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东海内陆架泥区沉积物的环境敏感粒度组分

肖尚斌 李安春

肖尚斌, 李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报, 2005, 23(1): 122-129.
引用本文: 肖尚斌, 李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报, 2005, 23(1): 122-129.
XIAO Shang-bin, LI An-chun. A Study on Environmentally Sensitive Grain-size Population in Inner Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1): 122-129.
Citation: XIAO Shang-bin, LI An-chun. A Study on Environmentally Sensitive Grain-size Population in Inner Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1): 122-129.

东海内陆架泥区沉积物的环境敏感粒度组分

基金项目: 中国科学院海洋研究所创新基金(L61022811)资助
详细信息
    作者简介:

    肖尚斌,男,1970年出生,博士,海洋地质。

  • 中图分类号: P736.2

A Study on Environmentally Sensitive Grain-size Population in Inner Shelf of the East China Sea

  • 摘要: 对东海内陆架泥质沉积区的DD2孔和悬浮体进行了陆源物质提取,应用激光粒度仪做了粒度分析,并分析了DD2孔粒度参数的垂向分布序列。通过计算粒级—标准偏差的变化获得了DD2孔沉积物中对沉积环境变化较为敏感的粒度组分,约 19和 130μm是DD2孔所属区域对沉积环境敏感的粒级,分别对应于东海沿岸流和风暴流沉积动力过程。敏感粒度组分含量随深度变化的分析表明,该孔上段的沉积作用主要受控于沿岸流,沉积环境相对稳定;而下段沉积环境变化大,是风暴流和沿岸流的混合作用沉积的结果。
  • [1] 1 AnZS,Liu T S,Lu Y C. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China[J].Quaternary International,1990.91-95.

    2 AnZS,Kukla G,Porter S C. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years[J].Quaternary Research,1991.29-36.

    3 施雅风,姚檀栋,杨保. 近2000a古里雅冰芯10a尺度的气候变化及其与中国东部文献记录的比较[J].中国科学D辑,1999,(zk):79-86.

    4 姚檀栋,Thompson L G,施雅风. 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,(05):447-452.

    5 洪业汤,姜洪波. 近5 ka温度的金川泥炭δ18O记录[J].中国科学D辑,1997,(06):525-530.

    6 FengX,Epstein S. Climatic implications of an 8000-year hydrogen isotope time series from Bristlecone Pine trees[J].Science,1994.1079-1081.

    8 刘东生,刘嘉麒,吕厚远. 玛珥湖高分辨率古环境研究的新进展[J].第四纪研究,1998,(04):289-295.

    9 ChenJA,Wan G J,Tang D G. Recent climatic changes recorded by sediment grain sizes and isotopes in Erhai Lake[J].Progress in Natural Science,2000,(01):54-61.

    10 TanMT,Liu J,Hou Lǚ. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature[J].Geophysical Research Letters,2003,(12):1617-1620.

    11 安芷生,刘晓东. 东亚季风气候的历史与变率[J].Chinese Science Bulletin,2000,(03):238-249.

    12 王律江,Sarnthein M. 南海北部陆坡近四万年的高分辨率古海洋学记录[J].第四纪研究,1999,(01):27-31.

    13 秦蕴珊,郑铁民. 东海大陆架沉积初分布特征的初步探讨[A].北京:科学出版社,1982.3l-51.

    14 秦蕴珊,赵一阳,陈丽蓉. 东海地质[M].北京:科学出版社,1987.

    15 金翔龙. 东海海洋地质[M].北京:海洋出版社,1992.185-215.

    16 郭志刚,杨作升,雷坤. 东海陆架北部泥质区沉积动力过程的季节性变化规律[J].青岛海洋大学学报,1999,(03):507-513.

    17 MillmanJD,Qin Y S,Park Y A. Sediments and sedimentary processes in the Yellow and East China Seas[A].Tokyo:Terra Scientific Publishing Company,1989.233-249.

    18 SaitoY,Yang Z S. Historical change of the Huanghe (Yellow River) and its impact on the sediment budget of the East China Sea[A].Sapporo:Hokkaido University,1994.7-12.

    19 AlexanderCR,DeMaster D J,Nittrouer C A. Sediment accumulation in a modern epicontinental-shelf setting: the Yellow Sea[J].Marine Geology,1991.51-72.

    20 LeeHJ,Chough S K. Sediment distribution, dispersal and budget in the Yellow Sea[J].Marine Geology,1989.195-205.

    21 郭志刚,杨作升,曲艳慧. 东海陆架泥质区沉积地球化学比较研究[J].沉积学报,2000,(02):284-289.

    22 范德江,孙效功,杨作升. 沉积物物源定量识别的非线性规划模型-以东海陆架北部表层沉积物物源识别为例[J].沉积学报,2002,(01):30-33.

    23 杨作升,郭志刚,王兆祥. 黄东海陆架悬浮体向其东部深海区输送的宏观格局[J].海洋学报(中文版),1992,(02):81-90.

    24 孙效功,方明,黄伟. 黄东海陆架区悬浮体输运的时空变化规律[J].海洋与湖沼,2000,(06):581-587.

    25 苏育松,李风歧,马鹤来. 东海北部底层冷水团的形成及其季节性变化[J].青岛海洋大学学报,1989,(01):1-14.

    26 胡敦欣,杨作升. 东海海洋通量关键过程[M].北京:海洋出版社,2001.3-13.

    27 DeMasterDJ,Mckee B A,Nittrouer C A. Rates of sediment accumulation and particle reworking based on radiochemical measurements from continental shelf deposits in the East China Sea[J].Continental Shelf Research,1985.143-158.

    28 YangZS,Saito Y,Guo Z G. Distal mud area as a material sink in the East China Sea[A].Sapporo:Hokkaido University,1994.1-6.

    29 HoriK,Saito Y,Zhao Q H. Evolution of the coastal depositional systems of the Changjiang Yangtze river in response to late Pleistocene-Holocene sea-level changes[J].Journal of Sedimentary Research,2002,(06):884-897.

    30 LiCX,Chen Q Q,Zhang J Q. Stratigraphy and paleoenviornmental changes in the yangtze delta during late quaternary[J].Journal of Asian Earth Sciences,2000,(18):63-79.

    31 Milliman JD,Meade R H. World-wide delivery of river sediments to theoceans[J].Journal of Geology,1983.1-21.

    32 喻普之,李乃胜. 东海地壳热流[M].北京:海洋出版社,1992.7.

    33 StuiverM,Reimer P J,Bard E. INTCAL98 Radiocarbon age calibration 24,000~0 cal aBP[J].Radiocarbon,1998,(3):1041-1083.

    34 VisherGS. Grain size distributions and depositional processes[J].Journal of Sedimentary Petrology,1969,(03):1074-1106.

    35 FolkRL,Ward W C. Brazos river Bar: A study in the significance of grain-size parameters[J].Journal of Sedimentary Petrology,1957,(27):3-26.

    36 MasonCC,Folk R L. Differentiation of beach, dune, and Aeolian flat environments' by size analysis, Mustang Island, Texas[J].Journal of Sedimentary Petrology,1958.211-226.

    37 FriedmanGM. Distribution between dune, beach, and river sands from the textural characteristics[J].Journal of Sedimentary Petrology,1961.514-519.

    38 FriedmanGM. Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands[J].Journal of Sedimentary Petrology,1961.327-354.

    39 KlovanJE. The use of factor analysis in determining depositional environments from grain-size distributions[J].Journal of Sedimentary Petrology,1966.115-125.

    40 孙东怀,安芷生,苏瑞侠. 古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展,2001,(03):269-276.

    41 SunD,Bloemendal J,Rea D K. Grain-size distribution function of polymodal sediments in hydraulic and Aeolian environments, and numerical partitioning of the sedimentary components[J].Sedimentary Geology,2002.263-277.

    42 高抒,Collins M. 沉积物粒度趋势与海洋沉积物动力学[J].中国科学基金,1998,(04):241-246.

    43 McCaveIN,Manighetti B,Beveridge N A S. Circulation in the glacial North Atlantic inferred from grain-size measurements[J].NATURE,1995.149-51.

    44 McCaveIN,Magnighetti B,Robinson S G. Sortable silt and fine sediment size-composition slicing:parameters forpalaeocurrent speed and palaeoceanography[J].Paleoceanography,1995.593-610.

    45 MoerzT,Wolf-Welling T C W. Data Report: Fine-fraction grain-size distribution data and their statistical treatment and relation to processes Site 1095 (ODP Leg 178, Western Antarctic Peninsula)[A].Results,2001.1-27.

    46 孙有斌,高抒,李军. 边缘海陆源物质中环境敏感粒度组分的初步分析[J].Chinese Science Bulletin,2003,(01):83-87.

    47 WangL,Sarnthein M,Erlenkeuzer H. East Asian monsoon climate during the late-Pleistocene: High resolution sediment records from the South China Sea[J].Marine Geology,1999,(1-4):245-284.

    48 PrinsMA,Postma G,Weltje G J. Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Makran continental slope[J].Marine Geology,2000.351-371.

    49 ReaDK,Hovan S A. Grain-size distribution and depositional processes of the mineal component of abyssal sediments: Lessons from the North Pacific[J].Paleoceanography,1995.251-258.

    50 PrinsMA,Postma G,Cleveringaa J. Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Indus Fan[J].Marine Geology,2000.327-349.

    51 Prins MA,Weltje G J. End-member modeling of siliciclastic grain-size distributions:The late Quaternary record of eolian and fluvial sediment supply to the Arabian Sea and its paleoclimatic significance[A].1999.91-111.

    52 StuutJW,Prins M A,Schneider R R. A 300-kyr record of aridity and wind strength in southwestern Africa: Inferences from grain-size distributions of sediments on Walvis Ridge, SE Atlantic[J].Marine Geology,2002.221-233.

    53 BoulayS,Colin C,Trentesaux A. Mineralogy and sedimentology of Pleistocene sediments on the South China Sea (ODP Site 1144) Proceedings of the Ocean Drilling Program[J].Scientific Results,2002.184.

    54 曲政. 沉积物粒度数据表征方法的研究[J].中国粉体技术,2001,(04):24-31.

    55 范德江,杨作升,孙效功. 东海陆架北部长江、黄河沉积物影响范围的定量估算[J].青岛海洋大学学报,2002,(05):748-756.
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目录

    东海内陆架泥区沉积物的环境敏感粒度组分

      基金项目:  中国科学院海洋研究所创新基金(L61022811)资助
      作者简介:

      肖尚斌,男,1970年出生,博士,海洋地质。

    • 中图分类号: P736.2

    摘要: 对东海内陆架泥质沉积区的DD2孔和悬浮体进行了陆源物质提取,应用激光粒度仪做了粒度分析,并分析了DD2孔粒度参数的垂向分布序列。通过计算粒级—标准偏差的变化获得了DD2孔沉积物中对沉积环境变化较为敏感的粒度组分,约 19和 130μm是DD2孔所属区域对沉积环境敏感的粒级,分别对应于东海沿岸流和风暴流沉积动力过程。敏感粒度组分含量随深度变化的分析表明,该孔上段的沉积作用主要受控于沿岸流,沉积环境相对稳定;而下段沉积环境变化大,是风暴流和沿岸流的混合作用沉积的结果。

    English Abstract

    肖尚斌, 李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报, 2005, 23(1): 122-129.
    引用本文: 肖尚斌, 李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报, 2005, 23(1): 122-129.
    XIAO Shang-bin, LI An-chun. A Study on Environmentally Sensitive Grain-size Population in Inner Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1): 122-129.
    Citation: XIAO Shang-bin, LI An-chun. A Study on Environmentally Sensitive Grain-size Population in Inner Shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1): 122-129.
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