Advanced Search
Volume 7 Issue 4
. 
Turn off MathJax
Article Contents
Abstract
References
Article Navigation >  Acta Sedimentologica Sinica  > 1989  >  7(4): 77-84

Luo Shangde, Wang Lei, Huang Yipu. RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS[J]. Acta Sedimentologica Sinica, 1989, 7(4): 77-84.
Citation: Luo Shangde, Wang Lei, Huang Yipu. RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS[J]. Acta Sedimentologica Sinica, 1989, 7(4): 77-84.
shu

RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

  • Department of Oceanography, Xiamen University, Xiamen

  • Received Date: 1987-07-28
  • Publish Date: 1989-12-10
  • 48 data sets on the major chemical compositions (Mn and Fe concentrations) and growth rates of manganese nodules from different sedimentary environments of the oceans have been collected and their fluxes of manganese and iron have been calculated. It has been shown that although the chemical compositions and growth rates of manganese nodules from different areas of the oceans are largely different ( Mn: 11.3-44.9% ； Fe: 0.724-20.5% ； growth rates； 0.8O-2OOmm/106yr) , there are small differences in Fe fluxes (10-102mg Fe/cm2 ? 106yr at most) but large one in Mn fluxes (in range of 10 to 104mg Mn/cm2 ? 106yr) ， reflecting that the diagenetic reactivity of manganese is much stronger than that of iron in marine environments. It has been demonstrated by statistical analyses the (I) the concentrations of manganese and iron of individual nodules are correlative positively for the nodules with the Mn /Fe ratios of ?1 but negatively for those with high Mn /Fe ratios becauce of different contribution of diagenetic manganese; (2) The relationships of Mn fluxes to Fe fluxes or Mn /Fe ratios of the manganese nodules are dependent on classification of sedimentary environments, but the changes of Mn fluxes and Mn /Fe ratios caused only by diagenetic processes are linearly correlative, independent on the classification of sedimentary environments. The following equation, derived from the correlation of Mn fluxes to Mn /Fe ratios of manganese modules, can be used to predict the growth rates from the Mn concentrations and Ma/Fe ratios of the nodules and reveal the importance of sedimentary environments to the chemical composition and growth rate of manganese nodules: S(mm/106yr) =[52.0(Mn/Fe-0.6O)125+ 10]/[Mn]
  • [1] Dyraond J. and Lyle M. et al.， 1984, Gcochim.Cosmochira.Acta 48, p.931-949.
    [2] Finney B., Health G.R. and Lylcr M., 1984, Gcochim.Cosmochira.Acta 48, p.911-917.
    [3] Heye D. and Marchig V., 1977, Mar.Geol.23， M19-M25.
    [4] Huh C.A.and Ku T.L., 1984, Geochim.Cosraochim.Acta 48, p.951-963.
    [5] Krishnaswami S. and Lal D., 1972, Manganese nodules and Budget of trace soluble in the oceans, In: The Changing Chemistry of the Oceans, Noble Symposium 20 (eds.D.Dyrsscn and Tagner), New York, Wiley Interscience.
    [6] Ku T.L.1977， Rates of accretion, In: Marine Manganese Deposits (ed. G.P.Glasby).
    [7] Kusakabc M. and Ku T.L. 1984, Geochim.Cosmochira.Acta 48, 2187-2193.
    [8] Lyle M., 1982, Gcochim.Cosmochira.Acta, 46， p.2301-2306.
    [9] Mero J.M. 1965, The Mineral Resources of the Sea, Amsterdam, Elsevier.
    [10] Moore W.S.et al., 1981, Earth Planet.Sci. lett.52, p.151-171.
    [11] Reyss J.L.et al., 1982, Nature 295, p.401-403.
    [12] Somayajulu B.L.K. et al., 1971， Geochim.Cosraochim.Acta, 35， p.621-624.
    [13] Tsunogai S., et al. 1982, Geochcm. J.16, p.199-212.
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-052024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-0400.250.50.7511.25
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 2.7 %FULLTEXT: 2.7 %META: 89.9 %META: 89.9 %PDF: 7.5 %PDF: 7.5 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 2.1 %其他: 2.1 %其他: 1.8 %其他: 1.8 %Seattle: 0.3 %Seattle: 0.3 %United States: 1.2 %United States: 1.2 %三明: 0.3 %三明: 0.3 %上海: 5.4 %上海: 5.4 %东京: 0.9 %东京: 0.9 %东莞: 0.3 %东莞: 0.3 %中卫: 0.9 %中卫: 0.9 %乌海: 0.3 %乌海: 0.3 %佛山: 0.3 %佛山: 0.3 %兰州: 0.3 %兰州: 0.3 %凉山: 0.3 %凉山: 0.3 %北京: 16.4 %北京: 16.4 %南宁: 0.3 %南宁: 0.3 %南通: 0.6 %南通: 0.6 %台州: 1.5 %台州: 1.5 %吕梁: 0.6 %吕梁: 0.6 %呼伦贝尔: 0.3 %呼伦贝尔: 0.3 %咸阳: 0.3 %咸阳: 0.3 %哥伦布: 0.3 %哥伦布: 0.3 %嘉峪关: 0.3 %嘉峪关: 0.3 %天津: 0.3 %天津: 0.3 %安康: 0.3 %安康: 0.3 %宜春: 0.3 %宜春: 0.3 %山景城: 0.3 %山景城: 0.3 %常州: 0.3 %常州: 0.3 %广州: 0.3 %广州: 0.3 %廊坊: 0.3 %廊坊: 0.3 %张家口: 1.8 %张家口: 1.8 %成都: 0.6 %成都: 0.6 %扬州: 0.3 %扬州: 0.3 %抚州: 0.3 %抚州: 0.3 %文山: 0.3 %文山: 0.3 %日喀则: 0.3 %日喀则: 0.3 %日照: 0.6 %日照: 0.6 %昆明: 0.3 %昆明: 0.3 %昌吉: 0.3 %昌吉: 0.3 %杭州: 3.9 %杭州: 3.9 %武汉: 1.2 %武汉: 1.2 %泉州: 0.3 %泉州: 0.3 %洛阳: 0.6 %洛阳: 0.6 %济南: 0.3 %济南: 0.3 %深圳: 0.3 %深圳: 0.3 %温州: 0.3 %温州: 0.3 %湖州: 0.9 %湖州: 0.9 %漯河: 1.2 %漯河: 1.2 %潍坊: 0.3 %潍坊: 0.3 %牡丹江: 0.3 %牡丹江: 0.3 %玉林: 0.3 %玉林: 0.3 %福州: 0.3 %福州: 0.3 %秦皇岛: 0.6 %秦皇岛: 0.6 %芒廷维尤: 4.8 %芒廷维尤: 4.8 %芝加哥: 2.7 %芝加哥: 2.7 %苏州: 0.6 %苏州: 0.6 %蚌埠: 0.3 %蚌埠: 0.3 %衡阳: 0.3 %衡阳: 0.3 %衢州: 0.3 %衢州: 0.3 %襄阳: 0.6 %襄阳: 0.6 %西宁: 31.6 %西宁: 31.6 %西安: 0.3 %西安: 0.3 %贵阳: 1.8 %贵阳: 1.8 %郑州: 0.6 %郑州: 0.6 %酒泉: 0.3 %酒泉: 0.3 %重庆: 0.6 %重庆: 0.6 %银川: 0.6 %银川: 0.6 %长沙: 0.9 %长沙: 0.9 %青岛: 0.6 %青岛: 0.6 %马鞍山: 0.6 %马鞍山: 0.6 %其他其他SeattleUnited States三明上海东京东莞中卫乌海佛山兰州凉山北京南宁南通台州吕梁呼伦贝尔咸阳哥伦布嘉峪关天津安康宜春山景城常州广州廊坊张家口成都扬州抚州文山日喀则日照昆明昌吉杭州武汉泉州洛阳济南深圳温州湖州漯河潍坊牡丹江玉林福州秦皇岛芒廷维尤芝加哥苏州蚌埠衡阳衢州襄阳西宁西安贵阳郑州酒泉重庆银川长沙青岛马鞍山
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

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索
Get Citation
PDF
XML

Article Metrics

Article views(582) PDF downloads(338) Cited by()

Proportional views
Related
Publishing history
  • Received:  1987-07-28
  • Published:  1989-12-10

RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

  • Department of Oceanography, Xiamen University, Xiamen
  • Received Date: 1987-07-28
  • Publish Date: 1989-12-10

Abstract: 48 data sets on the major chemical compositions (Mn and Fe concentrations) and growth rates of manganese nodules from different sedimentary environments of the oceans have been collected and their fluxes of manganese and iron have been calculated. It has been shown that although the chemical compositions and growth rates of manganese nodules from different areas of the oceans are largely different ( Mn: 11.3-44.9% ； Fe: 0.724-20.5% ； growth rates； 0.8O-2OOmm/106yr) , there are small differences in Fe fluxes (10-102mg Fe/cm2 ? 106yr at most) but large one in Mn fluxes (in range of 10 to 104mg Mn/cm2 ? 106yr) ， reflecting that the diagenetic reactivity of manganese is much stronger than that of iron in marine environments. It has been demonstrated by statistical analyses the (I) the concentrations of manganese and iron of individual nodules are correlative positively for the nodules with the Mn /Fe ratios of ?1 but negatively for those with high Mn /Fe ratios becauce of different contribution of diagenetic manganese; (2) The relationships of Mn fluxes to Fe fluxes or Mn /Fe ratios of the manganese nodules are dependent on classification of sedimentary environments, but the changes of Mn fluxes and Mn /Fe ratios caused only by diagenetic processes are linearly correlative, independent on the classification of sedimentary environments. The following equation, derived from the correlation of Mn fluxes to Mn /Fe ratios of manganese modules, can be used to predict the growth rates from the Mn concentrations and Ma/Fe ratios of the nodules and reveal the importance of sedimentary environments to the chemical composition and growth rate of manganese nodules: S(mm/106yr) =[52.0(Mn/Fe-0.6O)125+ 10]/[Mn]

Luo Shangde, Wang Lei, Huang Yipu. RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS[J]. Acta Sedimentologica Sinica, 1989, 7(4): 77-84.
Citation: Luo Shangde, Wang Lei, Huang Yipu. RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS[J]. Acta Sedimentologica Sinica, 1989, 7(4): 77-84.
shu

    HTML

Reference (13)

Catalog

    Links

    Journal Online

    Contact Us

    • Website Copyright © 2011 Editorial Office of Acta Sedimentologica Sinica
    • Address: 8 Tianshui Middle Road, Lanzhou
    • Post code: 730000   Tel:（0931）8264231
    • 陇ICP备2021001824号-28
    • 甘公网安备 62010202000673号
    Wechat

    Email alert

    RSS

    Supported by: Beijing Renhe Information Technology Co. Ltd  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return