In Situ, Nonlinear Optical Probe of Surfactant Adsorption on the Surface of Microparticles in Colloids

Langmuir ◽  
2000 ◽  
Vol 16 (6) ◽  
pp. 2475-2481 ◽  
Author(s):  
Hongfei Wang ◽  
Thomas Troxler ◽  
An-Gong Yeh ◽  
Hai-Lung Dai
RSC Advances ◽  
2017 ◽  
Vol 7 (82) ◽  
pp. 52125-52132 ◽  
Author(s):  
Xuyang Zhou ◽  
Yang Chen ◽  
Jian Su ◽  
Xiaohe Tian ◽  
Yonghuang Luo ◽  
...  

NIR-PDT strategy was introduced by employing a nonlinear optical conveyor bearing strong second-harmonic generation (SHG) property. A biocompatible micellic system co-delivered the conveyor and photosensitizer for in situ NIR-PDT.


Author(s):  
A. Lastras-Martinez ◽  
I. Lara-Velazquez ◽  
R.e. Balderas-Navarro ◽  
J. Ortega-Gallegos ◽  
L.f. Lastras-Martinez

Langmuir ◽  
2000 ◽  
Vol 16 (8) ◽  
pp. 3636-3640 ◽  
Author(s):  
A. Marcia Almanza-Workman ◽  
Srini Raghavan ◽  
Roger P. Sperline

2012 ◽  
Vol 20 (22) ◽  
pp. 24623 ◽  
Author(s):  
Gaël Latour ◽  
Jean-Philippe Echard ◽  
Marie Didier ◽  
Marie-Claire Schanne-Klein

Nature ◽  
2007 ◽  
Vol 447 (7148) ◽  
pp. 1098-1101 ◽  
Author(s):  
Yuri Nakayama ◽  
Peter J. Pauzauskie ◽  
Aleksandra Radenovic ◽  
Robert M. Onorato ◽  
Richard J. Saykally ◽  
...  

1994 ◽  
Vol 2 (3) ◽  
pp. 187-197 ◽  
Author(s):  
A.K. Liao ◽  
W.M. Cross ◽  
R.M. Winter ◽  
J.J. Kellar

2019 ◽  
Vol 58 (2) ◽  
pp. 231-245 ◽  
Author(s):  
Paul R. Field ◽  
Andrew J. Heymsfield ◽  
Andrew G. Detwiler ◽  
Jonathan M. Wilkinson

AbstractHail and graupel are linked to lightning production and are important components of cloud evolution. Hail can also cause significant damage when it precipitates to the surface. The accurate prediction of the amount and location of hail and graupel and the effects on the other hydrometeor species depends upon the size distribution assumed. Here, we use ~310 km of in situ observations from flights of the South Dakota School of Mines and Technology T-28 storm-penetrating aircraft to constrain the representation of the particle size distribution (PSD) of hail. The maximum ~1-km hail water content encountered was 9 g m−3. Optical probe PSD measurements are normalized using two-moment normalization relations to obtain an underlying exponential shape. By linking the two normalizing moments through a power law, a parameterization of the hail PSD is provided based on the hail water content only. Preliminary numerical weather simulations indicate that the new parameterization produces increased radar reflectivity relative to commonly used PSD representations.


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