Imaging reconstruction through long-range scattering media by using deep learning

Author(s):  
Bochao Zhang ◽  
Fang Liu ◽  
Baoxing Xiong ◽  
Fan Gao ◽  
Xiang Zhang ◽  
...  
Author(s):  
Elena Morotti ◽  
Davide Evangelista ◽  
Elena Loli Piccolomini

Deep Learning is developing interesting tools which are of great interest for inverse imaging applications. In this work, we consider a medical imaging reconstruction task from subsampled measurements, which is an active research field where Convolutional Neural Networks have already revealed their great potential. However, the commonly used architectures are very deep and, hence, prone to overfitting and unfeasible for clinical usages. Inspired by the ideas of the green-AI literature, we here propose a shallow neural network to perform an efficient Learned Post-Processing on images roughly reconstructed by the filtered backprojection algorithm. The results obtained on images from the training set and on unseen images, using both the non-expensive network and the widely used very deep ResUNet show that the proposed network computes images of comparable or higher quality in about one fourth of time.


Author(s):  
David Vint ◽  
Gaetano Di Caterina ◽  
John J. Soraghan ◽  
Robert A. Lamb ◽  
David Humphreys

1983 ◽  
Vol 73 (1) ◽  
pp. 125-142
Author(s):  
William Menke ◽  
Paul G. Richards

abstract We compare seismograms produced through the use of analog models of scattering and nonscattering Earth structure to access the effect of lateral heterogeneities on the horizontal propagation of P waves. Our results are applicable to propagation out to 16° and to periods as short as 5 sec. We find that layers of scatterers within the mantle near the turning points of P waves can cause these phases to have long coda similar in certain respects to the coda observed in long-range Pn. The overall appearance of this coda is similar to that produced in laterally homogeneous models that include low-velocity crustal material near their surfaces. Scatterers at shallower depths in the mantle or crust have a different effect. Those in very uppermost mantle seem to suppress the horizontal propagation of P waves while those in the crust have very little overall effect, at least at the perod range we studied. We also find that the scatterers have an amplifying effect on the horizontal propagation of the very longest periods (>20 sec), an effect that may be related to the scattering-controlled boundary waves discovered by Biot (1968).


Author(s):  
Milan Koirala ◽  
Raktim Sarma ◽  
Hui Cao ◽  
Alexey Yamilov

2020 ◽  
Vol 477 ◽  
pp. 126341
Author(s):  
Qiongyao Li ◽  
Jun Zhao ◽  
Yanzhu Zhang ◽  
Xuetian Lai ◽  
Ziyang Chen ◽  
...  

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