The Dead Sea (DS) is a lowest place at the Earth with a unique physical-chemical water composition. The most important physical factor of this basin is the vertical gradient of water density: from 1150 kg/m3 at the DS surface up to 1430 kg/m3 at the depth of 310-330 m. The new mathematical solution obtained for stratified, rotating and compressible liquid (with utilization of gravity, density, temperature and acoustic data) permits to create a solvable system of differential equations and utilize it for development of exact physical/mathematical/geological model of the DS basin.
|State||Published - 2010|
|Event||16th European Meeting of Environmental and Engineering Geophysics, Near Surface 2010 - Zurich, Switzerland|
Duration: 6 Sep 2010 → 8 Sep 2010
|Conference||16th European Meeting of Environmental and Engineering Geophysics, Near Surface 2010|
|Period||6/09/10 → 8/09/10|