Development and geometry of isotropic and directional shrinkage-crack patterns
- 1 June 2000
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review E
- Vol. 61 (6) , 6950-6957
- https://doi.org/10.1103/physreve.61.6950
Abstract
We have studied shrinkage-crack patterns which form when a thin layer of an alumina/water slurry dries. Both isotropic and directional drying were studied. The dynamics of the pattern formation process and the geometric properties of the isotropic crack patterns are similar to what is expected from recent models, assuming weak disorder. There is some evidence of a gradual increase in disorder as the drying layer become thinner, but no sudden transition, in contrast to what has been seen in previous experiments. The morphology of the crack patterns is influenced by drying gradients and front propagation effects, with sharp gradients having a strong orienting and ordering effect.Keywords
All Related Versions
This publication has 30 references indexed in Scilit:
- Two substorm intensifications compared: Onset, expansion, and global consequencesJournal of Geophysical Research, 1998
- Regular Patterns of Cracks Formed by Directional Drying of a Collodial SuspensionPhysical Review Letters, 1995
- Modelling the evolution of columnar jointsJournal of Volcanology and Geothermal Research, 1994
- Dynamic Fracture MechanicsPublished by Cambridge University Press (CUP) ,1990
- The Amateur ScientistScientific American, 1986
- Cyclic fracture mechanisms in cooling basaltGSA Bulletin, 1978
- POLYGONAL SANDSTONE FEATURES IN BOUNDARY BUTTE ANTICLINE AREA, SAN JUAN COUNTY, UTAH: DISCUSSIONGSA Bulletin, 1966
- POLYGONAL SANDSTONE FEATURES IN BOUNDARY BUTTE ANTICLINE AREA, SAN JUAN COUNTY, UTAH: REPLYGSA Bulletin, 1966
- POLYGONAL SANDSTONE FEATURES IN BOUNDARY BUTTE ANTICLINE AREA, SAN JUAN COUNTY, UTAHGSA Bulletin, 1965
- Some Factors Affecting the Development of Mud-CracksThe Journal of Geology, 1917