scholarly journals Rare-earth elements in the top samples of the cores from the Pacific Ocean floor

1972 ◽  
Vol 6 (2) ◽  
pp. 75-81 ◽  
Author(s):  
Toshinari Shimokawa ◽  
Akimasa Masuda ◽  
Kiyoaki Izawa
Minerals ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 142
Author(s):  
Jelena Milinovic ◽  
Francisco J. L. Rodrigues ◽  
Fernando J. A. S. Barriga ◽  
Bramley J. Murton

The rare earth elements (REE), comprising 15 elements of the lanthanum series (La-Lu) together with yttrium (Y) and scandium (Sc), have become of particular interest because of their use, for example, in modern communications, renewable energy generation, and the electrification of transport. However, the security of supply of REE is considered to be at risk due to the limited number of sources, with dependence largely on one supplier that produced approximately 63% of all REE in 2019. As a result, there is a growing need to diversify supply. This has resulted in the drive to seek new resources elsewhere, and particularly on the deep-ocean floor. Here, we give a summary of REE distribution in minerals, versatile applications, and an update of their economic value. We present the most typical onshore methods for the determination of REE and examine methods for their offshore exploration in near real time. The motivation for this comes from recent studies over the past decade that showed ΣREE concentrations as high as 22,000 ppm in ocean-floor sediments in the Pacific Ocean. The ocean-floor sediments are evaluated in terms of their potential as resources of REE, while the likely economic cost and environmental impacts of deep-sea mining these are also considered.


2011 ◽  
Vol 4 (8) ◽  
pp. 535-539 ◽  
Author(s):  
Yasuhiro Kato ◽  
Koichiro Fujinaga ◽  
Kentaro Nakamura ◽  
Yutaro Takaya ◽  
Kenichi Kitamura ◽  
...  

1975 ◽  
Vol 69 (4) ◽  
pp. 855-858 ◽  
Author(s):  
Alfred P. Rubin

In a series of newspaper columns and stories beginning March 19, 1975 the American public was told apparently correctly about the partial success of the Central Intelligence Agency in raising a Soviet submarine, its equipment, and dead crew from the Pacific Ocean floor. The location of the pertinent activities was reported to be well beyond any state's claim to territorial waters, continental shelves, contiguous zones, or other asserted inhibiting zones. The CIA vessel, The Glomar Explorer, was disguised as a commercially operated oceanographic research vessel. No international legal implications seem to have been perceived by the newspapers in the American intelligence activities.


Author(s):  
G. V. Novikov ◽  
N. V. Lobus ◽  
A. N. Drozdova ◽  
Yu. P. Dikov

Cobalt-rich manganese crusts and crust-concretion formations from the guyots of the Pacific Ocean were found to be the natural highly selective sorbents of rare-earth cations Ce3+, Y3+, La3+. Ion exchange capacity of ore minerals — vernadite, Fe-vernadite and Mn-ferroxyhyte — increases in the following sequence La3+<Y3+<Co2+<Ce3+ and averages from 1.67 (La3+) to 2.84 (Се3+) meq/g, which is quite high values among natural mineral ion exchangers. Ore minerals of crusts exhibit higher selectivity to Се3+ cation compared to Y3+ и La3+. The age of ore minerals does not affect their sorption with respect to rare earth element cations.


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