ZHAO Debo, WAN Shiming, SHEN Xingyan, YU Zhaojie, JIAO Dongfeng. A DISCUSSION ON METHODOLOGY TO EXTRACT CLAY MINERALS FROM MARINE SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 173-181. DOI: 10.16562/j.cnki.0256-1492.2015.05.020
Citation: ZHAO Debo, WAN Shiming, SHEN Xingyan, YU Zhaojie, JIAO Dongfeng. A DISCUSSION ON METHODOLOGY TO EXTRACT CLAY MINERALS FROM MARINE SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 173-181. DOI: 10.16562/j.cnki.0256-1492.2015.05.020

A DISCUSSION ON METHODOLOGY TO EXTRACT CLAY MINERALS FROM MARINE SEDIMENTS

More Information
  • Received Date: September 27, 2014
  • Revised Date: November 24, 2014
  • Clay minerals, as the most important components of terrigenous fine-grained clastic sediments, play a significant role in the research of sediment sources, oceanic currents, and paleoenvironmental evolution. Therefore, how to extract clay minerals correctly and efficiently from the sediments becomes a prerequisite for further research. In this study we presented two methods i.e. the gravity settling and centrifuged settling respectively to extract clay minerals from marine sediment samples. The two sets of results, compared each other by statistical analysis, show a positive correlation rather than significant difference. Downcore variation of clay mineral assemblages estimated by the two different methods for both ODP Site 1146 and core ZK001 has a very similar overall trend. The diffraction patterns of a clay-sized powder sample obtained by the two extract methods show a similar trend, dominated by clay minerals. Moreover, grain size measurements show that samples obtained by the two extract methods are all in the range of <2 μm. Thus we conclude that the centrifuged settling method can also accurately obtain important information about clay minerals, and is more efficient than traditional gravity settling method to extract clay minerals. Therefore, it is appropriate to promote centrifuged settling method in research of clay minerals in marine sediments.
  • [1]
    Biscaye P E. Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans[J]. Geological Society of America Bulletin, 1965, 76(7):803-812.
    [2]
    Carroll D. Clay minerals in Arctic Ocean sea-floor sediments[J]. Journal of Sedimentary Research, 1970, 40(3):814-821.
    [3]
    Kolla V, Kostecki J, Robinson F, et al. Distributions and origins of clay minerals and quartz in surface sediments of the Arabian Sea[J]. Journal of Sedimentary Research, 1981, 51(2):563-569.
    [4]
    李国刚. 中国近海表层沉积物中黏土矿物的组成、分布及其地质意义[J]. 海洋学报, 1990, 12(4):470-479.

    [LI Guogang. The composition of clay minerals in surface sediments of China offshore[J]. Acta Oceanologica Sinica, 1990, 12(4):470-479.]
    [5]
    Petschick R, Kuhn G, Gingele F. Clay mineral distribution in surface sediments of the South Atlantic:sources, transport, and relation to oceanography[J]. Marine Geology, 1996, 130(3):203-229.
    [6]
    Liu Z F, Trentesaux A, Clemens S C, et al. Clay mineral assemblages in the northern South China Sea:implications for East Asian monsoon evolution over the past 2 million years[J]. Marine Geology, 2003, 201(1):133-146.
    [7]
    Wan S M, Li A C, Clift P D, et al. Development of the East Asian monsoon:mineralogical and sedimentologic records in the northern South China Sea since 20 Ma[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 254(3):561-582.
    [8]
    靳宁, 李安春, 刘海志,等. 帕里西维拉海盆西北部表层沉积物中黏土矿物的分布特征及物源分析[J]. 海洋与湖沼, 2007, 38(6):504-511.

    [JIN Ning, LI Anchun, LIU Haizhi, et al. Clay minerals in surface sediment of the northwest Parece Vela Basin:Distribution and provenance[J]. Oceanologia et Limnologia Sinica, 2007, 38(6):504-511.]
    [9]
    王佳泽, 李安春, 黄杰. 17000年以来冲绳海槽中部沉积物物源演化及其古环境记录[J]. 海洋地质与第四纪地质, 2013, 33(6):105-114.

    [WANG Jiaze, LI Anchun, HUANG Jie, et al. Sediment provenance and paleoenvironment records of the central Okinawa trough for the last 17000 years[J]. Marine Geology and Quaternary Geology, 2013, 33(6):105-114.]
    [10]
    刘志飞, Trentesaux A, Clemens S C,等. 南海北坡ODP1146站第四纪黏土矿物记录:洋流搬运与东亚季风演化[J]. 中国科学D辑, 2003, 33(3):271-280.

    [LIU Zhifei, Trentesaux A, Clemens S C, et al. Quaternary clay mineralogy in the northern South China Sea (ODP Site 1146):Implications for oceanic current transport and East Asian monsoon evolution[J]. Science in China(Series D), 2003, 33(3):271-280.]
    [11]
    刘志飞, Colin C, Trentesaux A,等. 南海南部晚第四纪东亚季风演化的黏土矿物记录[J]. 中国科学D辑, 2004, 34(3). DOI: 10.3321

    /j.issn:1006-9267.2004.03.009.[LIU Zhifei, Colin C, Trentesaux A, et al. Clay mineral records of East Asian monsoon evolution during late Quaternary in the southern South China Sea[J]. Science in China(Series D), 2004, 34(3), DOI: 10.3321/j.issn:1006-9267.2004.03.009.]
    [12]
    Gingele F X, De Deckker P, Hillenbrand C-D. Late Quaternary terrigenous sediments from the Murray Canyons area, offshore South Australia and their implications for sea level change, palaeoclimate and palaeodrainage of the Murray-Darling Basin[J]. Marine Geology, 2004, 212(1):183-197.
    [13]
    刘志飞, 赵玉龙, 李建如,等. 南海西部越南岸外晚第四纪黏土矿物记录:物源分析与东亚季风演化[J]. 中国科学D辑, 2007, 37(9):1176-1184.

    [LIU, Zhifei, ZHAO Yulong, LI Jianru, et al. Late Quaternary clay minerals off Middle Vietnam in the western South China Sea:Implications for source analysis and East Asian monsoon evolution[J]. Science in China(Series D), 2007, 37(9):1176-1184.]
    [14]
    Lamy F, Hebbeln D, Wefer G. High-resolution marine record of climatic change in mid-latitude Chile during the last 28000 years based on terrigenous sediment parameters[J]. Quaternary Research, 1999, 51(1):83-93.
    [15]
    Wan S M, Li A C, Clift P D, et al. Increased contribution of terrigenous supply from Taiwan to the northern South China Sea since 3 Ma[J]. Marine Geology, 2010, 278(1):115-121.
    [16]
    Moore D M, Reynolds R C. X-ray Diffraction and the Identification and Analysis of Clay Minerals[M]. Oxford:Oxford University Press, 1989:179-200.
    [17]
    赵杏媛张有瑜. 黏土矿物与黏土矿物分析[M]. 北京:海洋出版社, 1990:75-79.[ZHAO Xingyuan, ZHANG Youyu. Clay Minerals and Clay Mineral Analysis[M]. Beijing:China Ocean Press, 1990:75

    -79.]
    [18]
    Wan S M, Tian J, Steinke S, et al. Evolution and variability of the East Asian summer monsoon during the Pliocene:Evidence from clay mineral records of the South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 293(1):237-247.
    [19]
    Wan S M, Yu Z J, Clift P D, et al. History of Asian eolian input to the West Philippine Sea over the last one million years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 326:152-159.
    [21]
    万世明. 近2千万年以来东亚季风演化的南海沉积矿物学记录[D]. 北京:中国科学院研究生院, 2006:32-35.[WAN Shiming. Evolution of the East Asian monsoon:mineralogical and sedimentologic records in the South China Sea since 20 Ma[D]. Beijing:University of Chinese Academy of Sciences, 2006

    :32-35.]
    [22]
    Cook H, Johnson P, Matti J, et al. IV. Methods of sample preparation, and X-ray diffraction data analysis, X-ray mineralogy laboratory, deep sea drilling project, University of California, Riverside[J]. Initial Reports of the Deep Sea Drilling Project, 1975, 25:999-1007.
    [23]
    Liu Z F, Colin C, Trentesaux A, et al. Erosional history of the eastern Tibetan Plateau since 190 kyr ago:clay mineralogical and geochemical investigations from the southwestern South China Sea[J]. Marine Geology, 2004, 209(1):1-18.
    [24]
    Huang J, Li A C, Wan S M, et al. Sensitive grain-size records of Holocene East Asian summer monsoon in sediments of northern South China Sea slope[J]. Quaternary Research, 2011, 75(3):734-44.
    [25]
    Wan S M, Clift P D, Li A C, et al. Tectonic and climatic controls on long-term silicate weathering in Asia since 5 Ma[J]. Geophysical Research Letters, 2012, 39, L15611, doi: 10.1029/2012GL052377.
    [26]
    Kahle M, Kleber M, Jahn R. Review of XRD-based quantitative analyses of clay minerals in soils:the suitability of mineral intensity factors[J]. Geoderma, 2002, 109(3):191-205.
  • Related Articles

    [1]GAO Dan, CHENG Rihui, SHEN Yanjie, HOU Shilin, FU Qiulin, WANG Liaoliang. Development of Mesozoic secondary pore zones in the Eastern Depression of North Yellow Sea Basin[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 194-201. DOI: 10.16562/j.cnki.0256-1492.2020121601
    [2]WANG Wenjuan, DOU Zhenya, CHEN Jianwen, ZHANG Yinguo, LIANG Jie. MARINE PALEO-MESOZOIC HYDROCARBON SOURCE ROCKS ON LAND OF THE LOWER YANGTZE PLATFORM AND THEIR IMPLICATIONS FOR OIL AND GAS EXPLORATION IN THE SOUTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 138-146. DOI: 10.16562/j.cnki.0256-1492.2017.03.014
    [3]LI Aimin. MESOZOIC RESERVOIR IN CHENGDAO AREA AND ITS CONTROLLING FACTORS[J]. Marine Geology & Quaternary Geology, 2016, 36(4): 111-117. DOI: 10.16562/j.cnki.0256-1492.2016.04.013
    [4]WU Shuyu, LIU Jun. APPLICATION OF TIME-FREQUENCY ANALYSIS TO THE MESOZOIC RESERVOIR, EASTERN DEPRESSION OF NORTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 189-196. DOI: 10.16562/j.cnki.0256-1492.2016.01.019
    [5]HU Xiaoqiang, WANG Liaoliang. APPLICATION OF DOUBLE-PARAMETER CONSTRAINTS AND PRE-STACK SIMULTANEOUS INVERSION TO PREDICTION OF IGNEOUS BODIES IN THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 87-94. DOI: 10.16562/j.cnki.0256-1492.2015.04.009
    [6]ZHANG Li, GENG Ansong, WANG Liaoliang, LIAO Yuhong, XU Guoqiang, WEI Zhenquan. ASSESSMENT OF MESOZOIC SOURCE ROCKS AT THE MARGIN OF SOUTH CHINA CONTINENT[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 99-108. DOI: 10.3724/SP.J.1140.2012.01099
    [7]LIU Baoming, LIU Hailing. THE MESOZOIC IN THE SOUTH CHINA SEA AND ADJACENT AREAS: NEW TARGETS FOR HYDROCARBON EXPLORATION[J]. Marine Geology & Quaternary Geology, 2011, 31(2): 105-109. DOI: 10.3724/SP.J.1140.2011.02105
    [8]ZHANG Li, SHA Zhi-bin, WANG Li-fei. HYDROCARBON RESOURCES POTENTIAL OF MESOZOIC IN LIYUE BASIN, NORTHEASTERN NANSHA SEA AREAS[J]. Marine Geology & Quaternary Geology, 2007, 27(4): 97-102.
    [9]JIN Chong, LI San-zhong, LOU Da, WANG Lu, XU Shu-mei, LIU Bo, ZHOU Li-hong. STRUCTURAL PATTERN AND EVOLUTION OF THE MESOZOIC STRATA IN THE BOHAI BAY BASIN RANGE: A CASE FROM SOUTHERN SHORE OF MIDDLE RANGE OF THE HUANGHUA DEPRESSION[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 101-110.
    [10]WU Guo-xuan, WANG Ru-jian, HAO Hu-jun, SHAO Lei. MICROFOSSIL EVIDENCE FOR DEVELOPMENT OF MARINE MESOZOIC IN THE NORTH OF SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 79-85.
  • Cited by

    Periodical cited type(2)

    1. 于沨,王登红,于扬,刘铸,高娟琴,仲佳爱,秦燕. 国内外主要沉积型锂矿分布及勘查开发现状. 岩矿测试. 2019(03): 354-364 .
    2. 瓦西拉里,王建华,陈慧娴,吴加学,陶慧. 伶仃洋ZK19孔晚第四纪沉积地球化学特征及其古环境意义. 热带地理. 2016(03): 343-354 .

    Other cited types(9)

Catalog

    Article views (1760) PDF downloads (21) Cited by(11)

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return