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Transmission of pressure head through the zone of tension saturation in the Lisse effect phenomenon
Authors:George W Waswa  Simon A Lorentz
Institution:1. School of Engineering and Centre for Water Resources Research, University of KwaZulu-Natal, Scottsville, South Africa;2. Department of Civil and Structural Engineering, Masinde Muliro University of Science and Technology, Kakamega, Kenya208529656@stu.ukzn.ac.za waswageorge@gmail.com
Abstract:ABSTRACT

The problem of transmission of pressure head through the zone of tension saturation in the Lisse effect (LE), i.e., the rapid response of groundwater level to pressurized pore air in the unsaturated zone, is investigated theoretically and experimentally. From the law of conservation of energy and the continuity equation, a one-dimensional diffusion equation is derived for transmission of pressure head through the zone of tension saturation. The solution to the equation is the pressure head at any point below the upper boundary of the zone of tension saturation and at any time after the compressed pore air pressure is imposed on the boundary. The key parameter, which determines the behaviour of transmission of pressure head, is the newly proposed pressure head diffusivity coefficient. The theoretical results agree with the experimental results, obtained from laboratory column experiments in three physically different soils.
Editor Demetris Koutsoyiannis Associate editor Xi Chen
Keywords:compressed pore air pressure  diffusion equation  mathematical model  potential energy  rapid water table response
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