(9): 1599-1612.]

陕西靖边统万城建城时期地表物质成因与自然环境

Causes of surface sediments and natural environment of Tongwan city in Jingbian county of Shaanxi province during its construction period

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