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  • ddc:550.724  (39)
  • 2020-2024  (39)
  • 1940-1944
  • 1
    Publication Date: 2024-03-12
    Description: Three‐dimensional (3d) numerical models are state‐of‐the‐art for investigating complex hydrodynamic flow patterns in reservoirs and lakes. Such full‐complexity models are computationally demanding and their calibration is challenging regarding time, subjective decision‐making, and measurement data availability. In addition, physically unrealistic model assumptions or combinations of calibration parameters may remain undetected and lead to overfitting. In this study, we investigate if and how so‐called Bayesian calibration aids in characterizing faulty model setups driven by measurement data and calibration parameter combinations. Bayesian calibration builds on recent developments in machine learning and uses a Gaussian process emulator as a surrogate model, which runs considerably faster than a 3d numerical model. We Bayesian‐calibrate a Delft3D‐FLOW model of a pump‐storage reservoir as a function of the background horizontal eddy viscosity and diffusivity, and initial water temperature profile. We consider three scenarios with varying degrees of faulty assumptions and different uses of flow velocity and water temperature measurements. One of the scenarios forces completely unrealistic, rapid lake stratification and still yields similarly good calibration accuracy as more correct scenarios regarding global statistics, such as the root‐mean‐square error. An uncertainty assessment resulting from the Bayesian calibration indicates that the completely unrealistic scenario forces fast lake stratification through highly uncertain mixing‐related model parameters. Thus, Bayesian calibration describes the quality of calibration and correctness of model assumptions through geometric characteristics of posterior distributions. For instance, most likely calibration parameter values (posterior distribution maxima) at the calibration range limit or with widespread uncertainty characterize poor model assumptions and calibration.
    Description: Plain Language Summary: Software tools for replicating a real‐world element, such as an artificial lake, need to account for many unknown parameters to create a physically sound conceptual computer model. Still, simplification assumptions are necessary to break down the complex reality into parameters that are easier to calculate. But the simplified parameters take on different values for each model and require specific adjustments. To perform these adjustments, a past event is typically reproduced with the conceptual model and different simplification parameter combinations. The simplification parameter combinations leading to the best possible replication of the past event are assumed to be valid to use the conceptual model for predictions of future events. Alas, many potentially false combinations can replicate a past event with very good results. Thus, a conceptual computer model can be overly adjusted regarding a particular phenomenon, such as heat transfer. Also, the number of possible adjustment tests is limited due to the long computing time of a conceptual model. For these reasons, we use a fast, simplified statistical model of a more complex conceptual model and machine learning for the adjustment process. We find that the statistic uncertainty increases with decreasing physical correctness of simplification parameter combinations.
    Description: Key Points: Bayesian calibration efficiently and objectively fits constrained, case‐specific model parameters and identifies remaining uncertainties. Post‐calibration uncertainty assessments help identify incorrect parameter combinations and constraints. More constrained calibration leads to lower uncertainty, which is not detected by global statistics.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Ministerium für Wissenschaft, Forschung und Kunst Baden‐Württemberg http://dx.doi.org/10.13039/501100003542
    Description: https://github.com/sergiocallau/ManuscriptSBT/releases/tag/v0.1
    Description: https://github.com/sschwindt/schwarzenbach-bc/archive/refs/tags/boundary-data.zip
    Keywords: ddc:550.724 ; Gaussian process regression ; Bayesian optimization ; supervised machine learning ; Delft3D ; surrogate ; meta model
    Language: English
    Type: doc-type:article
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  • 2
    Publication Date: 2024-02-23
    Description: Pharmaceutically active compounds (PhACs) released into the environment have an adverse impact on the soil and water ecosystem as well as human health. Sorption of PhACs by soils and its potential modification through introduced DOM in the applied animal manure or treated wastewater (TWW) determines the mobility and environmental relevance of PhACs. Sulfadiazine, caffeine and atenolol were selected as target PhACs to investigate their sorption behaviors by five selected arable soils in the absence and presence of pig manure DOM. Sulfadiazine was least sorbed, followed by caffeine and atenolol according to the Freundlich sorption isotherm fit (soil average Kf [μg〈sup〉(1−n)〈/sup〉 mL〈sup〉n〈/sup〉 g〈sup〉−1〈/sup〉] 4.07, 9.06, 18.92, respectively). The addition of manure DOM (31.34 mg C L〈sup〉−1〈/sup〉) decreased the sorption of sulfadiazine and especially of caffeine and atenolol (average K〈sub〉f〈/sub〉 3.04, 6.17, 5.79, respectively). Freundlich sorption isotherms of the PhACs became more nonlinear in the presence of manure DOM (Freundlich exponent n changed from 0.74–1.40 to 0.62–1.12), implying more heterogeneous sorption of PhACs in soil–DOM binary systems. Sorption competition of DOM molecules with sulfadiazine and caffeine mostly contributed to their decreased soil sorption when DOM was present. In contrast, the formation of DOM–atenolol associates in the solution phase caused the largely decreased soil sorption of atenolol in the presence of DOM. It is suggested that DOM concentration (e.g., ≥ 60 mg C L〈sup〉−1〈/sup〉) and its interaction with PhACs should be taken into consideration when assessing the environmental impact of land application of animal manure or irrigation with TWW.
    Description: China Scholarship Council http://dx.doi.org/10.13039/501100004543
    Description: CAS, Inst. of Mountain Hazard, Strategic program
    Description: Universität Trier (3163)
    Keywords: ddc:550.724 ; DOM associate ; Sorption competition ; Sorption nonlinearity ; Sorption strength ; Spectroscopy ; Treated wastewater
    Language: English
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  • 3
    Publication Date: 2024-02-21
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Linear kinematic features (LKFs) are found everywhere in the Arctic sea‐ice cover. They are strongly localized deformations often associated with the formation of leads and pressure ridges. In viscous‐plastic (VP) sea‐ice models, the simulation of LKFs depends on several factors such as the grid resolution, the numerical solver convergence, and the placement of the variables on the mesh. In this study, we compare two recently proposed discretization with a CD‐grid placement with respect to their ability to reproduce LKFs. The first (CD1) is based on a nonconforming finite element discretization, whereas the second (CD2) uses a conforming subgrid discretization. To analyze their resolution properties, we evaluate runs from different models (e.g., FESOM, MPAS) on a benchmark problem using quadrilateral, hexagonal and triangular meshes. Our findings show that the CD1 setup simulates more deformation structure than the CD2 setup. This highlights the importance of the type of spatial discretization for the simulation of LKFs. Due to the higher number of degrees of freedom, both CD‐grids resolve more LKFs than traditional A, B, and C‐grids at fixed mesh level. This is an advantage of the CD‐grid approach, as high spatial mesh resolution is needed in VP sea‐ice models to simulate LKFs.〈/p〉
    Description: Plain Language Summary: Sea ice in the polar regions is an important component of the climate system. Satellite images demonstrate that the sea‐ice cover can contain long features, such as cracks or leads and areas of increased sea‐ice density known as pressure ridges. In order to simulate these features, mathematical equations that describe the drift of ice are solved on a computational grid. A recent study showed that the simulation of these features on a grid with a given spacing is influenced by the way the variables are placed on grid cells. Locating them at the edge midpoints of the cells leads to simulations with more features than placing the variables on vertices or centers of cells. In this contribution, we show that, along with the placement, also the mathematical method used to approximate the equations on the computational grid plays a pivotal role on the number of simulated features.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉The type of spatial discretization used in CD‐grid approximations is important for the amount of simulated local kinematic features (LKFs)〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The CD‐grid discretization based on nonconforming finite elements simulates the highest amount of LKFs〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The CD‐grids resolve more LKFs than A‐grids, B‐grids, or C‐grids〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: German Research Foundation
    Description: https://doi.org/10.5281/zenodo.7662610
    Description: https://doi.org/10.5281/zenodo.7646908
    Description: https://data.mendeley.com/datasets/7h9hkjvx48/1
    Keywords: ddc:550.724 ; sea‐ice dynamics ; CD‐grids ; linear kinematic features ; nonconforming finite elements
    Language: English
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  • 4
    Publication Date: 2024-02-09
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Fluid flow in fracture porosity in the Earth's crust is in general accompanied by crystallization or dissolution depending on the state of saturation. The evolution of the microstructure in turn affects the transport and mechanical properties of the rock, but the understanding of this coupled system is incomplete. Here, we aim to simulate spatio‐temporal observations of laboratory experiments at the grain scale (using potash alumn), where crystals grow in a fracture during reactive flow, and show a varying growth rate along the fracture due to saturation differences. We use a multiphase‐field modeling approach, where reactive fluid flow and crystal growth is computed and couple the chemical driving force for grain growth to the local saturation state of the fluid. The supersaturation of the fluid is characterized by a concentration field which is advected by fluid flow and in turn affects the crystal growth with anisotropic growth kinetics. The simulations exhibit good agreement with the experimental results, providing the basis for upscaling our results to larger scale computations of combined multi‐physical processes in fractured porous media for applications as groundwater protection, geothermal, and hydrocarbon reservoir prediction, water recovery, or storing H〈sub〉2〈/sub〉 or CO〈sub〉2〈/sub〉 in the subsurface.〈/p〉
    Description: Plain Language Summary: In the Earth's crust fluid flow can occur in fractured rock and depending on the composition of the fluid and physical conditions minerals can precipitate or dissolve. This affects the properties of the rock system and is for example, of interest to subsurface engineering applications. In this work we simulate observations of laboratory experiments at the grain scale, where crystals grow in an open fracture during fluid flow. In these experiments, the growth rate of the crystals varies along the fracture since the supersaturation of the fluid decreases due to the crystallization. We use a multiphase‐field model for the numerical simulation of crystal growth in the open fracture and combine it with reactive fluid flow. With the presented model the driving force for grain growth is coupled to the local supersaturation, which enables the incorporation of reactive mass transport in open fractures. Our phase‐field simulations agree with the laboratory experiments. The presented simulative approach can be used for upscaling the results on microscale to larger length and time scales and can help to better predict the subsurface behavior for example, of groundwater, fractured geothermal, and hydrocarbon reservoirs.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Reactive fluid flow with advective mass transfer causes locally variable precipitation rate in open fracture〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉A higher flow velocity or a higher supersaturation results in faster precipitation along the flow channel〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Phase‐field modeling allows reproduction of laboratory crystal growth experiments from an advecting fluid using transmitted light microscopy〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100009318
    Description: https://doi.org/10.5281/zenodo.7516287
    Description: http://www.steinbeis.de/
    Keywords: ddc:550.724 ; phase‐field modeling ; fluid flow ; supersaturation ; crystal growth ; flow channel
    Language: English
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  • 5
    Publication Date: 2024-02-06
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉We have performed in situ time‐of‐flight neutron diffraction experiments to examine the uptake of deuterium in iron monosulfide at pressures up to 11.4 GPa and temperatures to 1300 K. A D〈sub〉2〈/sub〉 fluid was formed in the experiments through the decomposition of ND〈sub〉3〈/sub〉BD〈sub〉3〈/sub〉, resulting in an oxygen fugacity of approximately 1.2 log units below the iron‐wüstite buffer. Deuterium positions and site occupancies were determined in FeS V, using Rietveld refinements of the powder neutron diffraction patterns. Our structural model indicates that two normally unoccupied sites in the 〈italic〉P〈/italic〉6〈sub〉3〈/sub〉/〈italic〉mmc〈/italic〉 FeS V structure, at Wyckoff positions 〈italic〉6h〈/italic〉 and 〈italic〉4f〈/italic〉, are partially occupied by D atoms, with the latter being more dominant. The deuterium content D〈sub〉x〈/sub〉 in FeSD〈sub〉X〈/sub〉 increases with both pressure and temperature over the experimental conditions explored, from 0.126 (14) at 2.3 GPa and 787 K to 1.20 (16) at 9.7 GPa and 1300 K. The unit‐cell volume expansion per deuterium atom is 1.53 ± 0.16 Å〈sup〉3〈/sup〉 at 6.9 GPa and 960 K, which is smaller than that determined for metallic iron phases at similar conditions. The variation in unit‐cell volume indicates that most deuterium is lost from FeS V upon temperature quenching at high‐pressures. By fitting the obtained FeS V deuterium site occupancies to a thermodynamic model, estimates for the hydrogen contents of iron monosulfide at conditions and oxygen fugacities consistent with the base of the cratonic lithosphere can be made. This results in values in the range of 1,700–2,700 ppm, which contribute to approximately 2–3 ppm hydrogen in the bulk mantle.〈/p〉
    Description: Plain Language Summary: Small amounts of iron sulfide minerals are found in most rocks from the Earth's mantle and as inclusions trapped in natural diamonds. Hydrogen may dissolve into iron sulfide minerals under high pressures and temperature, but is most likely lost once pressure and temperature are removed. In this study, we determined deuterium contents (deuterium was used as a proxy for hydrogen as it has better neutron scattering properties) in iron sulfide, held under high pressure and temperature conditions, using neutron diffraction measurements. Our results show that the amount of deuterium in iron sulfide increases with both pressure and temperature, but the deuterium is lost on recovery to room conditions. The results are used to estimate hydrogen contents of iron sulfide minerals in the deep continental lithospheric mantle, which are found to be in the range 1,700–2,700 ppm. This corresponds to approximately 2–3 ppm of hydrogen in the bulk mantle.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Deuterium contents in iron sulfide were measured at high‐〈italic〉P〈/italic〉, up to 11.4 GPa and high‐〈italic〉T〈/italic〉 to 1300 K in in situ neutron diffraction experiments〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The total deuterium content, D〈sub〉x〈/sub〉 in FeSD〈sub〉X〈/sub〉, increases with both 〈italic〉P〈/italic〉 and 〈italic〉T〈/italic〉, from 0.126 (14) at 2.3 GPa and 787 K to 1.20 (16) at 9.7 GPa and 1300 K〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉A thermodynamic model shows that the hydrogen contents of iron monosulfide at the base of the cratonic lithosphere could be 1,700–2,700 ppm〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.6084/m9.figshare.21820677.v2
    Keywords: ddc:550.724 ; iron monosulfide ; neutron diffraction ; deuterium ; Earth's mantle
    Language: English
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  • 6
    Publication Date: 2024-02-05
    Description: We present an experimental study simulating atmospheric dust devils in a controlled laboratory experiment. The experimental facility, called the “Barrel of Ilmenau” (www.ilmenauer-fass.de) represents a classical Rayleigh‐Bénard set‐up and is believed to model the phenomena in a convective atmospheric boundary layer fairly well. Our work complements and extends the numerical work of Giersch and Raasch (2021)https//doi.org/10.1029/2020jd034334 by experiments. Dust devils are thermal convective vortices with a vertical axis of rotation visualized by entrained soil particles. They evolve in the convective atmospheric boundary layer and are believed to substantially contribute to the aerosol transport into the atmosphere. Thus, their evolution, size, lifetime, and frequency of occurrence are of particular research interest. Extensive experimental studies have been conducted by field measurements and laboratory experiments so far. Beyond that, our study is the first attempt of Rayleigh‐Bénard convection (RBC) in air to investigate dust devil‐like vortices in a laboratory experiment. Up to now, this set‐up mimics the natural process of dust devil evolution as closest to reality. The flow measurement was carried out by particle tracking velocimetry using neutrally buoyant soap bubbles. We initially identified dust devil‐like vortices by eye from the Lagrangian velocity field, and in a later, more sophisticated analysis by a specific algorithm from the corresponding Eulerian velocity field. We analyzed their frequency of occurrence, observation time, and size. With our work, we could demonstrate that turbulent RBC is an appropriate model to mimic the natural process of the evolution of dust devils in the convective atmospheric boundary layer without artificial stimulation.
    Description: Plain Language Summary: We could experimentally demonstrate that dust devil‐like vortices spontaneously arise in turbulent Rayleigh‐Bénard convection. This first‐time experimental survey simulates the evolution of dust devil‐like vortices in a laboratory experiment which mimics the convective atmospheric boundary layer quite closely and gets by without any artificial input of rotation. Dust devil‐like vortices are measured and identified using the particle tracking velocimetry technique. Within an observation period of 2 hr, 56 dust devil‐like vortices could be detected in total. Their properties coincide quite well with those structures identified in very recent direct numerical simulations (DNS) by Giersch and Raasch (2021, https//doi.org/10.1029/2020jd034334). As well, they show similarity to atmospheric dust devils. The size of our experimentally generated dust devil‐like vortices starts at about 1 dm and ranges up to about 1 m. This is larger than in DNS, but still smaller than in the atmosphere or in large eddy simulation.
    Description: Key Points: Dust devil‐like vortices spontaneously evolve in turbulent Rayleigh‐Bénard convection at sufficiently high Rayleigh numbers Ra 〉 1010. We studied their properties in a large‐scale Rayleigh‐Bénard experiment using Lagrangian particle tracking velocimetry. The vortical structures in the laboratory experiment are weaker than atmospheric dust devils, but they exhibit similar features.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://ftp.tu-ilmenau.de/hpc-private/mb/Dust_Devil_Scripts.rar
    Description: https://ftp.tu-ilmenau.de/hpc-private/mb/Kaestner_et_al_2022_dust_devil-like_vortex_in_turbulent_Rayleigh_Benard_convection.avi
    Keywords: ddc:550.724 ; dust devils ; particle tracking velocimetry ; Rayleigh‐Bénard convection ; turbulence ; atmospheric boundary layer
    Language: English
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  • 7
    Publication Date: 2024-02-05
    Description: 〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Penetrating, high‐energy synchrotron X‐rays are in strong demand, particularly for high‐pressure research in physics, chemistry and geosciences, and for materials engineering research under less extreme conditions. A new high‐energy wiggler beamline P61 has been constructed to meet this need at PETRA III in Hamburg, Germany. The first part of the paper offers an overview of the beamline front‐end components and beam characteristics. The second part describes the performance of the instrumentation and the latest developments at the P61B endstation. Particular attention is given to the unprecedented high‐energy photon flux delivered by the ten wigglers of the PETRA III storage ring and the challenges faced in harnessing this amount of flux and heat load in the beam. Furthermore, the distinctiveness of the world's first six‐ram Hall‐type large‐volume press, Aster‐15, at a synchrotron facility is described for research with synchrotron X‐rays. Additionally, detection schemes, experimental strategies and preliminary data acquired using energy‐dispersive X‐ray diffraction and radiography techniques are presented.〈/p〉
    Description: 〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉The operation of the P61B endstation large‐volume press and optics of P61 are reviewed. The instrumentation at P61B, including the large‐volume press, detection systems and data acquisition for 〈italic〉in situ〈/italic〉 high‐pressure experiments are described.〈boxed-text position="anchor" content-type="graphic" xml:lang="en"〉〈graphic position="anchor" id="jats-graphic-1" xlink:href="urn:x-wiley:16005775:jsy2ju5040:jsy2ju5040-fig-0001"〉 〈/graphic〉〈/boxed-text〉〈/p〉
    Keywords: ddc:550.724 ; extreme conditions ; high‐pressure ; large‐volume press ; energy‐dispersive X‐ray diffraction ; radiography ; resistive heating ; ultrasonic interferometry ; acoustic emissions detection
    Language: English
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  • 8
    Publication Date: 2024-01-26
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Riverbed clogging is key to assessing vertical connectivity in the hyporheic zone and is often quantified using single‐parameter or qualitative approaches. However, clogging is driven by multiple, interacting physical and bio‐geochemical parameters, which do not allow for a conclusive assessment of hyporheic connectivity with single‐parameter approaches. In addition, existing qualitative assessments lack transparency and repeatability. This study introduces a Multi‐Parameter Approach to quantify Clogging and vertical hyporheic connectivity (MultiPAC), which builds on standardized measurements of physical (grain size characteristics, porosity, hydraulic conductivity) and bio‐geochemical (interstitial dissolved oxygen) parameters. We apply MultiPAC at three gravel‐bed rivers and show how the set of parameters provides a representative appreciation of physical riverbed clogging, thus quantifying vertical hyporheic connectivity. However, more parameters are required to fully characterize biological clogging. In addition, MultiPAC locates clogged layers in the hyporheic zone through multi‐parameter vertical profiles over the riverbed depth. The discussion outlines the relevance of MultiPAC to guide field surveys.〈/p〉
    Description: https://github.com/Ecohydraulics/kf-converter-w-flopy
    Keywords: ddc:550.724 ; colmation ; dissolved oxygen ; grain size ; hydraulic conductivity ; porosity ; siltation
    Language: English
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  • 9
    Publication Date: 2024-01-22
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉The emergence, geometry and activation of faults are intrinsically linked to frictional rheology. The latter is thus a central element in geodynamic simulations which aim at modeling the generation and evolution of fault zones and plate boundaries. However, resolving frictional strain localization in geodynamic models is problematic. In simulations, equilibrium cannot always be attained and results can depend on mesh resolution. Spatial and temporal regularization techniques have been developed to alleviate these issues. Herein, we investigate three popular regularization techniques, namely viscoplasticity, gradient plasticity and the use of a Cosserat continuum. These techniques have been implemented in a single framework based on an accelerated pseudo‐transient solution strategy. The latter allows to explore the effects of regularization on shear banding using the same code and model configuration. We have used model configurations that involve three levels of complexity: from the emergence of a single isolated shear band to the visco‐elasto‐plastic stress buildup of a crust. All considered approaches allow to resolve shear banding, provide convergence upon mesh refinement and satisfaction of equilibrium. Viscoplastic regularization is straightforward to implement in geodynamic codes. Nevertheless, more stable shear banding patterns and strength estimates are achieved with computationally more expensive gradient and Cosserat‐type regularizations. We discuss the relative benefits of these techniques and their combinations for geodynamic modeling. Emphasis is put on the potential of Cosserat‐type media for geodynamic applications.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Regularization approaches for plastic strain localization are tested using a single code based on pseudo‐transient method〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉All considered schemes provide convergent result upon mesh refinement and satisfaction of equilibrium〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The use of Cosserat continuum is most robust regularization approach and is also is the most demanding〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: https://doi.org/10.5281/zenodo.7971379
    Description: https://doi.org/10.5281/zenodo.7692569
    Description: https://github.com/PTsolvers/PlasticityRegularisations_G3
    Keywords: ddc:550.724 ; strain localization ; frictional plasticity ; regularization ; viscoplasticity ; gradient plasticity ; Cosserat continuum
    Language: English
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  • 10
    Publication Date: 2024-01-15
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Transient creep of crustal rocks is important to explain time‐dependent geological processes such as postseismic deformation following a large continental earthquake. While the steady‐state creep flow law parameters of quartz and feldspar, major minerals in the upper and lower crust, are well known, the physical mechanism behind transient creep and the corresponding flow law parameters are poorly understood. We quantify the flow law parameters for both quartz and granulite (mixture of plagioclase and pyroxene) under wet conditions with a nonlinear Burgers model using a Markov chain Monte Carlo (MCMC) method. Modeling results yield an activation energy of 70 ± 20 kJ/mol and a stress exponent of 2.0 ± 0.1 for transient creep of quartz aggregates. For granulite/feldspar, we find activation energies of 280 ± 30 and 220 ± 20 kJ/mol and stress exponents of 1.0 ± 0.2 and 0.9 ± 0.1 under mid (1050–1100°C) and high (1125–1150°C), temperature conditions, respectively. The stress exponents and activation energies of transient creep are consistently smaller than those of steady‐state creep for both quartz and granulite/feldspar. Combined with results for transient creep of olivine that were previously obtained (Masuti & Barbot, 2021, 〈ext-link ext-link-type="uri" xlink:href="https://doi.org/10.1186/s40623-021-01543-9"〉https://doi.org/10.1186/s40623-021-01543-9〈/ext-link〉), we suggest that the activation energies and stress exponents of transient creep are smaller than those of steady‐state creep for volumetrically important silicate minerals of the crust and upper mantle. Extrapolation of the estimated flow law parameters of granulite/feldspar to natural conditions suggests that transient creep may dominate during the postseismic period and lasts longer than previously thought.〈/p〉
    Description: Plain Language Summary: Earthquakes induce intermittent deformation of the solid Earth at rates that are higher or lower than the interseismic strain rates. When an earthquake occurs, it is accompanied by a sudden slip on the fault and a rapid stress change in the lower crust leading to an evolving rock strength. Lower crustal rocks represent a complex assembly of minerals and several different micro‐mechanisms may be activated during deformation. We use experimental data for quartz and feldspar to constrain the mechanical properties of the transient creep (i.e., stress changes with strain under constant strain rate conditions or strain changes nonlinearly with time under constant stress conditions). Based on our results, we conclude that the transient creep following an earthquake may not be as short lived as previously has been thought.〈/p〉
    Description: Key Points: 〈list-item〉 〈p xml:lang="en"〉Transient creep flow law parameters of quartz and granulite are determined using a Markov chain Monte Carlo method〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Low stress exponent of the transient creep in silicates could be due to weak dependency of dislocation density on the stress〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Transient creep could be dominant during the postseismic phase of the earthquake cycle〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: Japan Society for the Promotion of Science http://dx.doi.org/10.13039/501100001691
    Description: Humboldt Research Fellowship for Postdoctoral Researchers
    Description: Alexander von Humboldt‐Stiftung http://dx.doi.org/10.13039/100005156
    Description: https://doi.org/10.5281/zenodo.8304793
    Description: https://doi.org/10.5281/zenodo.8304760
    Keywords: ddc:550.724 ; transient creep ; quartz ; feldspar ; rheology ; lower crust ; granulite
    Language: English
    Type: doc-type:article
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