A “uniform” heterogeneous photocatalyst: integrated p–n type CuInS2/NaInS2 nanosheets by partial ion exchange reaction for efficient H2 evolution

2015 ◽  
Vol 51 (45) ◽  
pp. 9381-9384 ◽  
Author(s):  
Peng Hu ◽  
Chee Keong Ngaw ◽  
Yee Yan Tay ◽  
Shaowen Cao ◽  
James Barber ◽  
...  

Single-crystalline-like p–n type CuInS2/NaInS2 heterogeneous nanosheets were synthesized by partial cation exchange reaction.

Nanoscale ◽  
2019 ◽  
Vol 11 (13) ◽  
pp. 5989-5997 ◽  
Author(s):  
Sampson Adjokatse ◽  
Hong-Hua Fang ◽  
Herman Duim ◽  
Maria Antonietta Loi

This study highlights the importance of a scalable blade coating technique and the ion exchange reaction in fabricating high-quality perovskite thin films.


MRS Advances ◽  
2021 ◽  
Author(s):  
Jonathan B. Junio ◽  
Prae Chirawatkul ◽  
Marlon T. Conato ◽  
Candy C. Mercado

AbstractTin (Sn2+) and strontium (Sr2+), two potential alternatives to lead (Pb2+) in perovskite formation, were explored in transforming calcium carbonate (CaCO3) into a leaving group in a cation exchange reaction. This is the first part of a sequential ion exchange process in transforming calcite into a Pb-free perovskite material for perovskite solar cell applications. Calcite, a polymorph of CaCO3, was successfully transformed into strontianite (SrCO3) through a cation exchange reaction. In the Sn substitution reaction on the other hand, no SnCO3 formation was noted. Instead, oxides of Sn were formed. The wider spaces in between Ca2+ cations in (100) orientation account for the higher atomic Sn2+ and Sr2+ concentrations as compared to (001) orientation, where the cation movement is restricted. X-ray absorption and photoelectron spectroscopies were used to investigate the ion-exchange transformation of calcite towards the formation of an intermediate carbonate material. Graphic abstract


RSC Advances ◽  
2016 ◽  
Vol 6 (105) ◽  
pp. 103215-103223 ◽  
Author(s):  
Yu-Qiao Zhang ◽  
Shun Li ◽  
Bo-Ping Zhang

A novel Bi2S3/CuS hybrid photocatalyst with a 3D hierarchical configuration was synthesized through an in situ solution-based cation exchange reaction that leads to obvious enhancements in charge separation and photocatalytic performance.


2000 ◽  
Vol 2 (19) ◽  
pp. 4461-4464 ◽  
Author(s):  
Hiroyuki Takahashi ◽  
Masato Kakihana ◽  
Yohichi Yamashita ◽  
Kiyohide Yoshida ◽  
Sigeru Ikeda ◽  
...  

2009 ◽  
Vol 1193 ◽  
Author(s):  
Haruo Sato

AbstractIn this study, the cation exchange capacity (CEC) and leached exchangeable cations (LC) of montmorillonite purified from bentonite produced in the Tsukinuno bentonite mine, Yamagata, Japan, were measured, and the exchangeable cations in the interlayer of the montmorillonite were discussed. A montmorillonite, in which the soluble minerals were completely removed, was prepared. Kunipia-F and Kunipia-P, for which both bentonites originally contain approximately 100 wt.% montmorillonite, were used as the initial material. All of the measurements were carried out in a N2 atmosphere-controlled glove-box.The CEC values of montmorillonites for both bentonites (100-110 meq/100g) were similar to data conventionally reported, and the sum of LC was also approximately in good agreement with the CEC values. The share of Na+ in the interlayer of montmorillonite calculated from the LC was about 3/4 of the sum of the LC (≍ CEC), and Mg2+ and Ca2+ occupied about 7 and 19 %, respectively. Although montmorillonite in bentonite produced in the Tsukinuno bentonite mine is known as a Na type, the sum of Ca2+ and Mg2+ occupied about 26 % of all exchangeable cations in the interlayer. Based on these data, the ion exchange reaction constant between Na+ and H+ in the interlayer of montmorillonite was calculated to be -0.07. This is nearly 2 orders of magnitude lower than data that are usually adopted.


1976 ◽  
Vol 49 (9) ◽  
pp. 2374-2376
Author(s):  
Tetsuo Morimoto ◽  
Hiromitu Naono ◽  
Kuniji N\={o}so ◽  
Yasumasa Shigetomi

1999 ◽  
Vol 64 (1) ◽  
pp. 149-156 ◽  
Author(s):  
Gabriel Čík ◽  
František Šeršeň ◽  
Alena Bumbálová

The formation of reactive oxygen species due to irradiation by a visible light of the polythiophene deposited in ZSM-5 zeolite channels in aqueous medium has been studied. Polymerization of thiophene was carried out in zeolite channels after the ion-exchange reaction of Na+ for Fe3+. By means of EPR spectroscopy, the temporarily generated 1O2 in irradiated aqueous medium was proved. The formation of O2-• was confirmed by the reduction of Fe3+-cytochrome c. Irradiation led to the water reduction to hydrogen.


2021 ◽  
Vol 9 (1) ◽  
pp. 104889
Author(s):  
Wyllamanney da S. Pereira ◽  
Fabrício B. Destro ◽  
Cipriano B. Gozzo ◽  
Edson R. Leite ◽  
Júlio C. Sczancoski

2006 ◽  
Vol 114 (1334) ◽  
pp. 861-865 ◽  
Author(s):  
Sachi TAKEZAWA ◽  
Takashi TERANISHI ◽  
Hironori ISHIKAWA ◽  
Toshiaki TOKUMITSU ◽  
Kenji TODA ◽  
...  

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