scholarly journals Sulfating Roasting of Manganese Nodules in the Presence of Jarosite

Author(s):  
Masayasu KAWAHARA ◽  
Kimihiro FURE ◽  
Toshiharu MITSUO
1991 ◽  
Vol 107 (5) ◽  
pp. 305-309 ◽  
Author(s):  
Masayasu KAWAHARA ◽  
Kiyozumi TOKIKAWA ◽  
Toshiharu MITSUO

1996 ◽  
Vol 183 (2) ◽  
pp. 374-379 ◽  
Author(s):  
K.M. Parida ◽  
A.K. Sahoo ◽  
N.N. Das

1973 ◽  
Vol 4 (4) ◽  
pp. 941-947 ◽  
Author(s):  
M. C. Hecke ◽  
R. W. Bartlett

1878 ◽  
Vol 9 ◽  
pp. 287-289
Author(s):  
J. Y. Buchanan

The manganese nodules occur in greater or less quantity all over the ocean-bed, and most abundantly in the Pacific. They occur of all sizes, from minute grains to masses of a pound weight, and even greater, and form nodular concretions of concentric shells, round a nucleus, which is very frequently a piece of pumice or a shark's tooth. Their outside has a peculiar and very characteristic mammillated surface, which enables them to be identified at a glance. When freshly brought up they are very soft, being easily scraped to powder with a knife. They gradually get harder on exposure to the air.


Minerals ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 227
Author(s):  
Akira Tsune

Manganese (polymetallic) nodules on the deep seafloor in the open ocean have attracted great interest because of their economic potential. Visual data on nodules found on the deep seafloor such as photographs and videos have increased exponentially with the recent progress of related technologies. These data are expected to reflect useful information for estimating these mineral resources, as well as understanding their geological origin. Although the size, number, and coverage of manganese nodules have been measured in seafloor images, the burial of such nodules has not been sufficiently examined. This paper focuses on mathematical expression of the burial of the manganese nodules and attempts to quantitatively elucidate relations among burial degree and nodule geological parameters. The results, that is, a dataset obtained by calculations of relations among parameters, are also utilized for considerations of quantitative expression of burial. These considerations are expected to contribute to a better understanding of the geological origin of manganese nodules.


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