Institute of Geomechanics, Chinese Academy of Geological SciencesHost
Advanced Search
Previous Article Next Article
2018 Vol. 24, No. 4
Article Contents
Article navigation > Journal of Geomechanics > 2018 > 24(4): 505-514
Next Article Previous Article

Ting HUANG, Zhenhong LI, Feng LIU, Jiawei CUI, Xiaopeng DONG, Yang ZHAO. THE CURRENT SITUATION OF DESERTIFICATION IN THE HONGSIBU BASIN, NINGXIA, AND ITS MAIN GEOLOGICAL CONTROLLING FACTORS[J]. Journal of Geomechanics, 2018, 24(4): 505-514. doi: 10.12090/j.issn.1006-6616.2018.24.04.053
Citation: Ting HUANG, Zhenhong LI, Feng LIU, Jiawei CUI, Xiaopeng DONG, Yang ZHAO. THE CURRENT SITUATION OF DESERTIFICATION IN THE HONGSIBU BASIN, NINGXIA, AND ITS MAIN GEOLOGICAL CONTROLLING FACTORS[J]. Journal of Geomechanics, 2018, 24(4): 505-514. doi: 10.12090/j.issn.1006-6616.2018.24.04.053
shu

THE CURRENT SITUATION OF DESERTIFICATION IN THE HONGSIBU BASIN, NINGXIA, AND ITS MAIN GEOLOGICAL CONTROLLING FACTORS

  • 1.

    School of Earth Sciences and Resources, China University of Geoscience, Beijing 100083, China

  • 2.

    Institute of Geomechanics, Chinese Academy of Geological Science, Beijing 100081, China

More Information
Received Date:  07 February 2018
Revised Date:  01 May 2018
    Abstract
  • Based on the landsand-TM remote sensing images, the desertification evolution history of the Hongsibu Basin in the last 30 years is rebuilt. Combining with the 1:50000 geological mapping, the Late Pleistocene sedimentary frame is systematically built and the lithofacies paleogeography for several important evolutional phases of the Hongsibu Basin is reconstructed. Moreover, the provenance of the eolian sand by detailed geological field and sedimentary geochemical works is traced. According to the primary research, several cognitions can be suggested that Although the desertification had not been eliminated, the ecological migration strategy implemented in 1999 effectively curbed the deterioration of the ecological environment and the range of desertification decreased; The sand ridges at the surface with zonal distribution characteristics mainly extend in NW-SE direction which parallels with the strike of the Daluo Mountain-Niushou Mountain tectonic belts, and Yantong Mountain tectonic belts; The eolian sand piled during the desertification mainly derived from the loosened lacustrine sand deposits, the third part of the Upper Pleistocene Salawusu formation sedimented during the regression, and this process is characterized with in-situ desertification; The similarities of the eolian sand at the surface and the lacustrine sand from the third part of the Salawusu formation in major elements, trace elements, and REE aspects revealed the affinity between these two sets of sands. What's more, this study contributes a lot to the comprehensive control for the regional desertification in the Hongsibu Basin, Ningxia.
    • FullText(HTML)
  • 加载中
    • References
  • Dregne H. Desertification-present and future[J]. International Journal for Development Technology, 1984, (2):255~259.

    Google Scholar

    CCICCD. China country paper to combat desertification[M]. Beijing:China Forestry Publishing House, 1996, 18~31.

    Google Scholar

    Lamb H F, Gasse F, Benkaddour A, et al. Relation between century-scale Holocene arid intervals in tropical and temperate zones[J]. Nature, 1995, 373(6510):134~137. doi: 10.1038/373134a0

    CrossRef Google Scholar

    Geist H J, Lambin E F. Dynamic causal patterns of desertification[J]. BioScience, 2004, 54(9):817~829. doi: 10.1641/0006-3568(2004)054[0817:DCPOD]2.0.CO;2

    CrossRef Google Scholar

    He Z, Zhou J, Yang L H, et al. Holocene dune mobility and forcing mechanisms at the northern margin of the East Asian Monsoon[J]. Acta Geologica Sinica, 2013, 87(4):1168~1178. doi: 10.1111/acgs.2013.87.issue-4

    CrossRef Google Scholar

    Si Y J, Li B S, Zhang D D, et al. Climate fluctuation on a kiloyear scale during the late last glacial in Mu Us Desert, China:Evidence from Rb and Sr contents and ratios[J]. Environmental Earth Sciences, 2014, 72(11):4521~4530. doi: 10.1007/s12665-014-3352-0

    CrossRef Google Scholar

    Cao S X, Chen L, Xu C G, et al. Impact of three soil types on afforestation in China's Loess Plateau:Growth and survival of six tree species and their effects on soil properties[J]. Landscape and Urban Planning, 2007, 83(2~3):208~217.

    Google Scholar

    Bennett D E, Gosnell H, Lurie S, et al. Utility engagement with payments for watershed services in the United States[J]. Ecosystem Services, 2014, 8:56~64. doi: 10.1016/j.ecoser.2014.02.001

    CrossRef Google Scholar

    Bartczak A, Metelska-Szaniawska K. Should we pay, and to whom, for biodiversity enhancement in private forests? An empirical study of attitudes towards payments for forest ecosystem services in Poland[J]. Land Use Policy, 2015, 48:261~269. doi: 10.1016/j.landusepol.2015.05.027

    CrossRef Google Scholar

    Li D J, Xu D Y, Wang Z Y, et al. Ecological compensation for desertification control:a review[J]. Journal of Geographical Sciences, 2018, 28(3):367~384. doi: 10.1007/s11442-018-1478-9

    CrossRef Google Scholar

    刘丹丹, 马俊海.土地利用现状更新调查中荒漠化地区绿地信息提取的方法研究[J].测绘工程, 2007, 16(2):33~35, 42.

    Google Scholar

    LIU Dandan, MA Junmei. Research in the method of extracting vegetation information from the desertification area in land use renewal surveying[J]. Engineering of Surveying and Mapping, 2007, 16(2):33~35, 42. (in Chinese with English abstract

    Google Scholar

    徐驰, 姜琦刚, 李远华, 等.呼伦贝尔地区土地荒漠化动态变化[J].世界地质, 2010, 29(1):160~167.

    Google Scholar

    XU Chi, JIANG Qigang, LI Yuanhua, et al. Dynamic change of desertification in Hulunbeier[J]. Global Geology, 2010, 29(1):160~167. (in Chinese with English abstract)

    Google Scholar

    崔瀚文, 姜琦刚, 邢宇, 等. 32 a来气候扰动下中国沙质荒漠化动态变化[J].吉林大学学报(地球科学版), 2013, 43(2):582~591.

    Google Scholar

    CUI Hanwen, JIANG Qigang, XING Yu, et al. Dynamics of sandy desertification under climate disturbance in China from 1975 to 2007[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(2):582~591. (in Chinese with English abstract)

    Google Scholar

    林年丰, 汤洁.第四纪环境演变与中国北方的荒漠化[J].吉林大学学报(地球科学版), 2003, 33(2):183~191.

    Google Scholar

    LIN Nianfeng, TANG Jie. Quaternary environmental evolution and desertification in North China[J]. Journal of Jilin University (Earth Science Edition), 2003, 33(2):183~191. (in Chinese with English abstract)

    Google Scholar

    张龙生, 马立鹏.黄河上游玛曲县土地沙漠化研究[J].中国沙漠, 2001, 21(1):8~87.

    Google Scholar

    ZHANG Longsheng, MA Lipeng. Study on desertification in Maqu County, upstream of Huanghe River[J]. Journal of Desert Research, 2001, 21(1):84~87. (in Chinese with English abstract)

    Google Scholar

    黄桂华, 黄立峰.生态移民地区跨越式发展的思考——以宁夏吴忠市红寺堡区为例[J].贵州民族研究, 2010, 31(2):101~105.

    Google Scholar

    HUANG Guihua, HUANG Lifeng. Ecology immigration area leap frog development ponder——take the Ningxia Wuzhong Hongsibao area as the example[J]. Guizhou Ethnic Studies, 2010, 31(2):101~105. (in Chinese with English abstract)

    Google Scholar

    郭慧秀, 贾科利.基于GIS的生态脆弱移民区土地资源承载力评价——以红寺堡区为例[J].宁夏工程技术, 2015, 14(4):375~379.

    Google Scholar

    GUO Huixiu, JIA Keli. Bearing capacity of land resources evaluation on GIS in the ecological fragile area:Take Hongsibu as an example[J]. Ningxia Engineering Technology, 2015, 14(4):375~379. (in Chinese with English abstract)

    Google Scholar

    李保生, 靳鹤龄, 祝一志, 等.萨拉乌苏河流域第四系岩石地层及其时间界限[J].沉积学报, 2004, 22(4):676~682.

    Google Scholar

    LI Baosheng, JIN Heling, ZHU Yizhi, et al. The quaternary Lithostrata in Salawusu river valley and their geochronology[J]. Acta Sedimentologica Sinica, 2004, 22(4):676~682. (in Chinese with English abstract)

    Google Scholar

    靳鹤龄, 李明启, 苏志珠, 等. 220 ka以来萨拉乌苏河流域地层磁化率与气候变化[J].中国沙漠, 2006, 26(5):680~686.

    Google Scholar

    JIN Heling, LI Mingqi, SU Zhizhu, et al. Climatic change reflected by stratigraphical magnetic susceptibility in Salawusu river basin, north China since 220 ka BP[J]. Journal of Desert Research, 2006, 26(5):680~686. (in Chinese with English abstract)

    Google Scholar

    靳鹤龄, 李明启, 苏志珠, 等.萨拉乌苏河流域地层沉积时代及其反映的气候变化[J].地质学报, 2007, 81(3):307~315.

    Google Scholar

    JIN Heling, LI Mingqi, SU Zhizhu, et al. Sedimentary age of strata in the Salawusu river basin and climatic changing[J]. Acta Geologica Sinica, 2007, 81(3):307~315. (in Chinese with English abstract

    Google Scholar

    姚檀栋, THOMPSON L G, 施雅风, 等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科学(D辑), 1997, 27(5):447~452.

    Google Scholar

    YAO Tandong, THOMPSON L G, SHI Yafeng, et al. Climate variation since the last interglaciation recorded in the Guliya ice core[J]. Science in China Series D:Earth Sciences, 1997, 40(6):662~668.

    Google Scholar

    周青硕, 张绪教, 叶培盛, 等.河套地区全新世黄河古河道的分布及期次划分[J].地质力学学报, 2017, 23(3):339~347.

    Google Scholar

    ZHOU Qingshuo, ZHANG Xujiao, YE Peisheng, et al. The Distribution and period division of Holocene Palaeo channels of the Yellow River in Hetao area[J]. Journal of Geomechanics, 2017, 23(3):339~347. (in Chinese with English abstract

    Google Scholar

    陈兴强, 施炜, 胡健民, 等.华北临汾盆地中部柴庄上新世-更新世剖面沉积学特征及其构造意义[J].地质力学学报, 2016, 22(4):984~993.

    Google Scholar

    CHEN Xingqiang, SHI Wei, HU Jianmin, et al. Sedimentation of the Pliocene-Pleistocene Chaizhuang section in the central of Linfen Basin, North China and its tectonic significance[J]. Journal of Geomechanics, 2016, 22(4):984~993. (in Chinese with English abstract)

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(7)

Tables(1)

Export Citation
PDF
XML

Article Metrics

Article views(1685) PDF downloads(88) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020