Terrain uplift due to natural hydrologic overpressure in karstic conduits View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2019-12

AUTHORS

Carla Braitenberg, Tommaso Pivetta, Dora Francesca Barbolla, Franci Gabrovšek, Roberto Devoti, Ildikó Nagy

ABSTRACT

Water supply from karst sources is a worldwide natural resource and the exploitation is tied to the knowledge of the positions of the hydrologic channels. We show that surface deformation induced by flood events in karst conduits is observable, and consists in uplift and outward movement from the hydraulic channel. Precipitation events produce the natural occurrence of subsurface hydraulic overpressure up to 1 MPa. Numerical modeling shows that the stresses are so strong to uplift and dislocate the surface by several mm and induce tilts in the order of microradians. The naturally induced deformation is compatible with a transient internal pressure loading of a channel. The results can be used to find new channels with dense GNSS networks. Sea water incursion and channels accessed for tourism could be monitored. Seismicity has been shown to have a seasonal variation in some areas, which could be explained by the subsurface stresses induced by the natural subsurface overpressure. The pressure induced deformation is expected to be observed in all karstic systems worldwide. More... »

PAGES

3934

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41598-019-38814-1

DOI

http://dx.doi.org/10.1038/s41598-019-38814-1

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1112641482

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/30850699


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