Photoactive Nanocrystals by Low-Temperature Welding of Copper Sulfide Nanoparticles and Indium Sulfide Nanosheets

ChemSusChem ◽  
2014 ◽  
Vol 7 (12) ◽  
pp. 3290-3294 ◽  
Author(s):  
Hui Min Lim ◽  
Jia Yi Tan ◽  
Sudip K. Batabyal ◽  
Shlomo Magdassi ◽  
Subodh G. Mhaisalkar ◽  
...  
ChemSusChem ◽  
2014 ◽  
Vol 7 (12) ◽  
pp. 3549-3549
Author(s):  
Hui Min Lim ◽  
Jia Yi Tan ◽  
Sudip K. Batabyal ◽  
Shlomo Magdassi ◽  
Subodh G. Mhaisalkar ◽  
...  

2007 ◽  
Vol 61 (28) ◽  
pp. 5029-5032 ◽  
Author(s):  
Jing Zou ◽  
Jianxue Zhang ◽  
Baohua Zhang ◽  
Pingtang Zhao ◽  
KaiXun Huang

2020 ◽  
Vol 25 ◽  
pp. 101188 ◽  
Author(s):  
Dongjing Liu ◽  
Zhen Zhang ◽  
Jiang Wu ◽  
Chaoen Li

2019 ◽  
Vol 49 (1) ◽  
pp. 25-29
Author(s):  
L. A. BERNARDEZ ◽  
L.R. P. DE ANDRADE LIMA ◽  
L.E. L. DE OLIVEIRA

The bioleaching of copper ore from the Caraiba Mine was assessed. A microorganism, Acidiothiobacillus ferrooxidans, was isolated from samples collected directly in acid mining drainage in a gold mine tailings pound and used in the bioleaching of the copper sulfide ore. This ore is composed mainly of 28% of oxidized species, 43% of secondary sulfides and 24% of primary sulfide. The shaking flasks experiments with the Caraiba ore showed copper chemical leaching of about 37% and copper bioleaching of about 60% within 60 days at low temperature and native microorganism.


2021 ◽  
Vol 2 (1) ◽  
Author(s):  
Katherine D. Burgess ◽  
Rhonda M. Stroud

AbstractSamples from asteroid 25143 Itokawa returned by the Hayabusa mission have been identified as LL4-6 ordinary chondrite materials and have shown it to be a rubble pile that aggregated after break-up of a parent body. Here we investigate particle RB-CV-0038 from the Itokawa regolith using scanning and transmission electron microscopy and energy dispersive spectroscopy. We identify a cubanite-chalcopyrite-troilite-pyrrhotite assemblage, the phases and structure of which are indicative of low-temperature, aqueous alteration. Cubanite is stable only at temperatures below around 250 °C and has thus far only been identified in CI carbonaceous chondrites and the comet 81P/Wild2 sample suite. Chalcopyrite is also very rare in the meteorite record and is found mostly in R chondrites and some CK chondrites. Because the Itokawa parent body experienced significant thermal alteration with little evidence of low-temperature equilibration or aqueous alteration, we propose that the assemblage we identify is most likely exogenous and represents a component of an impacting body.


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