Effect of binary pseudo-random grating and step on system transfer function calibration of interferometric measurement system

2015 ◽  
Vol 27 (7) ◽  
pp. 71010
Author(s):  
邓燕 Deng Yan ◽  
王翔峰 Wang Xiangfeng ◽  
嵇保健 Ji Baojian ◽  
石琦凯 Shi Qikai
2009 ◽  
Vol 186 ◽  
pp. 012080
Author(s):  
Hirokatsu Yumoto ◽  
Hidekazu Mimura ◽  
Soichiro Handa ◽  
Takashi Kimura ◽  
Satoshi Matsuyama ◽  
...  

Instruments ◽  
2020 ◽  
Vol 4 (3) ◽  
pp. 22
Author(s):  
Yu-Chung Lin ◽  
Joseph V. Sinfield

The emergence of a wide variety of relatively low-cost compact spectrometers has led to an increase in the use of spectroscopic techniques by researchers in a broad array of fields beyond those that have traditionally employed these analytical methods. While the fundamental elements and functions of Raman systems are generally consistent, the specific components that compose a system may vary in number, design, and configuration, and researchers often modify off-the-shelf spectrometers for unique applications. Understanding the effect of instrument design and components on acquired information is thus crucial and provides the prospect to optimize the system to individual needs and to properly compare results obtained with different systems while also reducing the potential for unintended misinterpretation of data. This paper provides a practical treatment of the influences in a typical compact spectroscopy system that can impact the extent to which the output of the system is representative of the observed environment, a relationship that in measurement science is classically termed the system transfer function. For clarity, the transfer function is developed in terms of traditional Raman output parameters, namely intensity, wavelength, and time.


Geophysics ◽  
1982 ◽  
Vol 47 (7) ◽  
pp. 1047-1058 ◽  
Author(s):  
D. P. Blair

Rise times for seismic pulses in rock are discussed for both nearly constant Q (NCQ) and constant Q (CQ) theories of pulse attenuation. The frequency content of the NCQ pulse is examined in detail. Frequencies close to the megahertz region are shown to have a significant contribution to the rise time of pulses a meter or so from an impulsive source. Hence, the measurement of such rise times is significantly influenced by the frequency response of the measurement system itself. In giving a numerical assessment of the system influence, I propose a model for a general system transfer function. The effect of such a system on the measurement of rise times of seismic pulses is then obtained by convolving the system impulse response with the given seismic pulse. For even the most broad‐band seismic measurement systems presently available, rise time measurements made especially within 10 m or so of an impulsive source show a large contribution dependent upon the rise time of the measurement system itself.


2007 ◽  
Vol 78 (2) ◽  
pp. 025104 ◽  
Author(s):  
H. Olkkonen ◽  
J. T. Olkkonen

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