scholarly journals The X-ray study of Fe-Ti ore minerals from the Pacific Ocean

1993 ◽  
Vol 49 (s1) ◽  
pp. c263-c264
Author(s):  
M. T. Dmitrieva
2013 ◽  
Vol 450 (1) ◽  
pp. 566-570 ◽  
Author(s):  
G. V. Novikov ◽  
I. V. Vikent’ev ◽  
M. E. Mel’nikov ◽  
O. Yu. Bogdanova ◽  
N. I. Eremin

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.


2018 ◽  
Vol 240 ◽  
pp. 274-292 ◽  
Author(s):  
Teruhiko Kashiwabara ◽  
Ryuichi Toda ◽  
Kentaro Nakamura ◽  
Kazutaka Yasukawa ◽  
Koichiro Fujinaga ◽  
...  

2001 ◽  
Vol 28 (19) ◽  
pp. 3721-3724
Author(s):  
Cathy Stephens

Sign in / Sign up

Export Citation Format

Share Document