Abstract
In the present study, inverse problems (IP) are applied with FEPEST® in FEFLOW® to find parameter distributions of hydraulic and thermal conductivity that lead to the observed thermal anomalies in the Lower Yarmouk Gorge (LYG) and a more accurate fit of borehole data. Results indicate reduced hydraulic conductivities in shallower parts of the system than previously estimated. The absence of a fault under the Lower Yarmouk Gorge in deeper sediments can be superseded by presence of interconnecting local fractures. The contribution of the conductive thermal regime turns out to be negligible.
Original language | English |
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Pages (from-to) | 419-426 |
Number of pages | 8 |
Journal | Energy Procedia |
Volume | 97 |
DOIs | |
State | Published - 2016 |
Externally published | Yes |
Event | European Geosciences Union General Assembly 2016, EGU Division Energy, Resources and the Environment, ERE 2016 - Vienna, Austria Duration: 17 Apr 2016 → 22 Apr 2016 |
Keywords
- FEPEST
- Inverse Problem
- Lower Yarmouk Gorge
- Tiberias Basin
- fault
- hydraulic conductivity
- temperature anomaly