Articles | Volume 28, issue 20
https://doi.org/10.5194/hess-28-4559-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-28-4559-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
23 Oct 2024
Research article |
| 23 Oct 2024
| 23 Oct 2024
Solutions and case studies for thermally driven reactive transport and porosity evolution in geothermal systems (reactive Lauwerier problem)
Civil and Environmental Engineering, Duke University, Durham, NC, USA
Einat Aharonov
Institute of Earth Sciences, The Hebrew University, Jerusalem, Israel
Piotr Szymczak
Institute of Theoretical Physics, Faculty of Physics, University of Warsaw, Warsaw, Poland
Manolis Veveakis
Civil and Environmental Engineering, Duke University, Durham, NC, USA
Boaz Lazar
Institute of Earth Sciences, The Hebrew University, Jerusalem, Israel
Laura E. Dalton
Civil and Environmental Engineering, Duke University, Durham, NC, USA
Related authors
No articles found.
Rachael Lau, Carolina Seguí, Tyler Waterman, Nathaniel Chaney, and Manolis Veveakis
Nat. Hazards Earth Syst. Sci., 24, 3651–3661, https://doi.org/10.5194/nhess-24-3651-2024, https://doi.org/10.5194/nhess-24-3651-2024, 2024
Short summary
Short summary
This work examines the use of interferometric synthetic-aperture radar (InSAR) alongside in situ borehole measurements to assess the stability of deep-seated landslides for the case study of El Forn (Andorra). Comparing InSAR with borehole data suggests a key trade-off between accuracy and precision for various InSAR resolutions. Spatial interpolation with InSAR informed how many remote observations are necessary to lower error in a remote sensing re-creation of ground motion over the landslide.
Klaus Regenauer-Lieb, Manman Hu, Christoph Schrank, Xiao Chen, Santiago Peña Clavijo, Ulrich Kelka, Ali Karrech, Oliver Gaede, Tomasz Blach, Hamid Roshan, Antoine B. Jacquey, Piotr Szymczak, and Qingpei Sun
Solid Earth, 12, 1829–1849, https://doi.org/10.5194/se-12-1829-2021, https://doi.org/10.5194/se-12-1829-2021, 2021
Short summary
Short summary
This paper presents a trans-disciplinary approach bridging the gap between observations of instabilities from the molecular scale to the very large scale. We show that all scales communicate via propagation of volumetric deformation waves. Similar phenomena are encountered in quantum optics where wave collisions can release sporadic bursts of light. Ocean waves show a similar phenomenon of rogue waves that seem to come from nowhere. This mechanism is proposed to be the trigger for earthquakes.
Hadar Berman, Nathan Paldor, and Boaz Lazar
Ocean Sci. Discuss., https://doi.org/10.5194/os-2017-58, https://doi.org/10.5194/os-2017-58, 2017
Revised manuscript has not been submitted
Short summary
Short summary
The paper develops a new non-dimensional parameter that quantifies the degree to which the surface flow in a given area is thermohaline. The proposed parameter can be easily estimated from cross sections of either salinity or isotopes of oxygen or hydrogen. The parameter was estimated from publicly available data in two areas and in both it has yielded estimates of the rates of evaporation that are consistent with previous detailed observational studies.
Related subject area
Subject: Groundwater hydrology | Techniques and Approaches: Theory development
Identification, mapping, and eco-hydrological signal analysis for groundwater-dependent ecosystems (GDEs) in Langxi River basin, north China
Technical note: Analytical solution for well water response to Earth tides in leaky aquifers with storage and compressibility in the aquitard
Flow recession behavior of preferential subsurface flow patterns with minimum energy dissipation
Towards a hydrogeomorphological understanding of proglacial catchments: an assessment of groundwater storage and release in an Alpine catchment
Effect of topographic slope on the export of nitrate in humid catchments: a 3D model study
Transit Time index (TTi) as an adaptation of the humification index to illustrate transit time differences in karst hydrosystems: application to the karst springs of the Fontaine de Vaucluse system (southeastern France)
In situ estimation of subsurface hydro-geomechanical properties using the groundwater response to semi-diurnal Earth and atmospheric tides
The Thiem team – Adolf and Günther Thiem, two forefathers of hydrogeology
Effects of aquifer geometry on seawater intrusion in annulus segment island aquifers
Depth to water table correction for initial carbon-14 activities in groundwater mean residence time estimation
Preferential pathways for fluid and solutes in heterogeneous groundwater systems: self-organization, entropy, work
Statistical characterization of environmental hot spots and hot moments and applications in groundwater hydrology
Technical note: Disentangling the groundwater response to Earth and atmospheric tides to improve subsurface characterisation
Flowing wells: terminology, history and role in the evolution of groundwater science
Asymmetric impact of groundwater use on groundwater droughts
New model of reactive transport in a single-well push–pull test with aquitard effect and wellbore storage
HESS Opinions: The myth of groundwater sustainability in Asia
Groundwater salinity variation in Upazila Assasuni (southwestern Bangladesh), as steered by surface clay layer thickness, relative elevation and present-day land use
Changes in groundwater drought associated with anthropogenic warming
Application of environmental tracers for investigation of groundwater mean residence time and aquifer recharge in fault-influenced hydraulic drop alluvium aquifers
HESS Opinions: Linking Darcy's equation to the linear reservoir
Effects of microarrangement of solid particles on PCE migration and its remediation in porous media
Hydrological connectivity from glaciers to rivers in the Qinghai–Tibet Plateau: roles of suprapermafrost and subpermafrost groundwater
Temporal variations of groundwater tables and implications for submarine groundwater discharge: a 3-decade case study in central Japan
Consequences and mitigation of saltwater intrusion induced by short-circuiting during aquifer storage and recovery in a coastal subsurface
Understanding groundwater – students' pre-conceptions and conceptual change by means of a theory-guided multimedia learning program
The referential grain size and effective porosity in the Kozeny–Carman model
Approximate analysis of three-dimensional groundwater flow toward a radial collector well in a finite-extent unconfined aquifer
Technical Note: The use of an interrupted-flow centrifugation method to characterise preferential flow in low permeability media
Shallow groundwater thermal sensitivity to climate change and land cover disturbances: derivation of analytical expressions and implications for stream temperature modeling
Confronting the vicinity of the surface water and sea shore in a shallow glaciogenic aquifer in southern Finland
Residence times and mixing of water in river banks: implications for recharge and groundwater–surface water exchange
Using 14C and 3H to understand groundwater flow and recharge in an aquifer window
Hydrogeology of an Alpine rockfall aquifer system and its role in flood attenuation and maintaining baseflow
Mobilisation or dilution? Nitrate response of karst springs to high rainfall events
Transferring the concept of minimum energy dissipation from river networks to subsurface flow patterns
Spectral induced polarization measurements for predicting the hydraulic conductivity in sandy aquifers
Transient analysis of fluctuations of electrical conductivity as tracer in the stream bed
Teaching hydrogeology: a review of current practice
Transient flow between aquifers and surface water: analytically derived field-scale hydraulic heads and fluxes
Influence of initial heterogeneities and recharge limitations on the evolution of aperture distributions in carbonate aquifers
Impact of climate change on groundwater point discharge: backflooding of karstic springs (Loiret, France)
Stream depletion rate with horizontal or slanted wells in confined aquifers near a stream
Tidal propagation in an oceanic island with sloping beaches
Mingyang Li, Fulin Li, Shidong Fu, Huawei Chen, Kairan Wang, Xuequn Chen, and Jiwen Huang
Hydrol. Earth Syst. Sci., 28, 4623–4642, https://doi.org/10.5194/hess-28-4623-2024, https://doi.org/10.5194/hess-28-4623-2024, 2024
Short summary
Short summary
Research on groundwater-dependent ecosystems (GDEs) started earlier, but because there is no good identification and classification method, most of the related research is concentrated in Europe and Australia. In this study, the lower Yellow River basin in northern China, with well-developed karsts, was selected as the study area, and a four-diagnostic-criteria framework for identifying the GDEs based on remote sensing, GIS data dredging, and hydrogeological surveys was proposed.
Rémi Valois, Agnès Rivière, Jean-Michel Vouillamoz, and Gabriel C. Rau
Hydrol. Earth Syst. Sci., 28, 1041–1054, https://doi.org/10.5194/hess-28-1041-2024, https://doi.org/10.5194/hess-28-1041-2024, 2024
Short summary
Short summary
Characterizing aquifer systems is challenging because it is difficult to obtain in situ information. They can, however, be characterized using natural forces such as Earth tides. Models that account for more complex situations are still necessary to extend the use of Earth tides to assess hydromechanical properties of aquifer systems. Such a model is developed in this study and applied to a case study in Cambodia, where a combination of tides was used in order to better constrain the model.
Jannick Strüven and Stefan Hergarten
Hydrol. Earth Syst. Sci., 27, 3041–3058, https://doi.org/10.5194/hess-27-3041-2023, https://doi.org/10.5194/hess-27-3041-2023, 2023
Short summary
Short summary
This study uses dendritic flow patterns to analyze the recession behavior of aquifer springs. The results show that the long-term recession becomes slower for large catchments. After a short recharge event, however, the short-term behavior differs strongly from the exponential recession that would be expected from a linear reservoir. The exponential component still accounts for more than 80 % of the total discharge, much more than typically assumed for karst aquifers.
Tom Müller, Stuart N. Lane, and Bettina Schaefli
Hydrol. Earth Syst. Sci., 26, 6029–6054, https://doi.org/10.5194/hess-26-6029-2022, https://doi.org/10.5194/hess-26-6029-2022, 2022
Short summary
Short summary
This research provides a comprehensive analysis of groundwater storage in Alpine glacier forefields, a zone rapidly evolving with glacier retreat. Based on data analysis of a case study, it provides a simple perceptual model showing where and how groundwater is stored and released in a high Alpine environment. It especially points out the presence of groundwater storages in both fluvial and bedrock aquifers, which may become more important with future glacier retreat.
Jie Yang, Qiaoyu Wang, Ingo Heidbüchel, Chunhui Lu, Yueqing Xie, Andreas Musolff, and Jan H. Fleckenstein
Hydrol. Earth Syst. Sci., 26, 5051–5068, https://doi.org/10.5194/hess-26-5051-2022, https://doi.org/10.5194/hess-26-5051-2022, 2022
Short summary
Short summary
We assessed the effect of catchment topographic slopes on the nitrate export dynamics in terms of the nitrogen mass fluxes and concentration level using a coupled surface–subsurface model. We found that flatter landscapes tend to retain more nitrogen mass in the soil and export less nitrogen mass to the stream, explained by the reduced leaching and increased potential of degradation in flat landscapes. We emphasized that stream water quality is potentially less vulnerable in flatter landscapes.
Leïla Serène, Christelle Batiot-Guilhe, Naomi Mazzilli, Christophe Emblanch, Milanka Babic, Julien Dupont, Roland Simler, Matthieu Blanc, and Gérard Massonnat
Hydrol. Earth Syst. Sci., 26, 5035–5049, https://doi.org/10.5194/hess-26-5035-2022, https://doi.org/10.5194/hess-26-5035-2022, 2022
Short summary
Short summary
This work aims to develop the Transit Time index (TTi) as a natural tracer of karst groundwater transit time, usable in the 0–6-month range. Based on the fluorescence of organic matter, TTi shows its relevance to detect a small proportion of fast infiltration water within a mix, while other natural transit time tracers provide no or less sensitive information. Comparison of the average TTi of different karst springs also provides consistent results with the expected relative transit times.
Gabriel C. Rau, Timothy C. McMillan, Martin S. Andersen, and Wendy A. Timms
Hydrol. Earth Syst. Sci., 26, 4301–4321, https://doi.org/10.5194/hess-26-4301-2022, https://doi.org/10.5194/hess-26-4301-2022, 2022
Short summary
Short summary
This work develops and applies a new method to estimate hydraulic and geomechanical subsurface properties in situ using standard groundwater and atmospheric pressure records. The estimated properties comply with expected values except for the Poisson ratio, which we attribute to the investigated scale and conditions. Our new approach can be used to cost-effectively investigate the subsurface using standard monitoring datasets.
Georg J. Houben and Okke Batelaan
Hydrol. Earth Syst. Sci., 26, 4055–4091, https://doi.org/10.5194/hess-26-4055-2022, https://doi.org/10.5194/hess-26-4055-2022, 2022
Short summary
Short summary
Unbeknown to most hydrologists, many methods used in groundwater hydrology today go back to work by Adolf and Günther Thiem. Their work goes beyond the Dupuit–Thiem analytical model for pump tests mentioned in many textbooks. It includes, e.g., the development and improvement of isopotential maps, tracer tests, and vertical well constructions. Extensive literature and archive research has been conducted to identify how and where the Thiems developed their methods and how they spread.
Zhaoyang Luo, Jun Kong, Chengji Shen, Pei Xin, Chunhui Lu, Ling Li, and David Andrew Barry
Hydrol. Earth Syst. Sci., 25, 6591–6602, https://doi.org/10.5194/hess-25-6591-2021, https://doi.org/10.5194/hess-25-6591-2021, 2021
Short summary
Short summary
Analytical solutions are derived for steady-state seawater intrusion in annulus segment aquifers. These analytical solutions are validated by comparing their predictions with experimental data. We find seawater intrusion is the most extensive in divergent aquifers, and the opposite is the case for convergent aquifers. The analytical solutions facilitate engineers and hydrologists in evaluating seawater intrusion more efficiently in annulus segment aquifers with a complex geometry.
Dylan J. Irvine, Cameron Wood, Ian Cartwright, and Tanya Oliver
Hydrol. Earth Syst. Sci., 25, 5415–5424, https://doi.org/10.5194/hess-25-5415-2021, https://doi.org/10.5194/hess-25-5415-2021, 2021
Short summary
Short summary
It is widely assumed that 14C is in contact with the atmosphere until recharging water reaches the water table. Unsaturated zone (UZ) studies have shown that 14C decreases with depth below the land surface. We produce a relationship between UZ 14C and depth to the water table to estimate input 14C activities for groundwater age estimation. Application of the new relationship shows that it is important for UZ processes to be considered in groundwater mean residence time estimation.
Erwin Zehe, Ralf Loritz, Yaniv Edery, and Brian Berkowitz
Hydrol. Earth Syst. Sci., 25, 5337–5353, https://doi.org/10.5194/hess-25-5337-2021, https://doi.org/10.5194/hess-25-5337-2021, 2021
Short summary
Short summary
This study uses the concepts of entropy and work to quantify and explain the emergence of preferential flow and transport in heterogeneous saturated porous media. We found that the downstream concentration of solutes in preferential pathways implies a downstream declining entropy in the transverse distribution of solute transport pathways. Preferential flow patterns with lower entropies emerged within media of higher heterogeneity – a stronger self-organization despite a higher randomness.
Jiancong Chen, Bhavna Arora, Alberto Bellin, and Yoram Rubin
Hydrol. Earth Syst. Sci., 25, 4127–4146, https://doi.org/10.5194/hess-25-4127-2021, https://doi.org/10.5194/hess-25-4127-2021, 2021
Short summary
Short summary
We developed a stochastic framework with indicator random variables to characterize the spatiotemporal distribution of environmental hot spots and hot moments (HSHMs) that represent rare locations and events exerting a disproportionate influence over the environment. HSHMs are characterized by static and dynamic indicators. This framework is advantageous as it allows us to calculate the uncertainty associated with HSHMs based on uncertainty associated with its contributors.
Gabriel C. Rau, Mark O. Cuthbert, R. Ian Acworth, and Philipp Blum
Hydrol. Earth Syst. Sci., 24, 6033–6046, https://doi.org/10.5194/hess-24-6033-2020, https://doi.org/10.5194/hess-24-6033-2020, 2020
Short summary
Short summary
This work provides an important generalisation of a previously developed method that quantifies subsurface barometric efficiency using the groundwater level response to Earth and atmospheric tides. The new approach additionally allows the quantification of hydraulic conductivity and specific storage. This enables improved and rapid assessment of subsurface processes and properties using standard pressure measurements.
Xiao-Wei Jiang, John Cherry, and Li Wan
Hydrol. Earth Syst. Sci., 24, 6001–6019, https://doi.org/10.5194/hess-24-6001-2020, https://doi.org/10.5194/hess-24-6001-2020, 2020
Short summary
Short summary
The gushing of water from flowing wells is a natural phenomenon of interest to the public. This review demonstrates that this spectacular phenomenon also instigated the science of groundwater and can be considered a root of groundwater hydrology. Observations of flowing wells not only led to the foundation of many principles of traditional groundwater hydrology but also played a vital role in the paradigm shift from aquitard-bound flow to cross-formational flow driven by topography.
Doris E. Wendt, Anne F. Van Loon, John P. Bloomfield, and David M. Hannah
Hydrol. Earth Syst. Sci., 24, 4853–4868, https://doi.org/10.5194/hess-24-4853-2020, https://doi.org/10.5194/hess-24-4853-2020, 2020
Short summary
Short summary
Groundwater use changes the availability of groundwater, especially during droughts. This study investigates the impact of groundwater use on groundwater droughts. A methodological framework is presented that was developed and applied to the UK. We identified an asymmetric impact of groundwater use on droughts, which highlights the relation between short-term and long-term strategies for sustainable groundwater use.
Quanrong Wang, Junxia Wang, Hongbin Zhan, and Wenguang Shi
Hydrol. Earth Syst. Sci., 24, 3983–4000, https://doi.org/10.5194/hess-24-3983-2020, https://doi.org/10.5194/hess-24-3983-2020, 2020
Franklin W. Schwartz, Ganming Liu, and Zhongbo Yu
Hydrol. Earth Syst. Sci., 24, 489–500, https://doi.org/10.5194/hess-24-489-2020, https://doi.org/10.5194/hess-24-489-2020, 2020
Short summary
Short summary
We are concerned about the sad state of affairs around groundwater in the developing countries of Asia and the obvious implications for sustainability. Groundwater production for irrigated agriculture has led to water-level declines that continue to worsen. Yet in the most populous countries, China, India, Pakistan, and Iran, there are only token efforts towards evidence-based sustainable management. It is unrealistic to expect evidence-based groundwater sustainability to develop any time soon.
Floris Loys Naus, Paul Schot, Koos Groen, Kazi Matin Ahmed, and Jasper Griffioen
Hydrol. Earth Syst. Sci., 23, 1431–1451, https://doi.org/10.5194/hess-23-1431-2019, https://doi.org/10.5194/hess-23-1431-2019, 2019
Short summary
Short summary
In this paper, we postulate a possible evolution of the groundwater salinity around a village in southwestern Bangladesh, based on high-density fieldwork. We identified that the thickness of the surface clay layer, the surface elevation and the present-day land use determine whether fresh or saline groundwater has formed. The outcomes show how the large groundwater salinity variation in southwestern Bangladesh can be understood, which is valuable for the water management in the region.
John P. Bloomfield, Benjamin P. Marchant, and Andrew A. McKenzie
Hydrol. Earth Syst. Sci., 23, 1393–1408, https://doi.org/10.5194/hess-23-1393-2019, https://doi.org/10.5194/hess-23-1393-2019, 2019
Short summary
Short summary
Groundwater is susceptible to drought due to natural variations in climate; however, to date there is no evidence of a relationship between climate change and groundwater drought. Using two long groundwater level records from the UK, we document increases in frequency, magnitude and intensity and changes in duration of groundwater drought associated with climate warming and infer that, given the extent of shallow groundwater globally, warming may widely effect changes to groundwater droughts.
Bin Ma, Menggui Jin, Xing Liang, and Jing Li
Hydrol. Earth Syst. Sci., 23, 427–446, https://doi.org/10.5194/hess-23-427-2019, https://doi.org/10.5194/hess-23-427-2019, 2019
Short summary
Short summary
Groundwater supplies the most freshwater for industrial and agricultural production and domestic use in the arid northwest of China. This research uses environmental tracers to enhance one's understanding of groundwater, including aquifer recharge sources and groundwater mean residence times in the alluvium aquifers. The results provide valuable implications for groundwater resources regulation and sustainable development and have practical significance for other arid areas.
Hubert H. G. Savenije
Hydrol. Earth Syst. Sci., 22, 1911–1916, https://doi.org/10.5194/hess-22-1911-2018, https://doi.org/10.5194/hess-22-1911-2018, 2018
Short summary
Short summary
This paper provides the connection between two simple equations describing groundwater flow at different scales: the Darcy equation describes groundwater flow at pore scale, the linear reservoir equation at catchment scale. The connection between the two appears to be very simple. The two parameters of the equations are proportional, depending on the porosity of the subsoil and the resistance for the groundwater to enter the surface drainage network.
Ming Wu, Jianfeng Wu, Jichun Wu, and Bill X. Hu
Hydrol. Earth Syst. Sci., 22, 1001–1015, https://doi.org/10.5194/hess-22-1001-2018, https://doi.org/10.5194/hess-22-1001-2018, 2018
Short summary
Short summary
Fractal models of regular triangle arrangement (RTA) and square pitch arrangement (SPA) are developed in this study. Results suggest RTA can cause more groundwater contamination and make remediation more difficult. In contrast, the cleanup of contaminants in aquifers with SPA is easier. This study demonstrates how microscale arrangements control contaminant migration and remediation, which is helpful in designing successful remediation schemes for subsurface contamination.
Rui Ma, Ziyong Sun, Yalu Hu, Qixin Chang, Shuo Wang, Wenle Xing, and Mengyan Ge
Hydrol. Earth Syst. Sci., 21, 4803–4823, https://doi.org/10.5194/hess-21-4803-2017, https://doi.org/10.5194/hess-21-4803-2017, 2017
Short summary
Short summary
The roles of groundwater flow in the hydrological cycle within the alpine area characterized by permafrost or seasonal frost are poorly known. We investigated the role of permafrost in controlling groundwater flow and hydrological connections between glaciers and river. The recharge, flow path and discharge of permafrost groundwater at the study site were explored. Two mechanisms were proposed to explain the significantly seasonal variation in interaction between groundwater and surface water.
Bing Zhang, Jing Zhang, and Takafumi Yoshida
Hydrol. Earth Syst. Sci., 21, 3417–3425, https://doi.org/10.5194/hess-21-3417-2017, https://doi.org/10.5194/hess-21-3417-2017, 2017
Short summary
Short summary
Since groundwater is the linkage between climate changes and fresh submarine groundwater discharge, the variations of and relationships among monthly groundwater table, rainfall, snowfall, and climate change events from 1985 to 2015 were analyzed by wavelet coherence to discuss the implications for climate changes. The results show the increase in precipitation and the groundwater table, indicating that fresh submarine groundwater discharge flux may increase under climate change.
Koen Gerardus Zuurbier and Pieter Jan Stuyfzand
Hydrol. Earth Syst. Sci., 21, 1173–1188, https://doi.org/10.5194/hess-21-1173-2017, https://doi.org/10.5194/hess-21-1173-2017, 2017
Short summary
Short summary
The subsurface is increasingly perforated for exploitation of water and energy. This has increased the risk of leakage between originally separated aquifers. It is shown how this leakage can have a very negative impact on the recovery of freshwater during aquifer storage and recovery (ASR) in brackish-saline aquifers. Deep interception of intruding brackish-saline water can mitigate the negative effects and buoyancy of freshwater to some extent, but not completely.
Ulrike Unterbruner, Sylke Hilberg, and Iris Schiffl
Hydrol. Earth Syst. Sci., 20, 2251–2266, https://doi.org/10.5194/hess-20-2251-2016, https://doi.org/10.5194/hess-20-2251-2016, 2016
Short summary
Short summary
Studies show that young people have difficulties with correctly understanding groundwater. We designed a multimedia learning program about groundwater and tested its learning efficacy with pupils and teacher-training students. A novelty is the theory-guided designing of the program on the basis of hydrogeology and science education. The pupils and students greatly benefited from working through the multimedia learning program.
Kosta Urumović and Kosta Urumović Sr.
Hydrol. Earth Syst. Sci., 20, 1669–1680, https://doi.org/10.5194/hess-20-1669-2016, https://doi.org/10.5194/hess-20-1669-2016, 2016
Short summary
Short summary
Calculation of hydraulic conductivity of porous materials is crucial for further use in hydrogeological modeling. The Kozeny–Carman model is theoretically impeccable but has not been properly used in recent scientific and expert literature. In this paper, proper use of the Kozeny-Carman formula is given through presentation of geometric mean grain size in the drilled-core sample as the referential mean grain size. Also, procedures for identification of real effective porosity of porous media are presented.
C.-S. Huang, J.-J. Chen, and H.-D. Yeh
Hydrol. Earth Syst. Sci., 20, 55–71, https://doi.org/10.5194/hess-20-55-2016, https://doi.org/10.5194/hess-20-55-2016, 2016
Short summary
Short summary
Existing solutions for the problem of pumping at a radial collector well (RCW) in unconfined aquifers either require laborious calculation or predict divergent results at a middle period of pumping. This study relaxes the above two limitations to develop a new analytical solution for the problem. The application of the solution is convenient for those who are not familiar with numerical methods. New findings regarding the responses of flow to pumping at RCW are addressed.
R. A. Crane, M. O. Cuthbert, and W. Timms
Hydrol. Earth Syst. Sci., 19, 3991–4000, https://doi.org/10.5194/hess-19-3991-2015, https://doi.org/10.5194/hess-19-3991-2015, 2015
Short summary
Short summary
We present an interrupted-flow centrifugation technique to characterise the vertical hydraulic properties of dual porosity, low permeability media. Use of large core samples (100mm diameter) enables hydraulic-conductivity-scale issues in dual porosity media to be overcome. Elevated centrifugal force also enables simulating in situ total stress conditions. The methodology is an important tool to assess the ability of dual porosity aquitards to protect underlying aquifer systems.
B. L. Kurylyk, K. T. B. MacQuarrie, D. Caissie, and J. M. McKenzie
Hydrol. Earth Syst. Sci., 19, 2469–2489, https://doi.org/10.5194/hess-19-2469-2015, https://doi.org/10.5194/hess-19-2469-2015, 2015
Short summary
Short summary
Changes in climate and land cover are known to warm streams by altering surface heat fluxes. However, the influence of these disturbances on shallow groundwater temperature are not as well understood. In small streams, groundwater discharge may also exert a control on stream temperature, and thus groundwater warming may eventually produce additional stream warming not considered in most existing models. This study investigates these processes and suggests stream temperature model improvements.
S. Luoma, J. Okkonen, K. Korkka-Niemi, N. Hendriksson, and B. Backman
Hydrol. Earth Syst. Sci., 19, 1353–1370, https://doi.org/10.5194/hess-19-1353-2015, https://doi.org/10.5194/hess-19-1353-2015, 2015
N. P. Unland, I. Cartwright, D. I. Cendón, and R. Chisari
Hydrol. Earth Syst. Sci., 18, 5109–5124, https://doi.org/10.5194/hess-18-5109-2014, https://doi.org/10.5194/hess-18-5109-2014, 2014
Short summary
Short summary
Periodic flooding of rivers should result in increased groundwater recharge near rivers and thus - younger and fresher groundwater near rivers. This study found the age and salinity of shallow groundwater to increase with proximity to the Tambo River in South East Australia. This appears to be due to the upwelling of older, regional groundwater closer the river. Other chemical parameters are consistent with this. This is a process that may be occurring in other similar river systems.
A. P. Atkinson, I. Cartwright, B. S. Gilfedder, D. I. Cendón, N. P. Unland, and H. Hofmann
Hydrol. Earth Syst. Sci., 18, 4951–4964, https://doi.org/10.5194/hess-18-4951-2014, https://doi.org/10.5194/hess-18-4951-2014, 2014
Short summary
Short summary
This research article uses of radiogenic isotopes, stable isotopes and groundwater geochemistry to study groundwater age and recharge processes in the Gellibrand Valley, a relatively unstudied catchment and potential groundwater resource. The valley is found to contain both "old", regionally recharged groundwater (300-10,000 years) in the near-river environment, and modern groundwater (0-100 years old) further back on the floodplain. There is no recharge of the groundwater by high river flows.
U. Lauber, P. Kotyla, D. Morche, and N. Goldscheider
Hydrol. Earth Syst. Sci., 18, 4437–4452, https://doi.org/10.5194/hess-18-4437-2014, https://doi.org/10.5194/hess-18-4437-2014, 2014
M. Huebsch, O. Fenton, B. Horan, D. Hennessy, K. G. Richards, P. Jordan, N. Goldscheider, C. Butscher, and P. Blum
Hydrol. Earth Syst. Sci., 18, 4423–4435, https://doi.org/10.5194/hess-18-4423-2014, https://doi.org/10.5194/hess-18-4423-2014, 2014
S. Hergarten, G. Winkler, and S. Birk
Hydrol. Earth Syst. Sci., 18, 4277–4288, https://doi.org/10.5194/hess-18-4277-2014, https://doi.org/10.5194/hess-18-4277-2014, 2014
M. Attwa and T. Günther
Hydrol. Earth Syst. Sci., 17, 4079–4094, https://doi.org/10.5194/hess-17-4079-2013, https://doi.org/10.5194/hess-17-4079-2013, 2013
C. Schmidt, A. Musolff, N. Trauth, M. Vieweg, and J. H. Fleckenstein
Hydrol. Earth Syst. Sci., 16, 3689–3697, https://doi.org/10.5194/hess-16-3689-2012, https://doi.org/10.5194/hess-16-3689-2012, 2012
T. Gleeson, D. M. Allen, and G. Ferguson
Hydrol. Earth Syst. Sci., 16, 2159–2168, https://doi.org/10.5194/hess-16-2159-2012, https://doi.org/10.5194/hess-16-2159-2012, 2012
G. H. de Rooij
Hydrol. Earth Syst. Sci., 16, 649–669, https://doi.org/10.5194/hess-16-649-2012, https://doi.org/10.5194/hess-16-649-2012, 2012
B. Hubinger and S. Birk
Hydrol. Earth Syst. Sci., 15, 3715–3729, https://doi.org/10.5194/hess-15-3715-2011, https://doi.org/10.5194/hess-15-3715-2011, 2011
E. Joigneaux, P. Albéric, H. Pauwels, C. Pagé, L. Terray, and A. Bruand
Hydrol. Earth Syst. Sci., 15, 2459–2470, https://doi.org/10.5194/hess-15-2459-2011, https://doi.org/10.5194/hess-15-2459-2011, 2011
P.-R. Tsou, Z.-Y. Feng, H.-D. Yeh, and C.-S. Huang
Hydrol. Earth Syst. Sci., 14, 1477–1485, https://doi.org/10.5194/hess-14-1477-2010, https://doi.org/10.5194/hess-14-1477-2010, 2010
Y.-C. Chang, D.-S. Jeng, and H.-D. Yeh
Hydrol. Earth Syst. Sci., 14, 1341–1351, https://doi.org/10.5194/hess-14-1341-2010, https://doi.org/10.5194/hess-14-1341-2010, 2010
Cited articles
Abbasi, M., Khazali, N., and Sharifi, M.: Analytical model for convection-conduction heat transfer during water injection in fractured geothermal reservoirs with variable rock matrix block size, Geothermics, 69, 1–14, 2017.
Agar, S. M. and Geiger, S.: Fundamental controls on fluid flow in carbonates: current workflows to emerging technologies, Geol. Soc. Lond. Spec. Publ., 406, 1–59, 2015.
Aharonov, E., Whitehead, J. A., Kelemen, P. B., and Spiegelman, M.: Channeling instability of upwelling melt in the mantle, J. Geophys. Res.-Solid, 100, 20433, https://doi.org/10.1029/95JB01307, 1995.
Aharonov, E., Spiegelman, M., and Kelemen, P.: Three-dimensional flow and reaction in porous media: Implications for the Earth's mantle and sedimentary basins, J. Geophys. Res.-Solid, 102, 14821–14833, 1997.
Aharonov, E., Tenthorey, E., and Scholz, C. H.: Precipitation sealing and diagenesis: 2. Theoretical analysis, J. Geophys. Res.-Solid, 103, 969–981, 1998.
Al-Sulaimi, B.: The energy stability of Darcy thermosolutal convection with reaction, Int. J. Heat Mass Transf., 86, 369–376, 2015.
Anderson, M. P., Woessner, W. W., and Hunt, R. J.: Applied groundwater modeling: simulation of flow and advective transport, Academic Press, ISBN 978-0-12-058103-0, 2015.
Andre, B. J. and Rajaram, H.: Dissolution of limestone fractures by cooling waters: Early development of hypogene karst systems, Water Resour. Res., 41, W01015, https://doi.org/10.1029/2004WR003331, 2005.
Bear, J. and Cheng, A. H.-D.: Modeling groundwater flow and contaminant transport, Springer Science & Business Media, https://doi.org/10.1007/978-1-4020-6682-5, 2010.
Bekri, S., Thovert, J. F., and Adler, P. M.: Dissolution of porous media, Chem. Eng. Sci., 50, 2765–2791, 1995.
Bhat, S. and Kovscek, A.: Permeability modification of diatomite during hot fluid injection, in: SPE Western Regional Meeting, Bakersfield, California, May 1998, https://doi.org/10.2118/46210-MS, 1998.
Bonte, M., Stuyfzand, P. J., and Breukelen, B. M. van: Reactive transport modeling of thermal column experiments to investigate the impacts of aquifer thermal energy storage on groundwater quality, Environ. Sci. Technol., 48, 12099–12107, 2014.
Budek, A. and Szymczak, P.: Network models of dissolution of porous media, Phys. Rev. E, 86, 056318, https://doi.org/10.1103/PhysRevE.86.056318, 2012.
Carroll, S., Mroczek, E., Alai, M., and Ebert, M.: Amorphous silica precipitation (60 to 120 °C): Comparison of laboratory and field rates, Geochim. Cosmochim. Ac., 62, 1379–1396, 1998.
Chadam, J., Hoff, D., Merino, E., Ortoleva, P., and Sen, A.: Reactive infiltration instabilities, IMA J. Appl. Math., 36, 207–221, 1986.
Chaudhuri, A., Rajaram, H., and Viswanathan, H.: Early-stage hypogene karstification in a mountain hydrologic system: A coupled thermohydrochemical model incorporating buoyant convection, Water Resour. Res., 49, 5880–5899, 2013.
Chen, C. and Reddell, D. L.: Temperature distribution around a well during thermal injection and a graphical technique for evaluating aquifer thermal properties, Water Resour. Res., 19, 351–363, 1983.
Corson, L. T. and Pritchard, D.: Thermosolutal convection in an evolving soluble porous medium, J. Fluid Mech., 832, 666–696, 2017.
Coudrain-Ribstein, A., Gouze, P., and de Marsily, G.: Temperature-carbon dioxide partial pressure trends in confined aquifers, Chem. Geol., 145, 73–89, 1998.
Craw, D.: Fluid flow at fault intersections in an active oblique collision zone, Southern Alps, New Zealand, J. Geochem. Explor., 69, 523–526, 2000.
Daccord, G.: Chemical Dissolution of a Porous Medium by a Reactive Fluid, Phys. Rev. Lett., 58, 479–482, 1987.
Dávila, G., Dalton, L., Crandall, D. M., Garing, C., Werth, C. J., and Druhan, J. L.: Reactive alteration of a Mt. Simon Sandstone due to CO2-rich brine displacement, Geochim. Cosmochim. Ac., 271, 227–247, https://doi.org/10.1016/j.gca.2019.12.015, 2020.
Deng, H. and Spycher, N.: Modeling reactive transport processes in fractures, Rev. Mineral. Geochem., 85, 49–74, 2019.
Deng, H., Molins, S., Trebotich, D., Steefel, C., and DePaolo, D.: Pore-scale numerical investigation of the impacts of surface roughness: Upscaling of reaction rates in rough fractures, Geochim. Cosmochim. Ac., 239, 374–389, 2018.
Detwiler, R. L. and Rajaram, H.: Predicting dissolution patterns in variable aperture fractures: Evaluation of an enhanced depth-averaged computational model, Water Resour. Res., 43, W04403, https://doi.org/10.1029/2006WR005147, 2007.
Diaz, A. R., Kaya, E., and Zarrouk, S. J.: Reinjection in geothermal fields- A worldwide review update, Renew. Sustain. Energ. Rev., 53, 105–162, 2016.
Diersch, H.-J. and Kolditz, O.: Variable-density flow and transport in porous media: approaches and challenges, Adv. Water Resour., 25, 899–944, 2002.
Dove, P. M. and Crerar, D. A.: Kinetics of quartz dissolution in electrolyte solutions using a hydrothermal mixed flow reactor, Geochim. Cosmochim. Ac., 54, 955–969, 1990.
Dreybrodt, W.: Processes in karst systems: physics, chemistry, and geology, Springer Verlag, Berlin, New York, xii, 288 pp., https://doi.org/10.1007/978-3-642-83352-6, 1988.
Dreybrodt, W., Gabrovšek, F., and Romanov, D.: Processes of speleogenesis: A modeling approach, Carsologica, edited by: Gabrovšek, F., Založba ZRC, Ljubljana, 375 pp., ISBN 961-6500-91-0, 2005.
Fleuchaus, P., Godschalk, B., Stober, I., and Blum, P.: Worldwide application of aquifer thermal energy storage – A review, Renew. Sustain. Energ. Rev., 94, 861–876, 2018.
Frick, S., Regenspurg, S., Kranz, S., Milsch, H., Saadat, A., Francke, H., Brandt, W., and Huenges, E.: Geochemical and process engineering challenges for geothermal power generation, Chem. Ing. Tech., 83, 2093–2104, https://doi.org/10.1002/cite.201100131, 2011.
Garing, C., Gouze, P., Kassab, M., Riva, M., and Guadagnini, A.: Anti-correlated porosity–permeability changes during the dissolution of carbonate rocks: experimental evidences and modeling, Transp. Porous Media, 107, 595–621, 2015.
Glassley, W. E.: Geothermal energy: renewable energy and the environment, CRC Press, https://doi.org/10.1201/b17521, 2014.
Goldscheider, N., Mádl-Szőnyi, J., Erőss, A., and Schill, E.: Thermal water resources in carbonate rock aquifers, Hydrogeol. J., 18, 1303–1318, 2010.
Golfier, F., Zarcone, C., Bazin, B., Lenormand, R., Lasseux, D., and Quintard, M.: On the ability of a Darcy-scale model to capture wormhole formation during the dissolution of a porous medium, J. Fluid Mech., 457, 213–254, 2002.
Grodzki, P. and Szymczak, P.: Reactive-infiltration instability in radial geometry: From dissolution fingers to star patterns, Phys. Rev. E, 100, 033108, https://doi.org/10.1103/PhysRevE.100.033108, 2019.
Hao, Y., Smith, M., Sholokhova, Y., and Carroll, S.: CO2-induced dissolution of low permeability carbonates. Part II: Numerical modeling of experiments, Adv. Water Resour., 62, 388–408, 2013.
Hoefner, M. L. and Fogler, H. S.: Pore evolution and channel formation during flow and reaction in porous media, AICHE J., 34, 45–54, 1988.
Hommel, J., Coltman, E., and Class, H.: Porosity–permeability relations for evolving pore space: a review with a focus on (bio-) geochemically altered porous media, Transp. Porous Media, 124, 589–629, 2018.
Huenges, E. and Ledru, P.: Geothermal energy systems: exploration, development, and utilization, John Wiley & Sons, https://doi.org/10.1002/9783527630479, 2011.
Huenges, E., Kohl, T., Kolditz, O., Bremer, J., Scheck-Wenderoth, M., and Vienken, T.: Geothermal energy systems: research perspective for domestic energy provision, Environ. Earth Sci., 70, 3927–3933, 2013.
Hussaini, S. R. and Dvorkin, J.: Specific surface area versus porosity from digital images, J. Petrol. Sci. Eng., 196, 107773, https://doi.org/10.1016/j.petrol.2020.107773, 2021.
Jamtveit, B. and Yardley, B.: Fluid flow and transport in rocks: mechanisms and effects, Springer Science & Business Media, https://doi.org/10.1007/978-94-009-1533-6, 1996.
Ji, J., Song, X., Song, G., Xu, F., Shi, Y., Lv, Z., Li, S., and Yi, J.: Study on fracture evolution model of the enhanced geothermal system under thermal-hydraulic-chemical-deformation coupling, Energy, 269, 126604, https://doi.org/10.1016/j.energy.2022.126604, 2023.
Jones, G. D. and Xiao, Y.: Geothermal convection in the Tengiz carbonate platform, Kazakhstan: Reactive transport models of diagenesis and reservoir quality, AAPG Bull., 90, 1251–1272, 2006.
Jupp, T. and Woods, A.: Thermally driven reaction fronts in porous media, J. Fluid Mech., 484, 329–346, 2003.
Jupp, T. and Woods, A.: Reaction fronts in a porous medium following injection along a temperature gradient, J. Fluid Mech., 513, 343–361, 2004.
Kalia, N. and Balakotaiah, V.: Modeling and analysis of wormhole formation in reactive dissolution of carbonate rocks, Chem. Eng. Sci., 62, 919–928, 2007.
Kelemen, P. B., Whitehead, J. A., Aharonov, E., and Jordahl, K. A.: Experiments on flow focusing in soluble porous media, with applications to melt extraction from the mantle, J. Geophys. Res.-Solid, 100, 475–496, 1995.
Kolditz, O., Shao, H., Wang, W., and Bauer, S.: Thermo-Hydro-Mechanical Chemical Processes in Fractured Porous Media: Modelling and Benchmarking, Springer, https://doi.org/10.1007/978-3-319-29224-3, 2016.
Ladd, A. J. and Szymczak, P.: Reactive Flows in Porous Media: Challenges in Theoretical and Numerical Methods, Annu. Rev. Chem. Biomol. Eng., 12, 543–571, https://doi.org/10.1146/annurev-chembioeng-092920-102703, 2021.
Ladd, A. J. C. and Szymczak, P.: Use and misuse of large-density asymptotics in the reaction-infiltration instability, Water Resour. Res., 53, 2419–2430, 2017.
Lai, P., Moulton, K., and Krevor, S.: Pore-scale heterogeneity in the mineral distribution and reactive surface area of porous rocks, Chem. Geol., 411, 260–273, 2015.
Lauwerier, H.: The transport of heat in an oil layer caused by the injection of hot fluid, Appl. Sci. Res. Sect. A, 5, 145–150, 1955.
Lichtner, P. C.: The Quasi-Stationary State Approximation to Fluid/Rock Reaction: Local Equilibrium Revisited, in: Diffusion, Atomic Ordering, and Mass Transport: Selected Topics in Geochemistry, edited by: Ganguly, J., Springer US, New York, NY, 452–560, https://doi.org/10.1007/978-1-4613-9019-0_13, 1991.
Lin, Y., Hu, T., and Yeh, H.: Analytical model for heat transfer accounting for both conduction and dispersion in aquifers with a Robin-type boundary condition at the injection well, Water Resour. Res., 55, 7379–7399, 2019.
Lu, P., Luo, P., Zhang, G., Zhang, S., and Zhu, C.: A mineral-water-gas interaction model of pCO2 as a function of temperature in sedimentary basins, Chem. Geol., 558, 119868, https://doi.org/10.1016/j.chemgeo.2020.119868, 2020.
Lucia, F. J.: Carbonate reservoir characterization: An integrated approach, in 2nd Edn., Springer-Verlag, Berlin, Heidelberg, ISBN 978-3-540-72740-8, 2007.
Maher, K., Steefel, C. I., DePaolo, D. J., and Viani, B. E.: The mineral dissolution rate conundrum: Insights from reactive transport modeling of U isotopes and pore fluid chemistry in marine sediments, Geochim. Cosmochim. Ac., 70, 337–363, 2006.
Maliva, R. G.: Anthropogenic aquifer recharge: WSP methods in water resources evaluation series no. 5, Springer, https://doi.org/10.1007/978-3-030-11084-0, 2019.
MATLAB: Version R2022b, Natick Mass. MathWorks Inc, https://www.mathworks.com (last access: 6 Septeber 2023), 2022.
Micklethwaite, S. and Cox, S. F.: Progressive fault triggering and fluid flow in aftershock domains: Examples from mineralized Archaean fault systems, Earth Planet. Sc. Lett., 250, 318–330, 2006.
Mostaghimi, P., Blunt, M. J., and Bijeljic, B.: Computations of absolute permeability on micro-CT images, Math. Geosci., 45, 103–125, 2013.
Narr, W. and Suppe, J.: Joint spacing in sedimentary rocks, J. Struct. Geol., 13, 1037–1048, 1991.
Nield, D. A. and Bejan, A.: Convection in Porous Media, Springer, https://doi.org/10.1007/978-3-319-49562-0_4, 2017.
Niemi, A., Bear, J., and Bensabat, J.: Geological Storage of CO2 in Deep Saline Formations, Springer, https://doi.org/10.1007/978-94-024-0996-3, 2017.
Noiriel, C.: Resolving Time-dependent Evolution of Pore-Scale Structure, Permeability and Reactivity using X-ray Microtomography, Rev. Miner. Geochem., 80, 247–285, 2015.
Noiriel, C., Steefel, C. I., Yang, L., and Ajo-Franklin, J.: Upscaling calcium carbonate precipitation rates from pore to continuum scale, Chem. Geol., 318–319, 60–74, 2012.
Olasolo, P., Juárez, M., Morales, M., and Liarte, I.: Enhanced geothermal systems (EGS): A review, Renew. Sustain. Energ. Rev., 56, 133–144, 2016.
Ortoleva, P., Chadam, J., Merino, E., and Sen, A.: Geochemical self-organization II; the reactive-infiltration instability, Am. J. Sci., 287, 1008–1040, 1987.
Pacheco, F. A. L. and Alencoão, A. M. P.: Role of fractures in weathering of solid rocks: narrowing the gap between laboratory and field weathering rates, J. Hydrol., 316, 248–265, 2006.
Pacheco, F. A. L. and Van der Weijden, C. H.: Role of hydraulic diffusivity in the decrease of weathering rates over time, J. Hydrol., 512, 87–106, 2014.
Palmer, A. N.: Origin and morphology of limestone caves, Geol. Soc. Am. Bull., 103, 1–21, 1991.
Pandey, S., Chaudhuri, A., Rajaram, H., and Kelkar, S.: Fracture transmissivity evolution due to silica dissolution/precipitation during geothermal heat extraction, Geothermics, 57, 111–126, 2015.
Pandey, S., Vishal, V., and Chaudhuri, A.: Geothermal reservoir modeling in a coupled thermo-hydro-mechanical-chemical approach: a review, Earth-Sci. Rev., 185, 1157–1169, 2018.
Peng, C., Crawshaw, J. P., Maitland, G. C., and Trusler, J. P. M.: Kinetics of calcite dissolution in CO2-saturated water at temperatures between (323 and 373) K and pressures up to 13.8 MPa, Chem. Geol., 403, 74–85, 2015.
Phillips, O. M.: Geological fluid dynamics: sub-surface flow and reactions, Cambridge University Press, https://doi.org/10.1017/CBO9780511807473, 2009.
Plummer, L. N., Wigley, T. M. L., and Parkhurst, D. L.: The kinetics of calcite dissolution in CO2-water systems at 5 degrees to 60 degrees C and 0.0 to 1.0 atm CO2, Am. J. Sci., 278, 179–216, https://doi.org/10.2475/ajs.278.2.179, 1978.
Possemiers, M., Huysmans, M., and Batelaan, O.: Influence of Aquifer Thermal Energy Storage on groundwater quality: A review illustrated by seven case studies from Belgium, J. Hydrol.: Reg. Stud., 2, 20–34, 2014.
Press, W. H., Teukolsky, S. A., Vetterling, W. T., and Flannery, B. P.: Numerical recipes: The art of scientific computing, Cambridge University Press, ISBN 13 978-0-511-33555-6, 2007.
Rawal, C. and Ghassemi, A.: A reactive thermo-poroelastic analysis of water injection into an enhanced geothermal reservoir, Geothermics, 50, 10–23, 2014.
Regenauer-Lieb, K., Veveakis, M., Poulet, T., Wellmann, F., Karrech, A., Liu, J., Hauser, J., Schrank, C., Gaede, O., and Fusseis, F.: Multiscale coupling and multiphysics approaches in earth sciences: Applications, J. Coupl. Syst. Multisc. Dyn., 1, 281–323, 2013.
Rimstidt, J. D. and Barnes, H.: The kinetics of silica-water reactions, Geochim. Cosmochim. Ac., 44, 1683–1699, 1980.
Roded, R.: MATLAB codes and data compiled here, Zenodo [code] and [data set], https://doi.org/10.5281/zenodo.12531720, 2024.
Roded, R., Shalev, E., and Katoshevski, D.: Basal heat-flow and hydrothermal regime at the Golan-Ajloun hydrological basins, J. Hydrol., 476, 200–211, 2013.
Roded, R., Paredes, X., and Holtzman, R.: Reactive transport under stress: Permeability evolution in deformable porous media, Earth Planet. Sc. Lett., 493, 198–207, 2018.
Roded, R., Aharonov, E., Holtzman, R., and Szymczak, P.: Reactive flow and homogenization in anisotropic media, Water Resour. Res., 56, e2020WR027518, https://doi.org/10.1029/2020WR027518, 2020.
Roded, R., Szymczak, P., and Holtzman, R.: Wormholing in anisotropic media: Pore-scale effect on large-scale patterns, Geophys. Res. Lett., 48, e2021GL093659, https://doi.org/10.1029/2021GL093659, 2021.
Roded, R., Aharonov, E., Frumkin, A., Weber, N., Lazar, B., and Szymczak, P.: Cooling of hydrothermal fluids rich in carbon dioxide can create large karst cave systems in carbonate rocks, Commun. Earth Environ., 4, 465, https://doi.org/10.1038/s43247-023-01082-z, 2023.
Sabo, M. S. and Beckingham, L. E.: Porosity-Permeability Evolution During Simultaneous Mineral Dissolution and Precipitation, Water Resour. Res., 57, e2020WR029072, https://doi.org/10.1029/2020WR029072, 2021.
Sahimi, M.: Flow and transport in porous media and fractured rock: from classical methods to modern approaches, John Wiley & Sons, https://doi.org/10.1002/9783527636693, 2011.
Sanford, W. E. and Konikow, L. F.: Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers, Water Resour. Res., 25, 655–667, 1989.
Scholz, C. H.: The mechanics of earthquakes and faulting, Cambridge University Press, https://doi.org/10.1017/9781316681473, 2019.
Seigneur, N., Mayer, K. U., and Steefel, C. I.: Reactive transport in evolving porous media, Rev. Mineral. Geochem., 85, 197–238, 2019.
Shaw-Yang, Y. and Hund-Der, Y.: An analytical solution for modeling thermal energy transfer in a confined aquifer system, Hydrogeol. J., 16, 1507–1515, 2008.
Spiegelman, M., Kelemen, P. B., and Aharonov, E.: Causes and consequences of flow organization during melt transport: The reaction infiltration instability in compactible media, J. Geophys. Res.-Solid, 106, 2061–2077, 2001.
Stauffer, F., Bayer, P., Blum, P., Molina Giraldo, N., and Kinzelbach, W.: Thermal Use of Shallow Groundwater, 1st Edition, CRC Press, https://doi.org/10.1201/b16239, 2013.
Steefel, C. I., Molins, S., and Trebotich, D.: Pore scale processes associated with subsurface CO2 injection and sequestration, Rev. Miner. Geochem., 77, 259–303, 2013.
Steefel, C. I., Appelo, C. A. J., Arora, B., Jacques, D., Kalbacher, T., Kolditz, O., Lagneau, V., Lichtner, P. C., Mayer, K. U., and Meeussen, J. C. L.: Reactive transport codes for subsurface environmental simulation, Comput. Geosci., 19, 445–478, 2015.
Szymczak, P. and Ladd, A. J. C.: Reactive-infiltration instabilities in rocks. Fracture dissolution, J. Fluid Mech., 702, 239–264, 2012.
Taron, J. and Elsworth, D.: Thermal–hydrologic–mechanical–chemical processes in the evolution of engineered geothermal reservoirs, Int. J. Rock Mech. Min. Sci., 46, 855–864, 2009.
Tripp, G. I. and Vearncombe, J. R.: Fault/fracture density and mineralization: a contouring method for targeting in gold exploration, J. Struct. Geol., 26, 1087–1108, 2004.
Turcotte, D. L. and Schubert, G.: Geodynamics, Cambridge University Press, https://doi.org/10.1017/CBO9780511807442, 2002.
Tutolo, B. M., Kong, X.-Z., Seyfried Jr., W. E., and Saar, M. O.: High performance reactive transport simulations examining the effects of thermal, hydraulic, and chemical (THC) gradients on fluid injectivity at carbonate CCUS reservoir scales, Int. J. Greenh. Gas Con., 39, 285–301, https://doi.org/10.1016/j.ijggc.2015.05.026, 2015.
Vafaie, A., Cama, J., Soler, J. M., Kivi, I. R., and Vilarrasa, V.: Chemo-hydro-mechanical effects of CO2 injection on reservoir and seal rocks: A review on laboratory experiments, Renew. Sustain. Energ. Rev., 178, 113270, https://doi.org/10.1016/j.rser.2023.113270, 2023.
Voigt, H. and Haefner, F.: Heat transfer in aquifers with finite caprock thickness during a thermal injection process, Water Resour. Res., 23, 2286–2292, 1987.
White, M., Fu, P., McClure, M., Danko, G., Elsworth, D., Sonnenthal, E., Kelkar, S., and Podgorney, R.: A suite of benchmark and challenge problems for enhanced geothermal systems, Geomech. Geophys. Geo-Energ. Geo-Resour., 4, 79–117, 2018.
Wood, J. R. and Hewett, T. A.: Reservoir diagenesis and convective fluid flow, AAPG Memoir., 37, 99–110, https://doi.org/10.1306/M37435C6, 1984.
Woods, A. W.: Flow in porous rocks, Cambridge University Press, https://doi.org/10.1017/CBO9781107588677, 2015.
Xu, L., Szymczak, P., Toussaint, R., Flekkøy, E. G., and Måløy, K. J.: Dissolution Phase Diagram in Radial Geometry, Front. Phys., 8, 369, https://doi.org/10.3389/fphy.2020.00369, 2020.
Yang, S.-Y., Yeh, H.-D., and Li, K.-Y.: Modelling transient temperature distribution for injecting hot water through a well to an aquifer thermal energy storage system, Geophys. J. Int., 183, 237–251, 2010.
Yardley, B. W., Manning, C. E., and Garven, G.: Frontiers in geofluids, John Wiley & Sons, https://doi.org/10.1002/9781444394900, 2011.
Zheng, Y., Ross, A., Villholth, K. G., and Dillon, P.: Managing Aquifer Recharge. A Showcase for Resilience and Sustainability, UNESCO, Paris, ISBN 978-92-3-100488-9, 2021.
Zhou, Q., Oldenburg, C. M., and Rutqvist, J.: Revisiting the analytical solutions of heat transport in fractured reservoirs using a generalized multirate memory function, Water Resour. Res., 55, 1405–1428, 2019.
Zhu, C.: In situ feldspar dissolution rates in an aquifer, Geochim. Cosmochim. Ac., 69, 1435–1453, 2005.
Ziagos, J. P. and Blackwell, D. D.: A model for the transient temperature effects of horizontal fluid flow in geothermal systems, J. Volcanol. Geoth. Res., 27, 371–397, 1986.
Short summary
Common practices in water resource management and geothermal applications involve the injection of hot or cold water into aquifers. The resulting thermal changes may lead to chemical disequilibrium and consequent mineral dissolution/precipitation in the rock void space. A mathematical model is developed to study the effects of such thermal fluid injection on the evolution of water composition, aquifer porosity, and permeability. The model is then applied to two important case studies.
Common practices in water resource management and geothermal applications involve the injection...
