scholarly journals The Impact of Physiological Motion on Tissue Tracking During Radiation Force Imaging

2007 ◽  
Vol 33 (7) ◽  
pp. 1149-1166 ◽  
Author(s):  
Brian J. Fahey ◽  
Mark L. Palmeri ◽  
Gregg E. Trahey
2016 ◽  
Vol 60 (5) ◽  
pp. 587-592 ◽  
Author(s):  
Nicole Harris ◽  
David Nadebaum ◽  
Michael Christie ◽  
Alexandra Gorelik ◽  
Amanda Nicoll ◽  
...  

2014 ◽  
Vol 41 (6Part8) ◽  
pp. 181-181 ◽  
Author(s):  
S Yip ◽  
J Rottmann ◽  
R Berbeco

2014 ◽  
Vol 41 (6Part1) ◽  
pp. 061702 ◽  
Author(s):  
Stephen Yip ◽  
Joerg Rottmann ◽  
Ross Berbeco

2020 ◽  
Vol 26 ◽  
pp. 100453
Author(s):  
Hideki Koike ◽  
Satoru Kishi ◽  
Naoki Hosoda ◽  
Shuhei Takemoto ◽  
Daijiro Tomii ◽  
...  

Author(s):  
Sylviane Hanquinet ◽  
Céline Habre ◽  
Méryle Laurent ◽  
Mehrak Anooshiravani ◽  
Seema Toso

Abstract Background Acoustic radiation force impulse (ARFI) imaging is a noninvasive ultrasound elastography technique for evaluating tissue stiffness. The association of liver and spleen stiffness provides additional information in the assessment of portal hypertension. The technique and normal values of spleen stiffness by point shear wave elastography (p-SWE) in pediatrics have not been well documented. Objective Our aim is to describe the feasibility and normal ARFI elastography values in the spleen for healthy children and to compare measurements in two different probe positions (the axial and sagittal planes). Materials and methods Spleen p-SWE using ARFI values were measured with a 6C1 probe in 102 healthy children (age range: 8 weeks to 17 years) divided into four age groups. An average of nine (standard deviation: two) spleen stiffness measurements were taken during free breathing in each plane (axial and sagittal). The impact of age and measurement plane in the spleen was analyzed using multivariate models. Results There was no significant difference in spleen stiffness values taken at different ages, with an average of the medians of 2.43±0.31 m/s. There was no significant difference based on probe orientation: sagittal plane (median: 2.46±0.29 m/s) and axial plane (median: 2.43±0.32 m/s) with Student’s t-test P=0.18. The mean depth of measurement varied between 2.3 cm and 3.7 cm, according to age. Conclusion Normal spleen stiffness values using ARFI imaging in children do not vary with age and correspond to a median of 2.43 m/s. No significant difference was found when using different probe positions.


Micromachines ◽  
2022 ◽  
Vol 13 (1) ◽  
pp. 113
Author(s):  
Xiufang Liu ◽  
Wenjun Zhang ◽  
Yanshu Jing ◽  
Shasha Yi ◽  
Umar Farooq ◽  
...  

Sonoporation employs ultrasound accompanied by microbubble (MB) cavitation to induce the reversible disruption of cell membranes and has been exploited as a promising intracellular macromolecular delivery strategy. Due to the damage to cells resulting from strong cavitation, it is difficult to balance efficient delivery and high survival rates. In this paper, a traveling surface acoustic wave (TSAW) device, consisting of a TSAW chip and a polydimethylsiloxane (PDMS) channel, was designed to explore single-cell sonoporation using targeted microbubbles (TMBs) in a non-cavitation regime. A TSAW was applied to precisely manipulate the movement of the TMBs attached to MDA-MB-231 cells, leading to sonoporation at a single-cell level. The impact of input voltage and the number of TMBs on cell sonoporation was investigated. In addition, the physical mechanisms of bubble cavitation or the acoustic radiation force (ARF) for cell sonoporation were analyzed. The TMBs excited by an ARF directly propelled cell membrane deformation, leading to reversible perforation in the cell membrane. When two TMBs adhered to the cell surface and the input voltage was 350 mVpp, the cell sonoporation efficiency went up to 83%.


1962 ◽  
Vol 14 ◽  
pp. 415-418
Author(s):  
K. P. Stanyukovich ◽  
V. A. Bronshten

The phenomena accompanying the impact of large meteorites on the surface of the Moon or of the Earth can be examined on the basis of the theory of explosive phenomena if we assume that, instead of an exploding meteorite moving inside the rock, we have an explosive charge (equivalent in energy), situated at a certain distance under the surface.


1962 ◽  
Vol 14 ◽  
pp. 169-257 ◽  
Author(s):  
J. Green

The term geo-sciences has been used here to include the disciplines geology, geophysics and geochemistry. However, in order to apply geophysics and geochemistry effectively one must begin with a geological model. Therefore, the science of geology should be used as the basis for lunar exploration. From an astronomical point of view, a lunar terrain heavily impacted with meteors appears the more reasonable; although from a geological standpoint, volcanism seems the more probable mechanism. A surface liberally marked with volcanic features has been advocated by such geologists as Bülow, Dana, Suess, von Wolff, Shaler, Spurr, and Kuno. In this paper, both the impact and volcanic hypotheses are considered in the application of the geo-sciences to manned lunar exploration. However, more emphasis is placed on the volcanic, or more correctly the defluidization, hypothesis to account for lunar surface features.


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