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Qian jiangchu, Xu Zhcnyu, Wang Xingfu. RESEARCH ON GROWTH RATES OF MANGANESE NODULES FROM NORTH PACIFIC[J]. Acta Sedimentologica Sinica, 1990, 8(1): 122-128.
Citation: Qian jiangchu, Xu Zhcnyu, Wang Xingfu. RESEARCH ON GROWTH RATES OF MANGANESE NODULES FROM NORTH PACIFIC[J]. Acta Sedimentologica Sinica, 1990, 8(1): 122-128.

RESEARCH ON GROWTH RATES OF MANGANESE NODULES FROM NORTH PACIFIC

  • Publish Date: 1990-03-10
  • Many research items on the manganese nodules from ocean bottom have been earned ouu but the growth rales of manganese nodules as well as their movements on the ocean bottom still puzzles the scientists. Various methods have bee created to answer these question. The trustworthy and acceptable methods are -230Th excess; -230Th / -232Th; -231Pa; K / Ar and -10Be. Three manganese nodules have been analysed using -230Th excess and -230Th / -232Th methods in order to detect their growth rates. The procedures are as follows: Successive layers of specimens from top side and bottom side arc scraped; acid leaching; separation and purification of U and Th using Dowcsi-8 resin; TTA extraction and a counting. The growth rates of three nodules using two different methods a;e agreeable, ranging l-10mm / M.Yr. The last turnover of the noduics can be evaluated from the different activities of -230Th at the surface of top and bottom sides. The results range from 5 ×104to 2.5 × 105ycars, thereat -210Pb profiles indicates that the turnover of the noduics didn ' t take place in the last 150 years.
  • [1] (1) Krishnaswami, S.1982. Earth Planct Sci. 1ctt.N.59 P.312-320.

    (2) Ku,ti.ct al. 1967. Earth Planct Sci. Lett N2 P.317-320.

    (3) Huh,C.A. and Ku, T.L.1984. Gcochim. Acta, 48.p.951-963.
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  • Published:  1990-03-10

RESEARCH ON GROWTH RATES OF MANGANESE NODULES FROM NORTH PACIFIC

Abstract: Many research items on the manganese nodules from ocean bottom have been earned ouu but the growth rales of manganese nodules as well as their movements on the ocean bottom still puzzles the scientists. Various methods have bee created to answer these question. The trustworthy and acceptable methods are -230Th excess; -230Th / -232Th; -231Pa; K / Ar and -10Be. Three manganese nodules have been analysed using -230Th excess and -230Th / -232Th methods in order to detect their growth rates. The procedures are as follows: Successive layers of specimens from top side and bottom side arc scraped; acid leaching; separation and purification of U and Th using Dowcsi-8 resin; TTA extraction and a counting. The growth rates of three nodules using two different methods a;e agreeable, ranging l-10mm / M.Yr. The last turnover of the noduics can be evaluated from the different activities of -230Th at the surface of top and bottom sides. The results range from 5 ×104to 2.5 × 105ycars, thereat -210Pb profiles indicates that the turnover of the noduics didn ' t take place in the last 150 years.

Qian jiangchu, Xu Zhcnyu, Wang Xingfu. RESEARCH ON GROWTH RATES OF MANGANESE NODULES FROM NORTH PACIFIC[J]. Acta Sedimentologica Sinica, 1990, 8(1): 122-128.
Citation: Qian jiangchu, Xu Zhcnyu, Wang Xingfu. RESEARCH ON GROWTH RATES OF MANGANESE NODULES FROM NORTH PACIFIC[J]. Acta Sedimentologica Sinica, 1990, 8(1): 122-128.
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