high speed camera (Nikon)
Structured Review
![( A ) Schematic of illustrating the cooling-induced ice eruptive fracture on solid substrate. ( B <t>)</t> <t>High-speed</t> camera snapshots of the ice ejection on hydrophilic silicon wafer substrate when cooled to −122°C. ( C ) High-speed camera snapshots of the eruptive fracture of the ice and the substrate disintegration at −133°C. ( D ) The ice bound to the light-weight substrate leapt. ( E ) Evolution of calculated mechanical energy with fracture temperature for varying formation temperature of ice. Inset images display bound leap and motionless fractures at different temperatures, corresponding to ice with different formation temperature, respectively. The critical temperature T c = −93° ± 3°C is highlighted. Time τ = 0 ms in (B) to (D) denotes the onset of crack formation. The cooling rate is set as −0.5°C s −1 . Freezing water volume: 20 μl. Scale bars, 5 mm [(B) to (E)].](https://pub-med-central-images-cdn.bioz.com/pub_med_central_ids_ending_with_1743/pmc13041743/pmc13041743__sciadv.adz8663-f1.jpg)
High Speed Camera, supplied by Nikon, used in various techniques. Bioz Stars score: 99/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/high speed camera/product/Nikon
Average 99 stars, based on 1 article reviews
Images
1) Product Images from "Abrupt eruptive instability of ice adhered to solid surfaces"
Article Title: Abrupt eruptive instability of ice adhered to solid surfaces
Journal: Science Advances
doi: 10.1126/sciadv.adz8663
Figure Legend Snippet: ( A ) Schematic of illustrating the cooling-induced ice eruptive fracture on solid substrate. ( B ) High-speed camera snapshots of the ice ejection on hydrophilic silicon wafer substrate when cooled to −122°C. ( C ) High-speed camera snapshots of the eruptive fracture of the ice and the substrate disintegration at −133°C. ( D ) The ice bound to the light-weight substrate leapt. ( E ) Evolution of calculated mechanical energy with fracture temperature for varying formation temperature of ice. Inset images display bound leap and motionless fractures at different temperatures, corresponding to ice with different formation temperature, respectively. The critical temperature T c = −93° ± 3°C is highlighted. Time τ = 0 ms in (B) to (D) denotes the onset of crack formation. The cooling rate is set as −0.5°C s −1 . Freezing water volume: 20 μl. Scale bars, 5 mm [(B) to (E)].
Techniques Used:
Figure Legend Snippet: ( A ) Material distribution according to their TECs and Young’s modulus values . Adapted with permission from , copyright 2011, Elsevier. The color dots show the occurrence of ice eruptive fracture on the corresponding materials. Insets: High-speed camera snapshots of bound leap of ice with aluminum alloy, sapphire, and quartz substrate. ( B ) Design of the automatic detachment of ice using substrate deformation upon temperature variation. ( C ) Spontaneous detachment of an ice block (volume: 100 ml) from a bimetallic strip upon cooling to −53°C. Scale bars, 1 cm (A) and 5 cm (C).
Techniques Used: Blocking Assay, Stripping Membranes


