Inverse Problem to Constrain Hydraulic and Thermal Parameters Inducing Anomalous Heat Flow in the Lower Yarmouk Gorge

Nora Goretzki; Nimrod Inbar; Michael Kühn; Peter Möller; Eliyahu Rosenthal; Michael Schneider; Christian Siebert; Marwan Raggad; Fabien Magri

doi:10.1016/j.egypro.2016.10.038

Inverse Problem to Constrain Hydraulic and Thermal Parameters Inducing Anomalous Heat Flow in the Lower Yarmouk Gorge

Nora Goretzki, Nimrod Inbar, Michael Kühn, Peter Möller, Eliyahu Rosenthal, Michael Schneider, Christian Siebert, Marwan Raggad, Fabien Magri

Research output: Contribution to journal › Conference article › peer-review

9 Scopus citations

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 The absence of a fault under the Lower Yarmouk Gorge in deeper sediments can be superseded by presence of interconnecting local fractures.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
Pages (from-to)	419-426
Number of pages	8
Journal	Energy Procedia
Volume	97
DOIs	https://doi.org/10.1016/j.egypro.2016.10.038
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

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10.1016/j.egypro.2016.10.038

Cite this

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title = "Inverse Problem to Constrain Hydraulic and Thermal Parameters Inducing Anomalous Heat Flow in the Lower Yarmouk Gorge",

abstract = "In the present study, inverse problems (IP) are applied with FEPEST{\textregistered} in FEFLOW{\textregistered} 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.",

keywords = "FEPEST, Inverse Problem, Lower Yarmouk Gorge, Tiberias Basin, fault, hydraulic conductivity, temperature anomaly",

author = "Nora Goretzki and Nimrod Inbar and Michael K{\"u}hn and Peter M{\"o}ller and Eliyahu Rosenthal and Michael Schneider and Christian Siebert and Marwan Raggad and Fabien Magri",

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year = "2016",

doi = "10.1016/j.egypro.2016.10.038",

language = "אנגלית",

volume = "97",

pages = "419--426",

journal = "Energy Procedia",

issn = "1876-6102",

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T1 - Inverse Problem to Constrain Hydraulic and Thermal Parameters Inducing Anomalous Heat Flow in the Lower Yarmouk Gorge

AU - Goretzki, Nora

AU - Inbar, Nimrod

AU - Kühn, Michael

AU - Möller, Peter

AU - Rosenthal, Eliyahu

AU - Schneider, Michael

AU - Siebert, Christian

AU - Raggad, Marwan

AU - Magri, Fabien

PY - 2016

Y1 - 2016

N2 - 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.

AB - 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.

KW - FEPEST

KW - Inverse Problem

KW - Lower Yarmouk Gorge

KW - Tiberias Basin

KW - fault

KW - hydraulic conductivity

KW - temperature anomaly

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SN - 1876-6102

VL - 97

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JO - Energy Procedia

JF - Energy Procedia

T2 - European Geosciences Union General Assembly 2016, EGU Division Energy, Resources and the Environment, ERE 2016

Y2 - 17 April 2016 through 22 April 2016

ER -

Inverse Problem to Constrain Hydraulic and Thermal Parameters Inducing Anomalous Heat Flow in the Lower Yarmouk Gorge

Abstract

Keywords

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