Hierarchical photoanode of rutile TiO2 nanorods coupled with anatase TiO2 nanosheets array for photoelectrochemical application

2016 ◽  
Vol 680 ◽  
pp. 206-211 ◽  
Author(s):  
Huizhen Yao ◽  
Wuyou Fu ◽  
Li Liu ◽  
Xue Li ◽  
Dong Ding ◽  
...  
Keyword(s):  
Anatase Tio2 ◽  
Tio2 Nanorods ◽  
Rutile Tio2 ◽  
Tio2 Nanosheets

Controlling the density of hydrothermally grown rutile TiO2 nanorods on anatase TiO2 films

2019 ◽  
Vol 15 ◽  
pp. 141-147 ◽  
Author(s):  
Julian Kalb ◽  
Alena Folger ◽  
Eugen Zimmermann ◽  
Melanie Gerigk ◽  
Bastian Trepka ◽  
...  
Keyword(s):  
Anatase Tio2 ◽  
Tio2 Nanorods ◽  
Tio2 Films ◽  
Rutile Tio2

Growth of rutile TiO2 nanorods on anatase TiO2 thin films on Si-based substrates

2011 ◽  
Vol 26 (13) ◽  
pp. 1646-1652 ◽  
Author(s):  
Jinsong Wu ◽  
Shihhan Lo ◽  
Kai Song ◽  
Baiju K. Vijayan ◽  
Wenyun Li ◽  
...  
Keyword(s):  
Thin Films ◽  
Anatase Tio2 ◽  
Tio2 Nanorods ◽  
Tio2 Thin Films ◽  
Rutile Tio2 ◽  
Image Position

Abstract

Effect of Chemical Lithium Insertion into Rutile TiO2 Nanorods

2009 ◽  
Vol 113 (32) ◽  
pp. 14567-14574 ◽  
Author(s):  
M. Vijayakumar ◽  
Sebastien Kerisit ◽  
Chongmin Wang ◽  
Zimin Nie ◽  
Kevin M. Rosso ◽  
...  
Keyword(s):  
Tio2 Nanorods ◽  
Lithium Insertion ◽  
Rutile Tio2

Aligned rutile TiO2 nanorods: Facile synthesis and field emission

2013 ◽  
Vol 59 ◽  
pp. 187-195 ◽  
Author(s):  
Dong-Sheng Li ◽  
Jian-Biao Chen ◽  
Cheng-Wei Wang ◽  
Wei-Dong Zhu ◽  
Ling Zhang ◽  
...  
Keyword(s):  
Field Emission ◽  
Tio2 Nanorods ◽  
Facile Synthesis ◽  
Rutile Tio2

scholarly journals Nano-Sized Minerals from Lower Cretaceous Sandstones in Israel Observed by Transmission Electron Microscopy (TEM)

2021 ◽  
Author(s):  
Nurit Taitel-Goldman ◽  
Vladimir Ezersky
Keyword(s):  
Clay Minerals ◽  
Iron Oxides ◽  
Lower Cretaceous ◽  
Fine Fraction ◽  
Anatase Tio2 ◽  
Rutile Tio2 ◽  
Transmission Electron ◽  
Quartz Arenite ◽  
Dark Violet ◽  
Hematite Fe2o3

Fine fraction in quartz arenite sandstones from Lower Cretaceous Hatira formation in Israel was observed by Transmission electron microscope (TEM). Samples were collected from Hatira and Ramon craters located in southern part of Israel and from Manara cliff from the northern part of Israel. The additional phases cause yellow, red, dark red and dark violet colors of the layered sandstones. The motivation was to identify the minerals of the fine factions that cause the variations in the colors. The minerals observed were clay minerals, mainly kaolinite (Al4Si4O20(OH)8), some illite (K0.65Al2.0[Al0.65Si3.35O10](OH)2) and smectite. Iron oxides were goethite (FeOOH) and hematite (Fe2O3), Titanium-iron oxides observed was ilmenite (FeTiO3), and Titanium-oxides were rutile (TiO2), and anatase (TiO2). Sulphates observed were jarosite (KFe3(SO4)2(OH)6) and alunite (KAl3(SO4)2(OH)6). Some of the hematite was formed by recrystallization of goethite. Ilmenite disintegrated into small iron oxides mainly hematite. Euhedral to sub-hedral rutile (TiO2) and anatase (TiO2) were preserved in clay-minerals. Crystals of alunite and jarosite were observed in sandstones in both craters. They probably crystallized due to some transgression of the Thetis Sea.

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