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Hydrogeological modeling of the saline hot springs at the Sea of Galilee, Israel
Author(s) -
Gvirtzman Haim,
Garven Grant,
Gvirtzman Gdaliahu
Publication year - 1997
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/96wr03191
Subject(s) - aquifer , phreatic , geology , hydrogeology , groundwater , water table , groundwater flow , hydrology (agriculture) , spring (device) , structural basin , rift , geomorphology , geotechnical engineering , mechanical engineering , engineering
Meteoric fresh groundwater from shallow aquifers and hot brines from deep aquifers mix while emerging from several springs along the western coast of the Sea of Galilee, a freshwater lake located within the Dead Sea Rift Valley, Israel. After the rainy season, when elevations of the groundwater table rise in the regional aquifers and discharge rates of springs increase, solute concentrations decrease at Tabha springs but, surprisingly, increase at Fulya springs, apparently suggesting two different salinization mechanisms. Two detailed geologic cross sections were constructed, one across the rift valley at Tabha and a second at Fulya, each about 6 km deep and 70 km long. The hydrodynamics in these cross sections were analyzed using a two‐dimensional finite element code that solves the coupled variable‐density groundwater flow and heat transfer equations. Numerical simulations indicate that a topography‐driven flow model explains both spring systems, and the opposite salinity behavior results from the different hydrogeological configurations of the two subsurface drainage basins. At Fulya, both aquifers, the shallow one and the deeper one, are partially phreatic, whereas at Tabha, the deeper aquifer is totally confined. The response of springs to changes in elevation of groundwater table were simulated, reproducing field observations. This analysis has implications for the management scheme for the lake and its surrounding aquifers.