锰结核生长与沉积环境的关系

罗尚德; 王蕾; 奕普

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锰结核生长与沉积环境的关系

罗尚德, 王蕾, 奕普

文章导航 > 沉积学报 > 1989 > 7(4): 77-84

罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系[J]. 沉积学报, 1989, 7(4): 77-84.

引用本文:

罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系[J]. 沉积学报, 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.

罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系[J]. 沉积学报, 1989, 7(4): 77-84.

引用本文:

罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系[J]. 沉积学报, 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.

锰结核生长与沉积环境的关系

厦门大学海洋系

详细信息

作者简介:
罗尚德，男，29岁，博士研究生，海洋化学

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文章访问数: 606
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RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

Department of Oceanography, Xiamen University, Xiamen

摘要

摘要: 本文收集了48组世界大洋各种沉积环境锰结核化学组成和生长速率数据并计算了它们的铁锰通量；讨论了不同环境的锰结核的铁锰含量之间的关系，以及锰通量与铁通量、Mn/Fe比的相关性；导出了由锰结核锰铁含量计算生长速率的经验关系；从本质上揭示了锰结核化学组成、生长速率与沉积环境的内在联系，为探讨锰结核形成机理提供了有力的依据。
- 锰结核 /
- 沉积环境 /
- 化学组成 /
- 生长速率
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]

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参考文献(13)

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[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.

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[18]	赵全基, 周希林, 张壮域, 王相芹. 北太平洋锰结核伴生沉积物中某些金属元素的地球化学行为探讨 . 沉积学报, 1990, 8(2): 97-104.
[19]	钱江初, 徐征宇, 王星福. 太平洋锰结核生长速率的初步研究 . 沉积学报, 1990, 8(1): 122-128.
[20]	沈华悌. 中太平洋海盆表层沉积物及其与锰结核的关系 . 沉积学报, 1989, 7(3): 129-136.

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锰结核生长与沉积环境的关系

厦门大学海洋系

作者简介:
罗尚德，男，29岁，博士研究生，海洋化学

收稿日期: 1987-07-28
刊出日期: 1989-12-10

关键词:

锰结核 /

沉积环境 /

化学组成 /

生长速率

摘要: 本文收集了48组世界大洋各种沉积环境锰结核化学组成和生长速率数据并计算了它们的铁锰通量；讨论了不同环境的锰结核的铁锰含量之间的关系，以及锰通量与铁通量、Mn/Fe比的相关性；导出了由锰结核锰铁含量计算生长速率的经验关系；从本质上揭示了锰结核化学组成、生长速率与沉积环境的内在联系，为探讨锰结核形成机理提供了有力的依据。

English Abstract

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]

罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系[J]. 沉积学报, 1989, 7(4): 77-84.

引用本文:

罗尚德, 王蕾, 奕普. 锰结核生长与沉积环境的关系[J]. 沉积学报, 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.

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锰结核生长与沉积环境的关系

作者简介:
罗尚德，男，29岁，博士研究生，海洋化学

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RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

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目录

锰结核生长与沉积环境的关系

厦门大学海洋系

作者简介:
罗尚德，男，29岁，博士研究生，海洋化学

English Abstract

RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

Department of Oceanography, Xiamen University, Xiamen

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锰结核生长与沉积环境的关系

作者简介: 罗尚德，男，29岁，博士研究生，海洋化学

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RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

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锰结核生长与沉积环境的关系

厦门大学海洋系

作者简介: 罗尚德，男，29岁，博士研究生，海洋化学

English Abstract

RELATIONSHIP BETWEEN ACCRETION OF MANGANESE NODULES AND SEDIMENTARY ENVIRONMENTS

Department of Oceanography, Xiamen University, Xiamen

全文HTML

目录

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期刊在线

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作者简介:
罗尚德，男，29岁，博士研究生，海洋化学

作者简介:
罗尚德，男，29岁，博士研究生，海洋化学