Characterization of optical properties on large-size PbWO4:Y crystals grown by modified Bridgman method

2006 ◽  
Vol 28 (3) ◽  
pp. 266-270
Author(s):  
Jianjun Xie ◽  
Hui Yuan ◽  
Peizhi Yang ◽  
Jingying Liao ◽  
Zhiwen Yin
RSC Advances ◽  
2014 ◽  
Vol 4 (53) ◽  
pp. 27830-27836 ◽  
Author(s):  
Shanpeng Wang ◽  
Guandong Liu ◽  
Qiong Shi ◽  
Xiang Zhang ◽  
Xixia Zhang ◽  
...  

A promising MIR NLO crystal LiGa3Te5 with large size (Ø16 mm × 50 mm) and wide transparency range (0.9–25 μm) was grown by modified Bridgman method.


2017 ◽  
Vol 712 ◽  
pp. 857-862 ◽  
Author(s):  
Min Jin ◽  
Hezhu Shao ◽  
Haoyang Hu ◽  
Debo Li ◽  
Hui Shen ◽  
...  

CrystEngComm ◽  
2019 ◽  
Vol 21 (16) ◽  
pp. 2614-2619 ◽  
Author(s):  
Jie Qiao ◽  
Qijun Liang ◽  
Shanpeng Wang ◽  
Xixi Xiong ◽  
Xutang Tao ◽  
...  

High quality and large size nonlinear optical LiInS2 (LIS) crystals were successfully grown by the optimized seeded Bridgman method.


2020 ◽  
Vol 12 (23) ◽  
pp. 3946
Author(s):  
Pasquale Sellitto ◽  
Silvia Bucci ◽  
Bernard Legras

Clouds in the tropics have an important role in the energy budget, atmospheric circulation, humidity, and composition of the tropical-to-global upper-troposphere–lower-stratosphere. Due to its non-sun-synchronous orbit, the Cloud–Aerosol Transport System (CATS) onboard the International Space Station (ISS) provided novel information on clouds from space in terms of overpass time in the period of 2015–2017. In this paper, we provide a seasonally resolved comparison of CATS characterization of high clouds (between 13 and 18 km altitude) in the tropics with well-established CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observation) data, both in terms of clouds’ occurrence and cloud optical properties (optical depth). Despite the fact that cloud statistics for CATS and CALIOP are generated using intrinsically different local overpass times, the characterization of high clouds occurrence and optical properties in the tropics with the two instruments is very similar. Observations from CATS underestimate clouds occurrence (up to 80%, at 18 km) and overestimate the occurrence of very thick clouds (up to 100% for optically very thick clouds, at 18 km) at higher altitudes. Thus, the description of stratospheric overshoots with CATS and CALIOP might be different. While this study hints at the consistency of CATS and CALIOP clouds characterizaton, the small differences highlighted in this work should be taken into account when using CATS for estimating cloud properties and their variability in the tropics.


2015 ◽  
Vol 54 (31) ◽  
pp. 9082 ◽  
Author(s):  
R. Márquez-Islas ◽  
C. Sánchez-Pérez ◽  
A. García-Valenzuela
Keyword(s):  

2021 ◽  
pp. 126303
Author(s):  
Masaru Nakamura ◽  
Hiroaki Nakamura ◽  
Kiyoshi Shimamura ◽  
Naoki Ohashi

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