T342 The Epikarst as a Boundary and Critical Zone (Posters)
Wednesday, 30 October 2013
9:00 AM - 6:30 PM
Hall D
EROSION POTENTIAL AND SOLUTE TRANSPORT BY CAPILLARY SOLITONS WITHIN THE EPIKARST
Paper number: T342-2
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Katrina M. HayPacific Lutheran University, Tacoma, WA
Abstract
Under specific circumstances, liquid films can become unstable, leading to the development of a wavy gas-liquid interfacial surface with waves that grow in time. These waves can grow to amplitudes more than 10 times that of the original film. When these waves touch the opposite crack wall, the fluid situation and geochemical erosion potential dramatically changes, wherein upon contact a wave immediately produces a droplet that is under capillary tension, creating a new hydraulically persistent entity. They do not re-merge with the liquid film, but rather absorb liquid and solutes in their path leaving behind a ‘dry’ patch. This poster will show visualization data of developing and evolving capillary droplets, discuss the criteria for droplet formation, pressure gradient calculations and solute transport potential.