Improvement of monodispersity and shape symmetry of silica shell for PbS quantum dots by introducing surface silanization and adjusting reverse micelle size

Author(s):  
Kohki MUKAI ◽  
Kosuke Ikeda ◽  
Reo Hatta

Abstract Increasing the thickness of the quantum dot silica coating layer reduces monodispersity and shape symmetry. This paper reports three effective ways to solve this problem and achieve a large silica-coated QDs, i.e., proper silanization on the QD surface, control of reverse micelle size by adjusting the amount of QD solvent, and two-step formation of silica shell. Proper substitution of ligands on the QD surface in the early stages of silica shell formation was important for uniform coating reaction. An amount of toluene as QD solvent determined the size of reverse micelles during the silica shell formation. There was an optimum combination of inverse micelle size and silica shell size to obtain silica-coated QDs with good monodispersity and high shape symmetry. We succeeded in growing the thick silica shell with expanding reverse micelle size by additionally supplying toluene with the raw material using the optimum silica-coated QDs as growth nucleus

2016 ◽  
Vol 74 (4) ◽  
pp. 941-954 ◽  
Author(s):  
Christina A. Frieder ◽  
Scott L. Applebaum ◽  
T.-C. Francis Pan ◽  
Dennis Hedgecock ◽  
Donal T. Manahan

Abstract Physiological increases in energy expenditure frequently occur in response to environmental stress. Although energy limitation is often invoked as a basis for decreased calcification under ocean acidification, energy-relevant measurements related to this process are scant. In this study we focus on first-shell (prodissoconch I) formation in larvae of the Pacific oyster, Crassostrea gigas. The energy cost of calcification was empirically derived to be ≤ 1.1 µJ (ng CaCO3)−1. Regardless of the saturation state of aragonite (2.77 vs. 0.77), larvae utilize the same amount of total energy to complete first-shell formation. Even though there was a 56% reduction of shell mass and an increase in dissolution at aragonite undersaturation, first-shell formation is not energy limited because sufficient endogenous reserves are available to meet metabolic demand. Further studies were undertaken on larvae from genetic crosses of pedigreed lines to test for variance in response to aragonite undersaturation. Larval families show variation in response to ocean acidification, with loss of shell size ranging from no effect to 28%. These differences show that resilience to ocean acidification may exist among genotypes. Combined studies of bioenergetics and genetics are promising approaches for understanding climate change impacts on marine organisms that undergo calcification.


1966 ◽  
pp. 169-188 ◽  
Author(s):  
Joyce C. Lewin ◽  
Bernhard E. Reimann ◽  
William F. Busby ◽  
Benjamin E. Volcani
Keyword(s):  

Planta ◽  
1976 ◽  
Vol 130 (2) ◽  
pp. 159-167 ◽  
Author(s):  
W. M. Darley ◽  
C. W. Sullivan ◽  
B. E. Volcani

Planta ◽  
1968 ◽  
Vol 82 (3) ◽  
pp. 280-292 ◽  
Author(s):  
J. Coombs ◽  
B. E. Volcani

Langmuir ◽  
2012 ◽  
Vol 28 (25) ◽  
pp. 9267-9274 ◽  
Author(s):  
Hoorshad Fathi ◽  
James P. Kelly ◽  
Victor R. Vasquez ◽  
Olivia A. Graeve

Langmuir ◽  
2011 ◽  
Vol 27 (19) ◽  
pp. 11845-11851 ◽  
Author(s):  
Mary E. Parent ◽  
Jun Yang ◽  
Yoocharn Jeon ◽  
Michael F. Toney ◽  
Zhang-Lin Zhou ◽  
...  
Keyword(s):  

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