Controls on rare earth elements distribution from Kerala coast, southwest India over the past 2000 years

2021 ◽  
pp. 1-16
Author(s):  
M. C. Manoj ◽  
Biswajeet Thakur ◽  
Prem Raj Uddandam
Author(s):  
Robert U. Ayres ◽  
Laura Talens Peiró

In the last few decades, progress in electronics, especially, has resulted in important new uses for a number of geologically rare metals, some of which were mere curiosities in the past. Most of them are not mined for their own sake (gold, the platinum group metals and the rare Earth elements are exceptions) but are found mainly in the ores of the major industrial metals, such as aluminium, copper, zinc and nickel. We call these major metals ‘attractors’ and the rare accompanying metals ‘hitch-hikers’. The key implication is that rising prices do not necessarily call forth greater output because that would normally require greater output of the attractor metal. We trace the geological relationships and the functional uses of these metals. Some of these metals appear to be irreplaceable in the sense that there are no known substitutes for them in their current functional uses. Recycling is going to be increasingly important, notwithstanding a number of barriers.


2019 ◽  
Vol 157 ◽  
pp. 103505
Author(s):  
Mariem Bouabdallah ◽  
Sarra Elgharbi ◽  
Karima Horchani-Naifer ◽  
Donatella Barca ◽  
Nabil Fattah ◽  
...  

2019 ◽  
Vol 98 ◽  
pp. 03001
Author(s):  
Ekaterina Kazak ◽  
Natalia Kharitonova ◽  
Yana Sorokoumova

The rare-earth elements and yttrium (REY) distribution data with depth in the Bazhenov formation are given for the case of the one well in the Nizhnevartovsk arch of the Western Siberia, Russian Federation. According to the correlation analysis, it was found that REY (mainly LREE) is concentrated in apatite more than in clays or plagioclase, while HREE is preferably accumulated in clay minerals. It was estimated that the water extracts from the Bazhenov formation contain REY up to 0.014 ppb, while LREE is contained in 3.6 times more than HREE. An attempt to estimate the REY content in the pore water of the Bazhenov formation was made using water extract composition data.


2019 ◽  
Vol 524 ◽  
pp. 11-36 ◽  
Author(s):  
V.Q. Pham ◽  
M. Grenier ◽  
S. Cravatte ◽  
S. Michael ◽  
S. Jacquet ◽  
...  

2019 ◽  
Vol 157 ◽  
pp. 103514
Author(s):  
Obialo Solomon Onwuka ◽  
Nuhu Degree Umar ◽  
Olufemi Victor Omonona ◽  
Ibrahim Giza Idris

2019 ◽  
Vol 2 (1) ◽  
pp. 141-148
Author(s):  
Dmitry Novikov ◽  
Anatoly Chernykh ◽  
Fedor Dultsev

The results of the analysis of rare earth elements distribution in groundwater of J1 reservoir of the Verkh-Tarka oil field are reported for the first time. It was established that groundwater with Cl Na composition are predominate, with a value of total mineralization from 24.7 up to 48.9 g/dm3. The content of REE ranges from 3.72 to 30.49 µg/dm3 with an average of 13.61 µg/dm3. The highest concentrations are observed (µg/dm3) in La (up to 20.8), Eu (up to 7.9), Gd (up to 1.8) and Dy (up to 0.65). The level of dissolved REE is determined by their distribution in the water-bearing sandstones. Migration of rare-earth elements is carried out in the form of free ions and hydroxide complexes.


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