The Influence of Incident-Light Field Distribution on High-Speed Response Characteristic of UTC Photodetector

Author(s):  
Chaozheng Xiao ◽  
Yongqing Huang ◽  
Huayun Zhi ◽  
Huijuan Niu ◽  
Xiaofeng Duan ◽  
...  
2014 ◽  
Vol 51 (11) ◽  
pp. 112301
Author(s):  
王天阳 Wang Tianyang ◽  
徐兆鹏 Xu Zhaopeng ◽  
朱化凤 Zhu Huafeng ◽  
刘佩 Liu Pei ◽  
叶春伟 Ye Chunwei ◽  
...  

2000 ◽  
Vol 184 (5-6) ◽  
pp. 391-396 ◽  
Author(s):  
A.V. Tarasishin ◽  
S.A. Magnitskii ◽  
V.A. Shuvaev ◽  
A.M. Zheltikov

2014 ◽  
Vol 45 (1) ◽  
pp. 1463-1464 ◽  
Author(s):  
Shunsuke Kobayashi ◽  
Kiyofumi Takeuchi ◽  
Masakazu Kaneoya ◽  
Kunihiko Kotani ◽  
Haruyoshi Takatsu

1982 ◽  
Vol 18 (22) ◽  
pp. 945 ◽  
Author(s):  
Y. Matsushima ◽  
S. Akiba ◽  
K. Sakai ◽  
Y. Kushiro ◽  
Y. Noda ◽  
...  

2007 ◽  
Vol 127 (9) ◽  
pp. 942-949 ◽  
Author(s):  
Toru Hayano ◽  
Isao Shibutani ◽  
Kiyoshi Ohishi ◽  
Toshimasa Miyazaki ◽  
Daiichi Koide ◽  
...  

2011 ◽  
Vol 23 (9) ◽  
pp. 2346-2350
Author(s):  
刘立力 Liu Lili ◽  
达争尚 Da Zhengshang ◽  
田新锋 Tian Xinfeng ◽  
段亚轩 Duan Yaxuan ◽  
李东坚 Li Dongjian ◽  
...  

Sensors ◽  
2019 ◽  
Vol 19 (15) ◽  
pp. 3399 ◽  
Author(s):  
Jheng-Jie Liu ◽  
Wen-Jeng Ho ◽  
June-Yan Chen ◽  
Jian-Nan Lin ◽  
Chi-Jen Teng ◽  
...  

This paper presents a novel front-illuminated InAlAs/InGaAs separate absorption, grading, field-control and multiplication (SAGFM) avalanche photodiodes (APDs) with a mesa-structure for high speed response. The electric fields in the InAlAs-multiplication layer and InGaAs-absorption layer enable high multiplication gain and high-speed response thanks to the thickness and concentration of the field-control and multiplication layers. A mesa active region of 45 micrometers was defined using a bromine-based isotropic wet etching solution. The side walls of the mesa were subjected to sulfur treatment before being coated with a thick polyimide layer to reduce current leakage, while lowering capacitance and increasing response speeds. The breakdown voltage (VBR) of the proposed SAGFM APDs was approximately 32 V. Under reverse bias of 0.9 VBR at room temperature, the proposed device achieved dark current of 31.4 nA, capacitance of 0.19 pF and multiplication gain of 9.8. The 3-dB frequency response was 8.97 GHz and the gain-bandwidth product was 88 GHz. A rise time of 42.0 ps was derived from eye-diagrams at 0.9 VBR. There was notable absence of intersymbol-interference and the signals remained error-free at data-rates of up to 12.5 Gbps.


2021 ◽  
Vol 480 ◽  
pp. 126467
Author(s):  
Jishi Cui ◽  
Tiantian Li ◽  
Fenghe Yang ◽  
Wenjing Cui ◽  
Hongmin Chen

2018 ◽  
Vol 8 (12) ◽  
pp. 2693 ◽  
Author(s):  
Philippe Massicotte ◽  
Guislain Bécu ◽  
Simon Lambert-Girard ◽  
Edouard Leymarie ◽  
Marcel Babin

The vertical diffuse attenuation coefficient for downward plane irradiance ( K d ) is an apparent optical property commonly used in primary production models to propagate incident solar radiation in the water column. In open water, estimating K d is relatively straightforward when a vertical profile of measurements of downward irradiance, E d , is available. In the Arctic, the ice pack is characterized by a complex mosaic composed of sea ice with snow, ridges, melt ponds, and leads. Due to the resulting spatially heterogeneous light field in the top meters of the water column, it is difficult to measure at single-point locations meaningful K d values that allow predicting average irradiance at any depth. The main objective of this work is to propose a new method to estimate average irradiance over large spatially heterogeneous area as it would be seen by drifting phytoplankton. Using both in situ data and 3D Monte Carlo numerical simulations of radiative transfer, we show that (1) the large-area average vertical profile of downward irradiance, E d ¯ ( z ) , under heterogeneous sea ice cover can be represented by a single-term exponential function and (2) the vertical attenuation coefficient for upward radiance ( K L u ), which is up to two times less influenced by a heterogeneous incident light field than K d in the vicinity of a melt pond, can be used as a proxy to estimate E d ¯ ( z ) in the water column.


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