The Enrichment Regularity of Rare Earth Elements and Resource Characteristics in Polymetallic Nodules/Crusts

Article Preview

Abstract:

Polymetallic nodules/crusts are one of the most important mineral deposits in the ocean, in which iron, manganese, copper, cobalt, nickel and other metals are rich, and rare earth elements are rich, too. In this study, the contents of 11 rare earth samples in polymetallic nodules/crusts from the Pacific, Atlantic, Indian Ocean and north of the South China Sea are analyzed. The average content of rare earth in polymetallic nodules/crusts is 1265.57×10-6, the average content of nodules is 1096.96×10-6, and the average content of crust is 1623.88×10-6. The enrichment of rare earth elements is controlled by iron and manganese oxides and clay minerals in nodules/crusts, which could absorb rare earth elements from seawater and sediment. Ce elements are highly enriched, making polymetallic nodules/crusts become the first used rare earth elements in mineral development.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 284-286)

Pages:

2497-2500

Citation:

Online since:

July 2011

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2011 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] McMurtry G M. Authigenic Deposits. Encyclopedia of Ocean Sciences, 2003, 201~212

Google Scholar

[2] Morgan C L. Resource estimates of the Clarion-Clipperton manganese nodule deposits: In, Handbook of Marine Mineral Deposits, Cronan, D.S., ed., CRC Press, London, 2000, 145~170

DOI: 10.1201/9780203752760-6

Google Scholar

[3] Suave R L, Pichocki C, Pautot G., et al.Geological and mineralogical study of Co-rich ferro- manganese crusts from a submerged atoll in the Tuamotu Archipelago (French Polynesia)[J]. Marine Geology, 1989, 87(2-4): 227~247

DOI: 10.1016/0025-3227(89)90063-7

Google Scholar

[4] Zhang F Y, Zhang W Y, Gao S T, et al. Distribution Characteristics of Cobalt-rich Ferro- manganese Crust Resources on Submarine Seamounts in the Western Pacific[J].Acta Geologica Sinica, 2008,82(4):70~77

DOI: 10.1111/j.1755-6724.2008.tb00633.x

Google Scholar

[5] Li T. Chemical Element Abundances in the Earth and It's Major Shells [J].Geochimica, 1976, 3:167~174

Google Scholar

[6] Lan X H,Wang H X,Zhang Z X,et al. Distributions of Rare Earth Elements and Provenance Relations in the Surface Sediments of the South Yellow Sea [J]. Journal of the Chinese Rare Earth Society, 2006, 26(4):745~749

DOI: 10.3724/sp.j.1140.2012.01011

Google Scholar

[7] Xu Z K,Li A C,Jiang F Q,et al. Characteristics and origin of the new-type Ferromanganese Crusts from deepwater areas of the East Philippine Sea [J]. Marine Geology & Quaternary Geology, 2006, 26(4):91~98

Google Scholar

[8] Piper D Z and Williamson M E. Composition of Pacific Ocean ferromanganese nodules. Marine Geology, 1977, 23(4):285~303

DOI: 10.1016/0025-3227(77)90036-6

Google Scholar