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Object Research Systems (ORS) Inc dragonfly pro software, version 2020.2 [windows
2D images from the center of the sample along the vertical axis, and 3D visualizations of the interior for the geo-architected samples after 6 full days of dehydration. The pixel edge length resolution is \documentclass[12pt]{minimal}
				\usepackage{amsmath}
				\usepackage{wasysym} 
				\usepackage{amsfonts} 
				\usepackage{amssymb} 
				\usepackage{amsbsy}
				\usepackage{mathrsfs}
				\usepackage{upgreek}
				\setlength{\oddsidemargin}{-69pt}
				\begin{document}$$\sim 40\; \upmu \text{m}$$\end{document} ∼ 40 μ m and the average radius is 19.05 mm. All samples contain non-connected pores (displayed in blue) which are shown only for the reference sample ( a ) and the LICI sample ( b ). Clay inclusions are displayed in brown. All cracks are displayed in red, as shown for the MSCS sample ( c ) and the CB-SK10 sample ( d ). Cracks are only observed in samples containing localized or distributed clay which can result in a 40% reduction in material strength (a comparison between the reference and the CB-SK10 sample). Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .
Dragonfly Pro Software, Version 2020.2 [Windows, supplied by Object Research Systems (ORS) 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/result/dragonfly pro software, version 2020.2 [windows/product/Object Research Systems (ORS) Inc
Average 90 stars, based on 1 article reviews
dragonfly pro software, version 2020.2 [windows - by Bioz Stars, 2026-06
90/100 stars

Images

1) Product Images from "The effect of differential mineral shrinkage on crack formation and network geometry"

Article Title: The effect of differential mineral shrinkage on crack formation and network geometry

Journal: Scientific Reports

doi: 10.1038/s41598-022-23789-3

2D images from the center of the sample along the vertical axis, and 3D visualizations of the interior for the geo-architected samples after 6 full days of dehydration. The pixel edge length resolution is \documentclass[12pt]{minimal}
				\usepackage{amsmath}
				\usepackage{wasysym} 
				\usepackage{amsfonts} 
				\usepackage{amssymb} 
				\usepackage{amsbsy}
				\usepackage{mathrsfs}
				\usepackage{upgreek}
				\setlength{\oddsidemargin}{-69pt}
				\begin{document}$$\sim 40\; \upmu \text{m}$$\end{document} ∼ 40 μ m and the average radius is 19.05 mm. All samples contain non-connected pores (displayed in blue) which are shown only for the reference sample ( a ) and the LICI sample ( b ). Clay inclusions are displayed in brown. All cracks are displayed in red, as shown for the MSCS sample ( c ) and the CB-SK10 sample ( d ). Cracks are only observed in samples containing localized or distributed clay which can result in a 40% reduction in material strength (a comparison between the reference and the CB-SK10 sample). Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .
Figure Legend Snippet: 2D images from the center of the sample along the vertical axis, and 3D visualizations of the interior for the geo-architected samples after 6 full days of dehydration. The pixel edge length resolution is \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\sim 40\; \upmu \text{m}$$\end{document} ∼ 40 μ m and the average radius is 19.05 mm. All samples contain non-connected pores (displayed in blue) which are shown only for the reference sample ( a ) and the LICI sample ( b ). Clay inclusions are displayed in brown. All cracks are displayed in red, as shown for the MSCS sample ( c ) and the CB-SK10 sample ( d ). Cracks are only observed in samples containing localized or distributed clay which can result in a 40% reduction in material strength (a comparison between the reference and the CB-SK10 sample). Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Techniques Used: Software

A comparison of the experimental and simulated damage, where the top row is comprised of two-dimensional (2D) images at the center of each geo-architected sample: ( a ) the reference sample with no visible cracks, ( b ) LICI and ( c ) MSCS with fractured regions in and surrounding the inclusions, and ( d ) the CB sample with many visible cracks. The bottom row is comprised of 2D images of the PD model results for each experimental structure: ( e ) is the data obtained for the reference model, ( f ) is data for the LICI sample, ( g ) is data for the MSCS sample, and ( h ) is data for the CB-SK10 sample. Damage is observed in both the experimental and PD models, and is localized and/ or distributed in areas that contain highly-shrinkable clay. All images are viewed along the transverse plane after six (6) full days of dehydration. Experimental data are processed with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .
Figure Legend Snippet: A comparison of the experimental and simulated damage, where the top row is comprised of two-dimensional (2D) images at the center of each geo-architected sample: ( a ) the reference sample with no visible cracks, ( b ) LICI and ( c ) MSCS with fractured regions in and surrounding the inclusions, and ( d ) the CB sample with many visible cracks. The bottom row is comprised of 2D images of the PD model results for each experimental structure: ( e ) is the data obtained for the reference model, ( f ) is data for the LICI sample, ( g ) is data for the MSCS sample, and ( h ) is data for the CB-SK10 sample. Damage is observed in both the experimental and PD models, and is localized and/ or distributed in areas that contain highly-shrinkable clay. All images are viewed along the transverse plane after six (6) full days of dehydration. Experimental data are processed with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Techniques Used: Software

2D images from the center of the interior of the CB-SK10 geo-architected sample with 20% montmorillonite showing time dependent deformation during moisture loss, ( a – d ) presents drying front progression, reduction of the coherent undamaged material and growth of the crack network. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .
Figure Legend Snippet: 2D images from the center of the interior of the CB-SK10 geo-architected sample with 20% montmorillonite showing time dependent deformation during moisture loss, ( a – d ) presents drying front progression, reduction of the coherent undamaged material and growth of the crack network. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Techniques Used: Software

3D visualizations of the interior and drying shrinkage deformation of a specimen with 20% montmorillonite distributed within the framework during the experimental dehydration period, where ( a – d ) shows the growth of the crack network in 3D, and ( e , f ) shows the reduction of the undamaged material zone (shrinking dark columns) and evolution of the drying front. The undamaged data for the initial sample is not shown as  93% of the sample remains undamaged. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .
Figure Legend Snippet: 3D visualizations of the interior and drying shrinkage deformation of a specimen with 20% montmorillonite distributed within the framework during the experimental dehydration period, where ( a – d ) shows the growth of the crack network in 3D, and ( e , f ) shows the reduction of the undamaged material zone (shrinking dark columns) and evolution of the drying front. The undamaged data for the initial sample is not shown as  93% of the sample remains undamaged. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Techniques Used: Software



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Object Research Systems (ORS) Inc dragonfly pro software, version 2020.2 [windows
2D images from the center of the sample along the vertical axis, and 3D visualizations of the interior for the geo-architected samples after 6 full days of dehydration. The pixel edge length resolution is \documentclass[12pt]{minimal}
				\usepackage{amsmath}
				\usepackage{wasysym} 
				\usepackage{amsfonts} 
				\usepackage{amssymb} 
				\usepackage{amsbsy}
				\usepackage{mathrsfs}
				\usepackage{upgreek}
				\setlength{\oddsidemargin}{-69pt}
				\begin{document}$$\sim 40\; \upmu \text{m}$$\end{document} ∼ 40 μ m and the average radius is 19.05 mm. All samples contain non-connected pores (displayed in blue) which are shown only for the reference sample ( a ) and the LICI sample ( b ). Clay inclusions are displayed in brown. All cracks are displayed in red, as shown for the MSCS sample ( c ) and the CB-SK10 sample ( d ). Cracks are only observed in samples containing localized or distributed clay which can result in a 40% reduction in material strength (a comparison between the reference and the CB-SK10 sample). Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .
Dragonfly Pro Software, Version 2020.2 [Windows, supplied by Object Research Systems (ORS) 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/result/dragonfly pro software, version 2020.2 [windows/product/Object Research Systems (ORS) Inc
Average 90 stars, based on 1 article reviews
dragonfly pro software, version 2020.2 [windows - by Bioz Stars, 2026-06
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A) Representative reconstructed 0.4x objective scan of the entire tibia. B) Reconstructed 4x objective scan of bone region 3 mm from the tibiofibular junction. C) Reconstructed 20x objective scan of a 0.3 mm 3 field of view of the bone region in the anterior medial aspect of the tibia. D) Negative image provides a visualization of osteocyte lacunae in bone, where lacunae are false colored by lacunar volume. Scans were reconstructed and visualized using Dragonfly 2020.2 Pro [Object Research Systems (ORS) Inc, Montreal, QC].
Dragonfly 2020.2 Pro, supplied by Object Research Systems (ORS) Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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Average 90 stars, based on 1 article reviews
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Image Search Results


2D images from the center of the sample along the vertical axis, and 3D visualizations of the interior for the geo-architected samples after 6 full days of dehydration. The pixel edge length resolution is \documentclass[12pt]{minimal}
				\usepackage{amsmath}
				\usepackage{wasysym} 
				\usepackage{amsfonts} 
				\usepackage{amssymb} 
				\usepackage{amsbsy}
				\usepackage{mathrsfs}
				\usepackage{upgreek}
				\setlength{\oddsidemargin}{-69pt}
				\begin{document}$$\sim 40\; \upmu \text{m}$$\end{document} ∼ 40 μ m and the average radius is 19.05 mm. All samples contain non-connected pores (displayed in blue) which are shown only for the reference sample ( a ) and the LICI sample ( b ). Clay inclusions are displayed in brown. All cracks are displayed in red, as shown for the MSCS sample ( c ) and the CB-SK10 sample ( d ). Cracks are only observed in samples containing localized or distributed clay which can result in a 40% reduction in material strength (a comparison between the reference and the CB-SK10 sample). Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .

Journal: Scientific Reports

Article Title: The effect of differential mineral shrinkage on crack formation and network geometry

doi: 10.1038/s41598-022-23789-3

Figure Lengend Snippet: 2D images from the center of the sample along the vertical axis, and 3D visualizations of the interior for the geo-architected samples after 6 full days of dehydration. The pixel edge length resolution is \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\sim 40\; \upmu \text{m}$$\end{document} ∼ 40 μ m and the average radius is 19.05 mm. All samples contain non-connected pores (displayed in blue) which are shown only for the reference sample ( a ) and the LICI sample ( b ). Clay inclusions are displayed in brown. All cracks are displayed in red, as shown for the MSCS sample ( c ) and the CB-SK10 sample ( d ). Cracks are only observed in samples containing localized or distributed clay which can result in a 40% reduction in material strength (a comparison between the reference and the CB-SK10 sample). Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Article Snippet: The acquired data were initially examined using Dragonfly Pro software, Version 2020.2 for [Windows] from Object Research Systems (ORS) Inc. .

Techniques: Software

A comparison of the experimental and simulated damage, where the top row is comprised of two-dimensional (2D) images at the center of each geo-architected sample: ( a ) the reference sample with no visible cracks, ( b ) LICI and ( c ) MSCS with fractured regions in and surrounding the inclusions, and ( d ) the CB sample with many visible cracks. The bottom row is comprised of 2D images of the PD model results for each experimental structure: ( e ) is the data obtained for the reference model, ( f ) is data for the LICI sample, ( g ) is data for the MSCS sample, and ( h ) is data for the CB-SK10 sample. Damage is observed in both the experimental and PD models, and is localized and/ or distributed in areas that contain highly-shrinkable clay. All images are viewed along the transverse plane after six (6) full days of dehydration. Experimental data are processed with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .

Journal: Scientific Reports

Article Title: The effect of differential mineral shrinkage on crack formation and network geometry

doi: 10.1038/s41598-022-23789-3

Figure Lengend Snippet: A comparison of the experimental and simulated damage, where the top row is comprised of two-dimensional (2D) images at the center of each geo-architected sample: ( a ) the reference sample with no visible cracks, ( b ) LICI and ( c ) MSCS with fractured regions in and surrounding the inclusions, and ( d ) the CB sample with many visible cracks. The bottom row is comprised of 2D images of the PD model results for each experimental structure: ( e ) is the data obtained for the reference model, ( f ) is data for the LICI sample, ( g ) is data for the MSCS sample, and ( h ) is data for the CB-SK10 sample. Damage is observed in both the experimental and PD models, and is localized and/ or distributed in areas that contain highly-shrinkable clay. All images are viewed along the transverse plane after six (6) full days of dehydration. Experimental data are processed with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Article Snippet: The acquired data were initially examined using Dragonfly Pro software, Version 2020.2 for [Windows] from Object Research Systems (ORS) Inc. .

Techniques: Software

2D images from the center of the interior of the CB-SK10 geo-architected sample with 20% montmorillonite showing time dependent deformation during moisture loss, ( a – d ) presents drying front progression, reduction of the coherent undamaged material and growth of the crack network. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .

Journal: Scientific Reports

Article Title: The effect of differential mineral shrinkage on crack formation and network geometry

doi: 10.1038/s41598-022-23789-3

Figure Lengend Snippet: 2D images from the center of the interior of the CB-SK10 geo-architected sample with 20% montmorillonite showing time dependent deformation during moisture loss, ( a – d ) presents drying front progression, reduction of the coherent undamaged material and growth of the crack network. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Article Snippet: The acquired data were initially examined using Dragonfly Pro software, Version 2020.2 for [Windows] from Object Research Systems (ORS) Inc. .

Techniques: Software

3D visualizations of the interior and drying shrinkage deformation of a specimen with 20% montmorillonite distributed within the framework during the experimental dehydration period, where ( a – d ) shows the growth of the crack network in 3D, and ( e , f ) shows the reduction of the undamaged material zone (shrinking dark columns) and evolution of the drying front. The undamaged data for the initial sample is not shown as  93% of the sample remains undamaged. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS  .

Journal: Scientific Reports

Article Title: The effect of differential mineral shrinkage on crack formation and network geometry

doi: 10.1038/s41598-022-23789-3

Figure Lengend Snippet: 3D visualizations of the interior and drying shrinkage deformation of a specimen with 20% montmorillonite distributed within the framework during the experimental dehydration period, where ( a – d ) shows the growth of the crack network in 3D, and ( e , f ) shows the reduction of the undamaged material zone (shrinking dark columns) and evolution of the drying front. The undamaged data for the initial sample is not shown as  93% of the sample remains undamaged. Data are visualized with Dragonfly Pro software, Version 2020.2 for [Windows] from ORS .

Article Snippet: The acquired data were initially examined using Dragonfly Pro software, Version 2020.2 for [Windows] from Object Research Systems (ORS) Inc. .

Techniques: Software

A) Representative reconstructed 0.4x objective scan of the entire tibia. B) Reconstructed 4x objective scan of bone region 3 mm from the tibiofibular junction. C) Reconstructed 20x objective scan of a 0.3 mm 3 field of view of the bone region in the anterior medial aspect of the tibia. D) Negative image provides a visualization of osteocyte lacunae in bone, where lacunae are false colored by lacunar volume. Scans were reconstructed and visualized using Dragonfly 2020.2 Pro [Object Research Systems (ORS) Inc, Montreal, QC].

Journal: bioRxiv

Article Title: Reduced local mechanical stimuli in spaceflight diminishes osteocyte lacunar morphometry and spatial heterogeneity in mouse cortical bone

doi: 10.1101/2022.01.04.474962

Figure Lengend Snippet: A) Representative reconstructed 0.4x objective scan of the entire tibia. B) Reconstructed 4x objective scan of bone region 3 mm from the tibiofibular junction. C) Reconstructed 20x objective scan of a 0.3 mm 3 field of view of the bone region in the anterior medial aspect of the tibia. D) Negative image provides a visualization of osteocyte lacunae in bone, where lacunae are false colored by lacunar volume. Scans were reconstructed and visualized using Dragonfly 2020.2 Pro [Object Research Systems (ORS) Inc, Montreal, QC].

Article Snippet: Individual scans were reconstructed using Zeiss Scout-and-Scan Control System Reconstructor 14.0.14829.3814 (Zeiss, Dublin, CA, United States of America) then imported into Dragonfly 2020.2 Pro [Object Research Systems (ORS) Inc, Montreal, QC] in which files were segmented using a global Otsu thresholding algorithm.

Techniques: