Synonyms
Definition
Quicksand is sediment of low bearing capacity caused by high volumes of water, or more rarely air, and a resultant decrease in the intergranular pressure due to disturbance. Quicksand is not any special type of sand, but instead it is a condition of zero effective stress.
The condition may occur in sediment with either standing water or flowing water. In the former case, the condition can be triggered by ground shaking (liquefaction). Most quicksand occurs in settings where there are natural springs, either at the base of alluvial fans, along riverbanks, or on beaches at low tide. In such cases, the loose packing is maintained by the upward movement of water (Fig. 1; Long 2002).
References
Long DGF (2002) What is quicksand? Scientific American article. https://www.scientificamerican.com/article/what-is-quicksand/
https://theconstructor.org/geotechnical/quick-sand-condition/3455/
https://www.europhysicsnews.org/articles/epn/pdf/2006/04/epn06404.pdf
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2018 Springer International Publishing AG
About this entry
Cite this entry
Lintern, G. (2018). Quicksand. In: Bobrowsky, P., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-12127-7_232-1
Download citation
DOI: https://doi.org/10.1007/978-3-319-12127-7_232-1
Received:
Accepted:
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-12127-7
Online ISBN: 978-3-319-12127-7
eBook Packages: Springer Reference Earth and Environm. ScienceReference Module Physical and Materials ScienceReference Module Earth and Environmental Sciences