Articles | Volume 19, issue 1
https://doi.org/10.5194/hess-19-137-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-19-137-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
09 Jan 2015
Research article |
| 09 Jan 2015
Thermal damping and retardation in karst conduits
A. J. Luhmann
CORRESPONDING AUTHOR
University of Minnesota, Department of Earth Sciences, 310 Pillsbury Dr. SE, Minneapolis, Minnesota 55455, USA
M. D. Covington
University of Arkansas, Department of Geosciences, 216 Ozark Hall, Fayetteville, Arkansas 72701, USA
J. M. Myre
University of Arkansas, Department of Geosciences, 216 Ozark Hall, Fayetteville, Arkansas 72701, USA
M. Perne
Jožef Stefan Institute, Department of Systems and Control, Jamova Cesta 39, Ljubljana, Slovenia
University of Arkansas, Department of Geosciences, 216 Ozark Hall, Fayetteville, Arkansas 72701, USA
S. W. Jones
527 Karrow St., Maryville, Tennessee 37803, USA
E. C. Alexander Jr.
University of Minnesota, Department of Earth Sciences, 310 Pillsbury Dr. SE, Minneapolis, Minnesota 55455, USA
M. O. Saar
University of Minnesota, Department of Earth Sciences, 310 Pillsbury Dr. SE, Minneapolis, Minnesota 55455, USA
ETH-Zürich, Geothermal Energy and Geofluids Group, Department of Earth Sciences, Zürich, Switzerland
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Cited
20 citations as recorded by crossref.
- Suivi des déformations du massif rocheux sous la fondation de la pile VII du Pont du Gard J. Serratrice 10.1051/geotech/2020023
- Shallow groundwater temperature patterns revealed through a regional monitoring well network K. Smith et al. 10.1002/hyp.14975
- Laboratory and numerical simulations of spatio-temporal variability of water exchange between the fissures and conduits in a karstic aquifer L. Shu et al. 10.1016/j.jhydrol.2020.125219
- Synthesizing multifaceted characterization techniques to refine a conceptual model of groundwater sources to springs in valley settings (Minnesota, USA) J. Barry et al. 10.1007/s10040-023-02613-w
- Tomographic Reservoir Imaging with DNA-Labeled Silica Nanotracers: The First Field Validation X. Kong et al. 10.1021/acs.est.8b04367
- Characterizing the heterogeneity of karst critical zone and its hydrological function: An integrated approach X. Chen et al. 10.1002/hyp.13232
- Heat: An Overlooked Tool in the Practicing Hydrogeologist's Toolbox B. Kurylyk & D. Irvine 10.1111/gwat.12910
- Controls on cave drip water temperature and implications for speleothem-based paleoclimate reconstructions G. Rau et al. 10.1016/j.quascirev.2015.03.026
- Thermal Attenuation and Lag Time in Fractured Rock: Theory and Field Measurements From Joint Heat and Solute Tracer Tests J. de La Bernardie et al. 10.1029/2018WR023199
- Temperature as a tracer of hydrological dynamics in an anchialine cave system with a submarine spring D. Domínguez-Villar et al. 10.1007/s10040-018-1724-3
- Joint inversion of groundwater flow, heat, and solute state variables: a multipurpose approach for characterization and forecast of karst systems A. Kavousi et al. 10.1007/s10040-023-02631-8
- Identifying the origin, recharge, and salinity sources of the Romqan saline spring, causing intense salinization of the Shirinrud River in southern Iran J. Mohammadzadeh-Habili & D. Khalili 10.1016/j.gsd.2024.101370
- Stream Gauge Calibration of a Cave Stream Using Water Temperature Variability as a Tracer M. Lüthi 10.1029/2018WR023762
- Solute tracer test quantification of the effects of hot water injection into hydraulically stimulated crystalline rock A. Kittilä et al. 10.1186/s40517-020-00172-x
- Geographic and transport controls of temperature response in karst springs M. Luo et al. 10.1016/j.jhydrol.2023.129850
- Effects of Changing Meteoric Precipitation Patterns on Groundwater Temperature in Karst Environments A. Brookfield et al. 10.1111/gwat.12456
- Comparison of microbial indicators and seasonal temperatures as means for evaluating the vulnerability of water resources from karst and siliciclastic springs D. Vesper et al. 10.1007/s10040-022-02496-3
- Karst hydrogeology of Lamprechtsofen (Leoganger Steinberge, Salzburg) K. Gröbner et al. 10.17738/ajes.2019.0004
- Carbon dioxide and dissolution rate dynamics within a karst underflow-overflow system, Savoy Experimental Watershed, Arkansas, USA M. Covington & K. Vaughn 10.1016/j.chemgeo.2018.03.009
- Identifying the recharge and salinization mechanisms of the Shekastian saline spring in southern Iran J. Mohammadzadeh-Habili et al. 10.1007/s11356-023-27308-3
20 citations as recorded by crossref.
- Suivi des déformations du massif rocheux sous la fondation de la pile VII du Pont du Gard J. Serratrice 10.1051/geotech/2020023
- Shallow groundwater temperature patterns revealed through a regional monitoring well network K. Smith et al. 10.1002/hyp.14975
- Laboratory and numerical simulations of spatio-temporal variability of water exchange between the fissures and conduits in a karstic aquifer L. Shu et al. 10.1016/j.jhydrol.2020.125219
- Synthesizing multifaceted characterization techniques to refine a conceptual model of groundwater sources to springs in valley settings (Minnesota, USA) J. Barry et al. 10.1007/s10040-023-02613-w
- Tomographic Reservoir Imaging with DNA-Labeled Silica Nanotracers: The First Field Validation X. Kong et al. 10.1021/acs.est.8b04367
- Characterizing the heterogeneity of karst critical zone and its hydrological function: An integrated approach X. Chen et al. 10.1002/hyp.13232
- Heat: An Overlooked Tool in the Practicing Hydrogeologist's Toolbox B. Kurylyk & D. Irvine 10.1111/gwat.12910
- Controls on cave drip water temperature and implications for speleothem-based paleoclimate reconstructions G. Rau et al. 10.1016/j.quascirev.2015.03.026
- Thermal Attenuation and Lag Time in Fractured Rock: Theory and Field Measurements From Joint Heat and Solute Tracer Tests J. de La Bernardie et al. 10.1029/2018WR023199
- Temperature as a tracer of hydrological dynamics in an anchialine cave system with a submarine spring D. Domínguez-Villar et al. 10.1007/s10040-018-1724-3
- Joint inversion of groundwater flow, heat, and solute state variables: a multipurpose approach for characterization and forecast of karst systems A. Kavousi et al. 10.1007/s10040-023-02631-8
- Identifying the origin, recharge, and salinity sources of the Romqan saline spring, causing intense salinization of the Shirinrud River in southern Iran J. Mohammadzadeh-Habili & D. Khalili 10.1016/j.gsd.2024.101370
- Stream Gauge Calibration of a Cave Stream Using Water Temperature Variability as a Tracer M. Lüthi 10.1029/2018WR023762
- Solute tracer test quantification of the effects of hot water injection into hydraulically stimulated crystalline rock A. Kittilä et al. 10.1186/s40517-020-00172-x
- Geographic and transport controls of temperature response in karst springs M. Luo et al. 10.1016/j.jhydrol.2023.129850
- Effects of Changing Meteoric Precipitation Patterns on Groundwater Temperature in Karst Environments A. Brookfield et al. 10.1111/gwat.12456
- Comparison of microbial indicators and seasonal temperatures as means for evaluating the vulnerability of water resources from karst and siliciclastic springs D. Vesper et al. 10.1007/s10040-022-02496-3
- Karst hydrogeology of Lamprechtsofen (Leoganger Steinberge, Salzburg) K. Gröbner et al. 10.17738/ajes.2019.0004
- Carbon dioxide and dissolution rate dynamics within a karst underflow-overflow system, Savoy Experimental Watershed, Arkansas, USA M. Covington & K. Vaughn 10.1016/j.chemgeo.2018.03.009
- Identifying the recharge and salinization mechanisms of the Shekastian saline spring in southern Iran J. Mohammadzadeh-Habili et al. 10.1007/s11356-023-27308-3
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Short summary
Water temperature is a non-conservative tracer. Variations in recharge temperature are damped and retarded as water moves through an aquifer due to heat exchange between water and rock. This paper presents relationships that describe thermal damping and retardation in karst conduits determined using analytical solutions and numerical simulations, with some support provided by field data. These relationships may be used with field data to estimate unknown flow path geometry in karst aquifers.
Water temperature is a non-conservative tracer. Variations in recharge temperature are damped...
