Abstract
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.
Original language | English |
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DOIs | |
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
Conference | 16th European Meeting of Environmental and Engineering Geophysics, Near Surface 2010 |
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Country/Territory | Switzerland |
City | Zurich |
Period | 6/09/10 → 8/09/10 |