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

东海内陆架泥区沉积物的环境敏感粒度组分

肖尚斌^1,2,
李安春¹

1.
中国科学院海洋研究所,山东青岛 266071;
2.
中国科学院南海海洋研究所,广州 510301

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

计量

文章访问数: 587
HTML全文浏览量: 18
PDF下载量: 731
被引次数: 0

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

XIAO Shang-bin^1,2,
LI An-chun¹

1.
Institute of Oceanology, Chinese Academy Sciences, Qingdao Shandong 266071;
2.
South China Sea Institute of Oceanology, Guangzhou 510301

摘要

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。
- 粒度组分 /
- 陆源物质 /
- 东海内陆架
Abstract: Grain-size distribution of 149 sediment samp les of Core DD2 and 3 suspended sediment samp les, pretreated by removing the organic matter and carbonate, are measured by use ofMalvern 2000. The samp ling sites are located in the inner shelf of the East China Sea. Vertical distribution of grain-size parameters of Core DD2 is studied. Standard deviations are calculated for all 149 samp les. Two peaks are observed in plot standard deviation values vs.grain-size classes, at about 19 and 130μm grain size, respectively. They are environmentally sensitive grain-size population. And about 19μm is sensitive to coastal current of the East China Sea, the other is to storm current. Each of these size classes rep resents a population of grainswith the highest variability through time. Vertical contents of sensitive grain-size population are carried out. It shows that the sedimentations of upper Core DD2 was controlled by coastal current and was in relatively stable environment. This result is supported by the comparison analysis between the modern suspended sediments and Core DD2. And lower part was controlled by combination of coastal and storm currents and was in unstable environment.
- grain-size population /
- terrigenousmatter /
- inner shelf of the East China Sea

HTML全文

参考文献(1)

[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.

[1]	刘晓杰, 季银利, 向荣, 张大海, 李先国. 东海内陆架岩心中木质素的沉积记录 . 沉积学报, 2022, 40(2): 525-533. doi: 10.14027/j.issn.1000-0550.2020.083
[2]	王明霄, 郑世雯, 范德江. 东海内陆架近两百年来有孔虫组合变化及原因 . 沉积学报, 2021, 39(4): 973-982. doi: 10.14027/j.issn.1000-0550.2020.108
[3]	袁忠鹏, 胡刚, 王永红, 黄畅, 贾仲佳, 梁伟强, 彭锦. 东海内陆架泥质体远端表层沉积物孢粉分布规律及其环境意义 . 沉积学报, 2021, 39(3): 610-620. doi: 10.14027/j.issn.1000-0550.2020.113
[4]	张明宇, 常鑫, 胡利民, 毕乃双, 王厚杰, 刘喜停. 东海内陆架有机碳的源—汇过程及其沉积记录 . 沉积学报, 2021, 39(3): 593-609. doi: 10.14027/j.issn.1000-0550.2020.080
[5]	丛静艺, 袁忠鹏, 胡刚, 毕世普, 张勇, 王永红, 马晓红, 江云水, 宁泽. 长江远端三角洲多源沉积分异作用及其动力机制 . 沉积学报, 2020, 38(3): 528-537. doi: 10.14027/j.issn.1000-0550.2019.064
[6]	周瑞琦, 傅恒, 徐国盛, 苗清, 付振群. 东海陆架盆地西湖凹陷平湖组-花港组沉积层序 . 沉积学报, 2018, 36(1): 132-141. doi: 10.3969/j.issn.1000-0550.2018.015
[7]	. 陆源沉积岩物源分析研究进展与发展趋势 . 沉积学报, 2013, 31(1): 99-107.
[8]	刘升发. 近2 ka以来东海内陆架泥质区高分辨率的生物硅记录及其古生产力意义 . 沉积学报, 2011, 29(2): 321-327.
[9]	徐方建. 末次冰消期以来东海内陆架古环境演化 . 沉积学报, 2009, 27(1): 118-127.
[10]	熊应乾. 东海陆架EA01孔沉积物常微量元素变化及其意义 . 沉积学报, 2006, 24(3): 356-364.
[11]	栾锡武, 赵一阳, 秦蕴珊, 高德章, 赵金海. 我国东海陆架区新生代地层岩石生热率研究 . 沉积学报, 2003, 21(4): 634-639.
[12]	郭志刚, 杨作升, 曲艳慧, 范德江. 东海陆架泥质区沉积地球化学比较研究 . 沉积学报, 2000, 18(2): 284-289.
[13]	陈刚. 中生代鄂尔多斯盆地陆源碎屑成分及其构造属性 . 沉积学报, 1999, 17(3): 409-413.
[14]	邵磊, 李文厚, 袁明生. 吐鲁番—哈密盆地陆源碎屑沉积环境及物源分析 . 沉积学报, 1999, 17(3): 435-442.
[15]	沈浩杰, 王先兰. 东海大陆架南部边缘晚更新世淹没海滩岩的发现及其地质意义 . 沉积学报, 1999, 17(S1): 782-788.
[16]	沈浩杰. 东海大陆架南缘海域地层声学剖面及地质解释 . 沉积学报, 1999, 17(1): 78-83.
[17]	张廷山, 兰光志, 陈晓慧, 俞剑华, 边立曾. 川西北早志留世陆源碎屑──碳酸盐混积缓坡 . 沉积学报, 1995, 13(4): 27-36.
[18]	秦蕴珊. 全球变化与陆架沉积 . 沉积学报, 1992, 10(3): 40-46.
[19]	王成厚. 东海陆架近岸区SO₄^2-扩散通量的初步研究 . 沉积学报, 1986, 4(1): 110-116.
[20]	唐运千, 垄敏, 朱凤冠. 东海大陆架沉积物中类脂和腐植物质的研究 . 沉积学报, 1983, 1(2): 118-130.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 587
HTML全文浏览量: 18
PDF下载量: 731
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

东海内陆架泥区沉积物的环境敏感粒度组分

作者简介:
肖尚斌，男，1970年出生，博士，海洋地质。

计量

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

计量

目录

东海内陆架泥区沉积物的环境敏感粒度组分

1. 中国科学院海洋研究所,山东青岛 266071;

2. 中国科学院南海海洋研究所,广州 510301

作者简介:
肖尚斌，男，1970年出生，博士，海洋地质。

English Abstract

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

1. Institute of Oceanology, Chinese Academy Sciences, Qingdao Shandong 266071;

2. South China Sea Institute of Oceanology, Guangzhou 510301

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

东海内陆架泥区沉积物的环境敏感粒度组分

作者简介: 肖尚斌，男，1970年出生，博士，海洋地质。

计量

出版历程

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

计量

出版历程

目录

东海内陆架泥区沉积物的环境敏感粒度组分

1. 中国科学院海洋研究所,山东青岛 266071; 2. 中国科学院南海海洋研究所,广州 510301

作者简介: 肖尚斌，男，1970年出生，博士，海洋地质。

English Abstract

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

1. Institute of Oceanology, Chinese Academy Sciences, Qingdao Shandong 266071; 2. South China Sea Institute of Oceanology, Guangzhou 510301

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
肖尚斌，男，1970年出生，博士，海洋地质。

1. 中国科学院海洋研究所,山东青岛 266071;

2. 中国科学院南海海洋研究所,广州 510301

作者简介:
肖尚斌，男，1970年出生，博士，海洋地质。

1. Institute of Oceanology, Chinese Academy Sciences, Qingdao Shandong 266071;

2. South China Sea Institute of Oceanology, Guangzhou 510301