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particle imaging velocimetry (piv) software  (MathWorks Inc)


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    MathWorks Inc particle imaging velocimetry (piv) software
    Particle Imaging Velocimetry (Piv) Software, supplied by MathWorks Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/particle+image+velocimetry+(piv)+software/particle+image+velocimetry/bio_rxiv__2024__05__13__593501-179-18-25
    Average 90 stars, based on 1 article reviews
    particle imaging velocimetry (piv) software - by Bioz Stars, 2026-09
    90/100 stars

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    Related Articles

    other:

    Article Title: Cell segregation via differential collision modes between heterotypic cell populations
    Article Snippet: Images were acquired every 10 min for 36 h. To measure the cells’ velocity field, stabilized images were analyzed by particle image velocimetry (PIV) software provided by MATLAB.

    Article Title: Combinational concentration gradient confinement through stagnation flow.
    Article Snippet: Concentration gradient generation in microfluidics is typically constrained by two conflicting mass transport requirements: short characteristic times (τ) for precise temporal control of concentration gradients but at the expense of high flow rates and hence, high flow shear stresses (σ).. To decouple the limitations from these parameters, here we propose the use of stagnation flows to confine concentration gradients within large velocity gradients that surround the stagnation point.. We developed a modified cross-slot (MCS) device capable of feeding binary and combinational concentration sources in stagnation flows.

    Article Title: Electric field–induced migration and intercellular stress alignment in a collective epithelial monolayer
    Article Snippet: Postprocessed images were then analyzed by custom particle image velocimetry (PIV) software written in MATLAB for the measurement of the velocity field.

    Article Title: Transport and trapping of dust particles in a potential well created by inductively coupled diffused plasmas.
    Article Snippet: The series of images are then stored in a high-speed computer and later analyzed with the help of Matlab based freely available Particle Image Velocimetry (PIV) software.

    Article Title: Anatomy of the Bezymianny volcano merely before an explosive eruption on 20.12.2017
    Article Snippet: Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python.

    Article Title: Methods for predicting mammalian embryo viability
    Article Snippet: Particle Image Velocimetry (PIV) Analysis DIC images of fertilized eggs were analyzed using custom written software in MATLAB (The Mathworks Inc., Natick, Mass., USA) using algorithms adapted from MatPIV v1.6.150.

    Article Title: Detailed observations reveal the genesis and dynamics of destructive debris-flow surges
    Article Snippet: The field data were processed using the following open-source software: • PIV-Lab https://www.mathworks.com/matlabcentral/fileexchange/27659-pivlab-particle-image-velocimetry-piv-tool-with-gui .

    Software:

    Article Title: Long-range ordered vorticity patterns in living tissue induced by cell division
    Article Snippet: .. We used the PIVlab software package ( www.mathworks.com/matlabcentral/fileexchange/27659-pivlab-time-resolved-particle-image-velocimetry-piv-tool ) for MATLAB (The MathWorks, Natick, MA) and used an interrogation area of 15.4 × 15.4 μm 2 corresponding to 24 × 24 pixels 2 . ..



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    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image <t>Velocimetry</t> <t>(PIV)</t> software <t>PIVlab,</t> plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).
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    Image Search Results


    TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).

    Journal: Scientific Reports

    Article Title: Anatomy of the Bezymianny volcano merely before an explosive eruption on 20.12.2017

    doi: 10.1038/s41598-021-81498-9

    Figure Lengend Snippet: TerraSAR-X amplitude imagery of Bezymianny. ( a ) Surface reflectivity of the radar signal on 07 December 2017. Arrows refer to the azimuth and Line-of-Sight (LOS) direction of the sattelite. Inset indicates the area zoomed in for ( a – d ). ( b ) Reflectivity on 18 December 2017. Dark shadow regions due to opening tensile fractures (20 m wide, N–S extent, approx. 100 m) that appeared two days before the 20 December 2017 eruption. ( c ) Amplitude changes shown with red and green colored pixels. Please note the concentric pattern (white dashed lines) of newly emerged radar shadows. ( d ) Pixel offsets indicate the motion of displacement related to the opening of the shadow casting fractures and summit uplift towards LOS. Images a-c generated using GAMMA Remote Sensing software as well as Matplotlib, OpenCV libraries in Python. Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python. TerraSAR-X (TSX) spotlight-mode satellite images available from German Aerospace Center (DLR).

    Article Snippet: Image d: displacements generated with the Matlab based Particle Image Velocimetry (PIV) software PIVlab, plotted with Python.

    Techniques: Generated, Software