scholarly journals Catastrophic failure: how and when? Insights from 4D in-situ x-ray micro-tomography

2020 ◽  
Author(s):  
Alexis Cartwright-Taylor ◽  
Ian G Main ◽  
Ian B Butler ◽  
Florian Fusseis ◽  
Michael Flynn ◽  
...  
2020 ◽  
Author(s):  
Alexis Cartwright-Taylor ◽  
Ian G Main ◽  
Ian B Butler ◽  
Florian Fusseis ◽  
Michael Flynn ◽  
...  

2020 ◽  
Author(s):  
Alexis Cartwright-Taylor ◽  
Ian G Main ◽  
Ian B Butler ◽  
Florian Fusseis ◽  
Michael Flynn ◽  
...  

2018 ◽  
Vol 116 ◽  
pp. 490-504 ◽  
Author(s):  
Stephen T. Carter ◽  
John Rotella ◽  
Ronald F. Agyei ◽  
Xiaghui Xiao ◽  
Michael D. Sangid
Keyword(s):  
X Ray ◽  

2012 ◽  
Vol 24 (4) ◽  
pp. 599-606 ◽  
Author(s):  
Fabrizio Nestola ◽  
Marcello Merli ◽  
Paolo Nimis ◽  
Matteo Parisatto ◽  
Maya Kopylova ◽  
...  

2012 ◽  
Vol 706-709 ◽  
pp. 1713-1718 ◽  
Author(s):  
Luc Salvo ◽  
Marco Di Michiel ◽  
Mario Scheel ◽  
Pierre Lhuissier ◽  
B. Mireux ◽  
...  

X-ray micro-tomography has been applied recently in a wide range of research fields (damage in materials, solidification …). Thanks to the high flux of synchrotrons and specific cameras the total time to acquire a scan was considerably reduced. The use of a specific camera based on CMOS technology allows dividing the acquisition time for a complete scan by a factor of 100. Therefore we have been able to perform in situ solidification of aluminium-copper alloys at high cooling rates (between 1 and 10°C/s) and we will show results concerning the evolution of the microstructure in 3D in the early stage of solidification, in particular the morphology of the solid phase and the kinetics of growth.


Solid Earth ◽  
2012 ◽  
Vol 3 (1) ◽  
pp. 71-86 ◽  
Author(s):  
F. Fusseis ◽  
C. Schrank ◽  
J. Liu ◽  
A. Karrech ◽  
S. Llana-Fúnez ◽  
...  

Abstract. We conducted an in-situ X-ray micro-computed tomography heating experiment at the Advanced Photon Source (USA) to dehydrate an unconfined 2.3 mm diameter cylinder of Volterra Gypsum. We used a purpose-built X-ray transparent furnace to heat the sample to 388 K for a total of 310 min to acquire a three-dimensional time-series tomography dataset comprising nine time steps. The voxel size of 2.2 μm3 proved sufficient to pinpoint reaction initiation and the organization of drainage architecture in space and time. We observed that dehydration commences across a narrow front, which propagates from the margins to the centre of the sample in more than four hours. The advance of this front can be fitted with a square-root function, implying that the initiation of the reaction in the sample can be described as a diffusion process. Novel parallelized computer codes allow quantifying the geometry of the porosity and the drainage architecture from the very large tomographic datasets (20483 voxels) in unprecedented detail. We determined position, volume, shape and orientation of each resolvable pore and tracked these properties over the duration of the experiment. We found that the pore-size distribution follows a power law. Pores tend to be anisotropic but rarely crack-shaped and have a preferred orientation, likely controlled by a pre-existing fabric in the sample. With on-going dehydration, pores coalesce into a single interconnected pore cluster that is connected to the surface of the sample cylinder and provides an effective drainage pathway. Our observations can be summarized in a model in which gypsum is stabilized by thermal expansion stresses and locally increased pore fluid pressures until the dehydration front approaches to within about 100 μm. Then, the internal stresses are released and dehydration happens efficiently, resulting in new pore space. Pressure release, the production of pores and the advance of the front are coupled in a feedback loop.


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