• The Core Journal of China
  • Included in Chinese Scientific and Technical Papers and Citations Database
  • Included in Chinese Science Citation Database (CSCD)
  • Included in Chemical Abstracts (CA)
  • Included in Scopus
Advanced Search
WANG Jian-feng, LEI Tian-zhu, ZHANG Sheng-yin, ZHANG Xi-long, CHEN Wenlei, FAN Hai-long. Trace element geochemistry of the surface sediments in the Liujiaxia Reservoir,Gansu[J]. Sedimentary Geology and Tethyan Geology, 2018, 38(3): 51-59.
Citation: WANG Jian-feng, LEI Tian-zhu, ZHANG Sheng-yin, ZHANG Xi-long, CHEN Wenlei, FAN Hai-long. Trace element geochemistry of the surface sediments in the Liujiaxia Reservoir,Gansu[J]. Sedimentary Geology and Tethyan Geology, 2018, 38(3): 51-59.

Trace element geochemistry of the surface sediments in the Liujiaxia Reservoir,Gansu

More Information
  • Received Date: February 27, 2017
  • Revised Date: June 24, 2017
  • Published Date: September 29, 2018
  • The concentration,correlation,spatial distribution,controlling factor and source of 25 trace elements in the surface sediments from the Liujiaxia Reservoir,Gansu are analyzed by using the multivariate statistical method. The mean contents of the elements Sr,Zn,Zr and Ba are higher than 170 μg/g,while the values of the elements Cd,Mo and Tl are lower than 1 μg/g in the surface sediments from the Liujiaxia Reservoir. The values of other analyzed elements lie within the range of 2.01-104.34 μg/g. Evident correlation and similar distribution exist among the elements Cu,V,Co,Cr,Ni,Rb,Li,Cd,Be,Pb,Sc,As,Ga,Nb,Sn,Cs,Tl,Th and Al2O3. Factor analysis shows that the trace elements in the Liujiaxia Reservoir are divided into three main sources in the following. The distribution of the first component elements is controlled by the weathering and erosion of the natural minerals and rocks,and their contribution rate is 63.20%. The Zr and Ba distribution of the second component elements are mainly affected by the migration and transformation of the elements in the fluvial sediments,and their contribution rate is 12.51%. The Sr distribution of the third component elements is mainly controlled by the biogenic origin,and their contribution rate is 9.76%. In addition,the contents of the elements Zn and As in the heavy metallic elements in the study area are much higher than the average values of the global shales,which is worth further study in the future.
  • Related Articles

    [1]CHEN Huan, FENG Xiaoliang, LIU Yimin, ZHAO Han, LIU Yang, GUO Lang, ZHANG Jun. Research on predicting surface displacement of landslides based on CNN-BiLSTM-Attention in the Three Gorges reservoir area[J]. Sedimentary Geology and Tethyan Geology, 2024, 44(3): 572-581. DOI: 10.19826/j.cnki.1009-3850.2024.08006
    [2]Jiang Qibao, Wei Jin, Ouyang Yongpeng, Rao Jianfeng, Li Yanping, Zhang Xuehui. Geochemistry of stream sediments and its implication for ore-finding, Dayoushan, Jiangxi Province[J]. Sedimentary Geology and Tethyan Geology, 2021, 41(1): 73-81. DOI: 10.19826/j.cnki.1009-3850.2020.10004
    [3]Liu Xiang, Guo Jianming, Fan Hailong, Zhang Shengyin, Zhang Shuncun, Lei Tianzhu, Wang Jianfeng. Evaluation of Heavy Metal Pollution in Surface Sediments of Southwest Liujiaxia Reservoir, Gansu[J]. Sedimentary Geology and Tethyan Geology, 2020, 40(4): 1-10. DOI: 10.19826/j.cnki.1009-3850.2020.08003
    [4]TIAN Bo, WANG Wei-feng, ZOU Juan. The reservoir spaces and influencing factors of the volcanic reservoirs[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(4): 86-94.
    [5]CHEN Rong, Wang Feng, Tian Jingchun. Provenance analysis and reservoirs characteristics of the clastic rocks from the Yangchang Formation in west-central Ordos Basin[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(1): 21-26.
    [6]CHEN Lan, YIN Hai-sheng, SHI Zhi-qiang. The Jurassic sediments and their depositional environments in the Yanshiping region of the Qiangtang Basin, northern Xizang[J]. Sedimentary Geology and Tethyan Geology, 2002, 22(3): 80-84.
    [7]Yan Jiaping, Wang Zhenwei. SEDIMENTARY CHARACTERISTICS AND PALAEOGEOGRAPHIC SIGNIFICANCE OF THE LOOSE SEDIMENTS AT THE LOWERMOST PART OF THE CENOZOIC STRATA IN THE SOUTHERN HUAIBEI COALFIELD[J]. Sedimentary Geology and Tethyan Geology, 1997, 17(2): 47-52.
    [8]Wang Longzhang. SEDIMENT FLUX AND MECHANISM FOR THE UPLIFTING OF THE MOUNTAIN SYSTEM AROUND THE JUNGGAR INLAND BASIN[J]. Sedimentary Geology and Tethyan Geology, 1996, 16(3): 39-46.
    [9]Ai Huaguo, Wang Huamin, Liu Lanlan. SEDIMENTATION, DIAGENESIS AND RESERVOIR CHARACTERISTICS OF THE UPPER CARBONIFEROUS CARBONATE ROCKS IN THE MIDDLE YANGTZE AREA[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(4): 28-37.
    [10]G. Einsele, S. Dürr, W. Frisch, Liu Guanghua, H. P. Luterbacher, L. Ratschbacher, W. Ricken, J. Weridt, A. Wetzel, Liu Baojun, Yu Guangming, Zheng Haixiang. THE XIGAZE FOREARC BASIN (CRETACEOUS, TIBET): SEDIMENTS AND BASIN EVOLUTION[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(1): 3-31,56.

Catalog

    Article views (67) PDF downloads (83) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return