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

XIAO Shang-bin; LI An-chun

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 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.

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

Received Date: 2004-02-13
Rev Recd Date: 2004-10-09
Publish Date: 2005-03-10

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

References

[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.

Proportional views

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

Get Citation

PDF

XML

Article Metrics

Article views(643) PDF downloads(734) Cited by()

Proportional views

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

Received Date: 2004-02-13

Rev Recd Date: 2004-10-09

Publish Date: 2005-03-10

Key words:

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.

HTML

Reference (1)

[1]

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

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related