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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Hydrogeology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (560 pages)
    Edition: 1st ed.
    ISBN: 9781119166580
    Series Statement: Wiley Works
    Language: English
    Note: Cover -- Title Page -- Copyright -- Dedication -- Contents -- List of contributors -- About the companion websites -- Chapter 1 Introduction -- Motivation and background -- Nomenclature: porosity, permeability, hydraulic conductivity, and relative permeability -- Static versus dynamic permeability -- Contents of this book -- Data structures to integrate and extend existing knowledge -- Acknowledgments -- Chapter 2 DigitalCrust - a 4D data system of material properties for transforming research on crustal fluid flow -- Motivation -- Data integration to transform science -- The DigitalCrust vision -- An action plan -- Concluding remarks -- Acknowledgments -- Part I The physics of permeability -- Chapter 3 The physics of permeability -- Chapter 4 A pore-scale investigation of the dynamic response of saturated porous media to transient stresses -- Introduction -- Background -- Methods -- Results -- Discussion -- Conclusions -- Acknowledgments -- Chapter 5 Flow of concentrated suspensions through fractures: small variations in solid concentration cause significant in-plane velocity variations -- Introduction -- Overview of experiments -- Image analysis -- Experimental results -- Computational simulations -- Concluding remarks -- Acknowledgments -- Supporting information -- Chapter 6 Normal stress-induced permeability hysteresis of a fracture in a granite cylinder -- Introduction -- Theoretical aspects -- Experimental procedures -- Experimental procedures and results -- Concluding remarks -- Acknowledgements -- Chapter 7 Linking microearthquakes to fracture permeability evolution -- Introduction -- Channeling flows through heterogeneous fractures at laboratory scale -- Channeling flows through heterogeneous fractures beyond laboratory scale -- Conclusions -- Acknowledgments. , Chapter 8 Fractured rock stress-permeability relationships from in situ data and effects of temperature and chemical-mechanical couplings -- Introduction -- Fractured rock stress-permeability relation and sample size effect -- In situ block and ultra-large core experiments -- Borehole injection tests -- Model calibration against excavation-induced permeability changes -- Depth-dependent permeability of shallow bedrock -- Model calibration against the Yucca Mountain drift scale test -- Thermal and chemically mediated mechanical changes -- Application to geoengineering activities and potential implications for crustal permeability -- Concluding remarks -- Acknowledgments -- Part II Static permeability -- Chapter 9 Static permeability -- Sediments and sedimentary rocks -- Igneous and metamorphic rocks -- Part II (A): Sediments and sedimentary rocks -- Chapter 10 How well can we predict permeability in sedimentary basins? Deriving and evaluating porosity-permeability equations for noncemented sand and clay mixtures -- Introduction -- Data and methods -- Results -- Conclusions -- Acknowledgments -- Supporting information -- Chapter 11 Evolution of sediment permeability during burial and subduction -- Introduction -- Subduction zone sediments -- Methods -- Results and discussion -- Conclusions -- Acknowledgments -- Supporting information -- Part II (B): Igneous and metamorphic rocks -- Chapter 12 Is the permeability of crystalline rock in the shallow crust related to depth, lithology, or tectonic setting? -- Introduction -- Data sources, synthesis, and analysis -- Results and discussion -- Conclusions -- Data availability -- Acknowledgments -- Chapter 13 Understanding heat and groundwater flow through continental flood basalt provinces: insights gained from alternative models of permeability/depth relationships for the Columbia Plateau, United States. , Introduction -- Background -- Methods of analysis and results -- Results -- Discussion -- Conclusions -- Acknowledgments -- Chapter 14 Deep fluid circulation within crystalline basement rocks and the role of hydrologic windows in the formation of the Truth or Consequences, New Mexico low-temperature geothermal system -- Introduction -- Field measurements -- Thermal Peclet number analysis methods -- Geothermometry methods -- Hydrothermal modeling methods -- Results -- Discussion and conclusions -- Acknowledgments -- Chapter 15 Hydraulic conductivity of fractured upper crust: insights from hydraulic tests in boreholes and fluid-rock interaction in crystalline basement rocks -- Introduction -- Permeability - significance in fractured basement rocks -- Permeability and fluid flow in the crust -- Reactive fluid flow in the crust and its effect on permeability -- Fluid flow and permeability structure of the upper crust -- Summary and conclusions -- Acknowledgments -- Part III Dynamic permeability -- Chapter 16 Dynamic permeability -- Oceanic crust -- Fault zones -- Crustal-scale behavior -- Effects of fluid injection at the scale of a reservoir or ore deposit -- Part III (A): Oceanic crust -- Chapter 17 Rapid generation of reaction permeability in the roots of black smoker systems, Troodos ophiolite, Cyprus -- Introduction -- The Troodos ophiolite: Geological setting -- Epidosite zones: Previous work -- Results -- Discussion -- Conclusions -- Acknowledgements -- Part III (B): Fault zones -- Chapter 18 The permeability of active subduction plate boundary faults -- Introduction -- Fault zone architecture: inferences about hydraulic properties and behavior -- Observations of fluid flow, advective transport, and simple models -- Quantitative constraints on fault zone permeability from measurements and flow models -- Implications and key outstanding questions. , Acknowledgments -- Chapter 19 Changes in hot spring temperature and hydrogeology of the Alpine Fault hanging wall, New Zealand, induced by distal South Island earthquakes -- Introduction -- Setting and context -- Copland hot spring temperature observations -- Fluid chemistry of Copland hot spring -- Dynamic shaking -- Permanent deformation -- Discussion -- Summary and conclusions -- Acknowledgements -- Supporting information -- Chapter 20 Transient permeability in fault stepovers and rapid rates of orogenic gold deposit formation -- Introduction -- Association between stepovers and mineralisation -- Geometry and scaling properties of stepovers -- Numerical analysis of the relationship between stepover geometry and fault damage -- Discussion -- Conclusions -- Acknowledgements -- Supporting information -- Chapter 21 Evidence for long-timescale (> -- 10 3 years) changes in hydrothermal activity induced by seismic events -- Introduction -- Study area -- Methods -- Results -- Discussion and conclusions -- Acknowledgments -- Part III (C): Crustal-scale behavior -- Chapter 22 The permeability of crustal rocks through the metamorphic cycle: an overview -- Introduction -- Permeability and fluid flow in metamorphic rocks -- Permeability during devolatilization -- The contribution of metamorphism to the permeability structure of the crust -- Acknowledgements -- Chapter 23 An analytical solution for solitary porosity waves: dynamic permeability and fluidization of nonlinear viscous and viscoplastic rock -- Introduction -- Mathematical formulation -- Analytical solution for the 1D steady state -- Discussion -- Concluding remarks -- Acknowledgments -- Appendix: nondimensionalization. , Chapter 24 Hypocenter migration and crustal seismic velocity distribution observed for the inland earthquake swarms induced by the 2011 Tohoku-Oki earthquake in NE Japan: implications for crustal fluid distribution and crustal permeability -- Introduction -- Data and method -- Results -- Discussion -- Conclusions -- Acknowledgments -- Chapter 25 Continental-scale water-level response to a large earthquake -- Introduction -- The Wenchuan earthquake and the groundwater-level monitoring network -- Coseismic groundwater-level changes induced by the Wenchuan earthquake -- Mechanisms of the coseismic water-level change -- Discussion -- Conclusions -- Acknowledgments -- Supporting information -- Part III (D): Effects of fluid injection at the scale of a reservoir or ore-deposit -- Chapter 26 Development of connected permeability in massive crystalline rocks through hydraulic fracture propagation and shearing accompanying fluid injection -- Introduction -- Numerical approach -- Experiment and numerical analysis description -- Results -- Discussion on the development of connected permeability -- Conclusions -- Acknowledgments -- Chapter 27 Modeling enhanced geothermal systems and the essential nature of large-scale changes in permeability at the onset of slip -- Introduction -- The Basel fluid injection experiment -- The model -- Initial conditions -- Modeling results -- Discussion -- Conclusions -- Acknowledgments -- Chapter 28 Dynamics of permeability evolution in stimulated geothermal reservoirs -- Introduction -- Methodology -- Coupling strategy -- Results -- Conclusion -- Chapter 29 The dynamic interplay between saline fluid flow and rock permeability in magmatic-hydrothermal systems -- Introduction -- Porphyry copper and epithermal gold deposits -- Methods -- Results -- Discussion -- Conclusions -- Acknowledgments -- Part IV Conclusion. , Chapter 30 Toward systematic characterization.
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  • 2
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    PANGAEA
    In:  Supplement to: Luijendijk, Elco; Gleeson, Tom; Moosdorf, Nils (2019): The Flow of Fresh Groundwater and Solutes to the World's Oceans and Coastal Ecosystems. EarthArXiv Preprints, https://doi.org/10.31223/osf.io/sw8r4
    Publication Date: 2023-01-30
    Description: This dataset contains 1) results of a series of model runs that explore the sensitivity coastal groundwater discharge to hydrogeological parameters, 2) results of a large series of numerical models of coastal groundwater discharge that cover parameter space for topographic gradients, recharge and permeability of coastal groundwater systems and 3) the results of a global geospatial data analysis of relief, watershed geometry, recharge and permeability of coastal watersheds, and values for coastal groundwater discharge that are based on a combination of the model experiments and the geospatial data analysis. A description of the methods that were used to generate these datasets can be found in a preprint on eartharxiv, see linked publication below.
    Keywords: coastal hydrology; File format; File name; File size; groundwater; SGD; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 3
    Publication Date: 2021-05-04
    Description: The spatial distribution of subsurface parameters such as permeability are increasingly relevant for regional to global climate, land surface, and hydrologic models that are integrating groundwater dynamics and interactions. Despite the large fraction of unconsolidated sediments on Earth's surface with a wide range of permeability values, current global, high‐resolution permeability maps distinguish solely fine‐grained and coarse‐grained unconsolidated sediments. Representative permeability values are derived for a wide variety of unconsolidated sediments and applied to a new global map of unconsolidated sediments to produce the first geologically constrained, two‐layer global map of shallower and deeper permeability. The new mean logarithmic permeability of the Earth's surface is −12.7 ± 1.7 m2 being 1 order of magnitude higher than that derived from previous maps, which is consistent with the dominance of the coarser sediments. The new data set will benefit a variety of scientific applications including the next generation of climate, land surface, and hydrology models at regional to global scales.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2024-02-07
    Description: This planetary boundaries framework update finds that six of the nine boundaries are transgressed, suggesting that Earth is now well outside of the safe operating space for humanity. Ocean acidification is close to being breached, while aerosol loading regionally exceeds the boundary. Stratospheric ozone levels have slightly recovered. The transgression level has increased for all boundaries earlier identified as overstepped. As primary production drives Earth system biosphere functions, human appropriation of net primary production is proposed as a control variable for functional biosphere integrity. This boundary is also transgressed. Earth system modeling of different levels of the transgression of the climate and land system change boundaries illustrates that these anthropogenic impacts on Earth system must be considered in a systemic context.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
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