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Статті в журналах з теми "Microstructure des roches":
Fauchille, Anne-Laure, Bram van den Eijnden, Kevin Taylor, and Peter David Lee. "Détermination de la taille et du nombre d’échantillons devant être analysés en laboratoire pour la caractérisation statistique de la microstructure d’une roche argileuse." Revue Française de Géotechnique, no. 165 (2020): 1. http://dx.doi.org/10.1051/geotech/2020024.
Higgins, Michael Denis. "Igneous Rock Associations 17. Advances in the Textural Quantification of Crystalline Rocks." Geoscience Canada 42, no. 2 (April 10, 2015): 263. http://dx.doi.org/10.12789/geocanj.2015.42.069.
Goswami, Tapos Kumar. "Kink band microstructures in Mica in the Dafla Formation of the Siwalik Group of rocks, West Kameng District, Arunachal Pradesh." International Journal of Scientific Research 2, no. 12 (June 1, 2012): 260–61. http://dx.doi.org/10.15373/22778179/dec2013/75.
Trepmann, Claudia A., and John G. Spray. "Shock-induced crystal-plastic deformation and post-shock annealing of quartz: microstructural evidence from crystalline target rocks of the Charlevoix impact structure, Canada." European Journal of Mineralogy 18, no. 2 (May 11, 2006): 161–73. http://dx.doi.org/10.1127/0935-1221/2006/0018-0161.
Ciftci, Eda, Sevil Köse, Petek Korkusuz, Muharrem Timuçin, and Feza Korkusuz. "Boron Containing Nano Hydroxyapatites (B-n-HAp) Stimulate Mesenchymal Stem Cell Adhesion, Proliferation and Differentiation." Key Engineering Materials 631 (November 2014): 373–78. http://dx.doi.org/10.4028/www.scientific.net/kem.631.373.
M. Salleh, M. N., M. Ishak, M. H. Aiman, M. M. Quazi, and A. M. Hanafi. "Weld Geometry Investigation on Dissimilar Boron Steel Laser Welded for TWB Application." International Journal of Automotive and Mechanical Engineering 16, no. 4 (December 30, 2019): 7364–74. http://dx.doi.org/10.15282/ijame.16.4.2019.12.0546.
Farrow, M., J. Biglands, S. Tanner, E. Hensor, S. Mackie, P. Emery, and A. L. Tan. "THU0522 DIFFERENCES IN MUSCLE PROPERTIES IN GCA PATIENTS COMPARED TO HEALTHY CONTROLS AS ASSESSED BY QUANTITATIVE MRI." Annals of the Rheumatic Diseases 79, Suppl 1 (June 2020): 500.2–500. http://dx.doi.org/10.1136/annrheumdis-2020-eular.6025.
Kemenes, S., S. Bayat, D. Simon, G. Krönke, D. Bohr, L. Valor, F. Hartmann, et al. "AB0385 BARICITINIB LEADS TO RAPID AND PERSISTENT RESOLUTION OF SYNOVITIS AS MEASURED BY HAND MRI IN PATIENTS WITH ACTIVE RHEUMATOID ARTHRITIS (RA) FAILING cs/bDMARD THERAPY." Annals of the Rheumatic Diseases 81, Suppl 1 (May 23, 2022): 1320–21. http://dx.doi.org/10.1136/annrheumdis-2022-eular.476.
Leiderman, Ricardo, Andre M. B. Pereira, Francisco M. J. Benavides, Carla S. Silveira, Rodrigo M. R. Almeida, and Rodrigo A. Bagueira. "PERSONAL COMPUTER-BASED DIGITAL PETROPHYSICS." Revista Brasileira de Geofísica 35, no. 2 (June 21, 2017). http://dx.doi.org/10.22564/rbgf.v35i2.891.
Дисертації з теми "Microstructure des roches":
Léger, Marie. "Formation des réseaux karstiques : Rôle des hétérogénéités structurales, hydrodynamiques et minérales." Thesis, Université de Montpellier (2022-….), 2022. http://www.theses.fr/2022UMONG012.
Carbonate rocks constitute a very important part of the rocks at the Earth surface. Associated reservoirs represent essential resources for human societies, whether direct (water, gas, hydrocarbons) or indirect (geothermal energy, storage of CO2).The high reactivity of carbonate rocks is responsible for karstification, a reaction process due to the thermodynamic imbalance between the rock and the water circulating in the reservoir. This results in the formation of karstic aquifers, characterized by strong structural heterogeneities going with a complex hydrological behavior. This makes it a vulnerable system, but also a very productive one.In order to better manage these reservoirs and the water resource they contain, a better understanding of the formation and location of karst conduits is necessary.For this purpose, laboratory experiments can be performed to reproduce the karstification phenomenon at small scale. Rock samples from three types of carbonate rocks are extracted from homogeneous rock blocks in order to be dissolved. The rocks studied are a chalk, a crinoidal limestone and a dolomite, and the samples are considered to be REV.Before the experiments, the samples are characterized by laboratory and imaging methods, in order to know their structural, elastic, mechanical, mineral and hydrodynamic properties.They are then submitted to an injection of acidic fluid in an experimental device developed during the thesis. For chalk samples, two fluids with different acid concentrations are used, unlike crinoidal limestone and dolomite, where only one acid is used. Different flow rates, associated with different Péclet conditions, are applied to the samples. During the dissolutions, hydrodynamic and hydrochemical data are recorded continuously.After the experiments, the same measurements as before the experiments are performed.The characterization of the samples has shown that the microstructure controls the rock properties, and that the relationships established between the petrophysical properties at the sample scale are found at large scale reservoirs.For all rocks, the injection of acidic fluid into the samples causes rock dissolution, leading to the formation of preferential conduits, associated with an increase in permeability and porosity. Moreover, the observed dissolution regimes are directly correlated to the concentration of the injected acid and its flow rate, but also to the initial structural properties of the rock.For the experiments conducted on chalk, which is a very heterogeneous rock due to its high proportion of micropores, heterogeneities are responsible for the dissolution patterns observed, in particular the formation of channels while the experimental conditions suggest an uniform dissolution.For experiments involving all three rock types, the dolomite-containing rock shows a lower dissolution rate than the rocks without dolomite, which is due to the lower reaction kinetics of dolomite compared to calcite. With its high microporosity, chalk is the rock with the highest dissolution rate. Moreover, the conduits created in dolomite are much more localized and linear than the conduits in the other rocks. For the same amount of acid injected, the mineralogy of the rock, associated with its structure, is therefore mainly responsible for the dissolution figures in the rock
Fabre, Géraldine. "Fluage et endommagement des roches argileuses : évolution de la microstructure et modélisation phénoménologique." Phd thesis, Université Joseph Fourier (Grenoble), 2005. http://tel.archives-ouvertes.fr/tel-00009830.
Ammiar, Belkacem. "Microstructure et effet d'échelle dans les essais de micro-indentation sur les roches." Marne-la-vallée, ENPC, 2003. http://www.theses.fr/2003ENPC0004.
Léger, Marie. "Formation des réseaux karstiques : Rôle des hétérogénéités structurales, hydrodynamiques et minérales." Thesis, Montpellier, 2022. http://www.theses.fr/2022MONTG012.
Carbonate rocks constitute a very important part of the rocks at the Earth surface. Associated reservoirs represent essential resources for human societies, whether direct (water, gas, hydrocarbons) or indirect (geothermal energy, storage of CO2).The high reactivity of carbonate rocks is responsible for karstification, a reaction process due to the thermodynamic imbalance between the rock and the water circulating in the reservoir. This results in the formation of karstic aquifers, characterized by strong structural heterogeneities going with a complex hydrological behavior. This makes it a vulnerable system, but also a very productive one.In order to better manage these reservoirs and the water resource they contain, a better understanding of the formation and location of karst conduits is necessary.For this purpose, laboratory experiments can be performed to reproduce the karstification phenomenon at small scale. Rock samples from three types of carbonate rocks are extracted from homogeneous rock blocks in order to be dissolved. The rocks studied are a chalk, a crinoidal limestone and a dolomite, and the samples are considered to be REV.Before the experiments, the samples are characterized by laboratory and imaging methods, in order to know their structural, elastic, mechanical, mineral and hydrodynamic properties.They are then submitted to an injection of acidic fluid in an experimental device developed during the thesis. For chalk samples, two fluids with different acid concentrations are used, unlike crinoidal limestone and dolomite, where only one acid is used. Different flow rates, associated with different Péclet conditions, are applied to the samples. During the dissolutions, hydrodynamic and hydrochemical data are recorded continuously.After the experiments, the same measurements as before the experiments are performed.The characterization of the samples has shown that the microstructure controls the rock properties, and that the relationships established between the petrophysical properties at the sample scale are found at large scale reservoirs.For all rocks, the injection of acidic fluid into the samples causes rock dissolution, leading to the formation of preferential conduits, associated with an increase in permeability and porosity. Moreover, the observed dissolution regimes are directly correlated to the concentration of the injected acid and its flow rate, but also to the initial structural properties of the rock.For the experiments conducted on chalk, which is a very heterogeneous rock due to its high proportion of micropores, heterogeneities are responsible for the dissolution patterns observed, in particular the formation of channels while the experimental conditions suggest an uniform dissolution.For experiments involving all three rock types, the dolomite-containing rock shows a lower dissolution rate than the rocks without dolomite, which is due to the lower reaction kinetics of dolomite compared to calcite. With its high microporosity, chalk is the rock with the highest dissolution rate. Moreover, the conduits created in dolomite are much more localized and linear than the conduits in the other rocks. For the same amount of acid injected, the mineralogy of the rock, associated with its structure, is therefore mainly responsible for the dissolution figures in the rock
Zoussi, Sophia. "Mesures et modélisation de la microstructure et des propriétés de transport de roches sédimentaires." Université Louis Pasteur (Strasbourg) (1971-2008), 1995. http://www.theses.fr/1995STR10335.
Kalo, Kassem. "Caractérisation microstructurale et modélisation micromécanique de roches poreuses oolithiques." Thesis, Université de Lorraine, 2017. http://www.theses.fr/2017LORR0203/document.
The aim of this work is to study the influence of the microstructure of heterogeneous porous rocks on the behavior at the macroscopic scale. Thus, we characterized the microstructure and micromechanical properties (thanks to nano-indentation tests) of two porous oolitic rocks (Lavoux limestone and iron ore) to calculate their effective mechanical and thermal properties. Oolitic rocks are constituted by an assemblage of porous grains (oolites), pores and inter-granular crystals. Scanning electron microscopy and X-ray 3D Computed Tomography were used to identify the different components of these rocks. Particular attention was given to X-Ray computed tomography since this analytical method allows the characterization of the porous network (size, spatial distribution, and volume fraction), and the shapes of oolites and inter-oolitic crystals. The novelty of this work lies in taking into account the 3D real shape of pores. Hence, we approximated porous oolites by spheres and irregularly shaped pores by ellipsoids. This approximation was performed thanks to the principal component analysis (PCA), which provides the geometrical properties such as length of semi-axes and orientation of resulting ellipsoids. The sphericity of the approximated oolites was calculated and the values close to 1 allowed us to consider oolites as spheres. To verify the approximation in the case of pores, we evaluated the contribution of these irregularly shaped three-dimensional pores to the overall elastic properties. Thus, compliance contribution tensors for 3D irregular pores and their ellipsoidal approximations were calculated using the finite element method (FEM). These tensors were compared and a relative error was estimated to evaluate the accuracy of the approximation. This error produces a maximum discrepancy of 4.5% between the two solutions for pores and ellipsoids which verifies the proposed approximation procedure based on PCA. The FEM numerical method was verified by comparing the numerical solution for compliance contribution tensors of ellipsoids to the analytical solution based on Eshelby’s theory. The difference between these two solutions does not exceed 3%. The same numerical method was used to calculate thermal resistivity contribution tensors. Calculated compliance and resistivity contribution tensors were used to evaluate effective elastic properties (bulk modulus and shear coefficient) and effective thermal conductivity by considering the two-step Maxwell homogenization scheme. The results showed an important influence of the porosity on effective properties. Finally, the results obtained for irregular pores were compared to those for ellipsoidal ones and they showed a good agreement with a maximum deviation of 4% which verifies once again the approximation of irregularly shaped pores by tri-axial ellipsoids
Gasc-Barbier, Muriel. "Étude des mécanismes de déformation de roches argileuses profondes : apport de la microstructure et des analyses pétrophysiques." Paris 6, 2002. http://www.theses.fr/2002PA066151.
Saur, Hugo. "Étude des microstructures par tomographie à rayons X : application aux roches clastiques à grain fin." Electronic Thesis or Diss., Pau, 2022. http://www.theses.fr/2022PAUU3005.
The study of the microstructure of rocks is essential for our contemporary and future challenges in energy, engineering and construction. Furthermore, this study allows us to characterize the geological deformation processes that led to the current state of geological formations. Fine-grained clastic rocks, commonly called "shales", represent about two-thirds of all sedimentary rocks. 3D data concerning silt-sized grains or clasts embedded in the porous clay-rich matrix of this type of rock are relatively scarce despite the fact that these data are crucial to understand the anisotropic properties of these rocks at the macroscale but also to evaluate the deformation state of the rock matrix. A better understanding of the microstructure of these rocks would allow us to predict their mechanical or physical properties, which are essential for applications in the energy sector, among others. X-ray computed tomography (XCT) is a non-destructive technique providing a 3D image of the microstructure of any object. A direct geometric characterization of the constituents of fine-grained clastic rocks is possible with this technique. Based on XCT images, this thesis aims first to develop methodological aspects to study the 3D shape fabric of silt particles and their spatial distribution. The moments of inertia of segmented grains from 3D digital images are used for this development. We then present applications on fine-grained rocks with a sedimentary fabric and on deformed fine-grained rocks with a tectonic fabric. The first application part of the thesis focuses on the same lithologic unit having experienced different amounts of deformation. Samples from the South Pyrenean Basin and samples from a historical outcrop in the Central Appalachians were collected. We provide new data on the evolution of the 3D shape of grains and pores at the micrometer scale and their arrangement in the rock matrix with respect to the deformation intensity. The obtained data allow discussing the deformation mechanisms at the grain scale of the different mineralogical phases. However, the limited size of the imaged samples by means of XCT (≤ 2 mm diameter) raises the question of the representativeness of these analyses. On the South Pyrenean site, some samples are studied in more detail to evaluate the homogeneity of the results. We show that the XCT data complement the indirect petrophysical measurements by providing access to localized sub-fabrics that are integrated in a bulk measurement of the rock fabric. The limits are reached when the characteristic length of the deformation structures are on the order of the sample size imaged by XCT. In the second application part, samples from turbiditic systems of the South Pyrenean basin are analyzed. These systems, when deformed in compressive tectonic settings, record the same amount of shortening differently expressed in the various siliciclastic matrices. The results obtained from the shape data of the clasts are compared to our bulk magnetic fabric measurements and show a good consistency. The methodology presented in this work can be extended to other types of porous and granular media for a better understanding of the influence of fabric anisotropy on their macroscopic properties and mechanical behavior
Clavaud, Jean-Baptiste. "Etude des proprietes de transport (hydraulique et electrique) des roches : effets de la microstructure, de la presence de plusieurs fluides, de la fracturation et de l'interaction eau-roche." Paris 7, 2001. http://www.theses.fr/2001PA077016.
Xie, Shouyi Shao Jianfu. "Contribution à l'étude du comportement mécanique d'une roche poreuse." Villeneuve d'Ascq : Université des sciences et technologies de Lille, 2007. https://iris.univ-lille1.fr/dspace/handle/1908/189.
N° d'ordre (Lille 1) : 3647. Résumé en français et en anglais. Titre provenant de la page de titre du document numérisé. Bibliogr. p. 128-135.
Книги з теми "Microstructure des roches":
Vernon, R. H. A practical guide to rock microstructure. Cambridge, UK: Cambridge University Press, 2008.
Barker, A. J. Introduction to metamorphic textures and microstructures. Glasgow: Blackie, 1990.
Barker, A. J. Introduction to metamorphic textures and microstructures. 2nd ed. Cheltenham, UK: Stanley Thornes (Publishers), 1998.
Dresen, Georg, Mark Handy, and Christoph Janssen. Deformation Mechanisms Rheology Microstructures. Potsdam: [Neustadt an der Weinstrasse], 1999.
1939-, Bennett Richard Harold, Bryant William R, and Hulbert Mattthew H, eds. The Microstructure of fine-grained sediments, from mud to shale. New York: Springer-Verlag, 1991.
Trouw, R. A. J. Atlas of Mylonites - and related microstructures. Berlin, Heidelberg: Springer-Verlag Berlin Heidelberg, 2010.
Shelley, David. Igneous and metamorphic rocks under the microscope: Classification, textures, microstructures, and mineral preferred-orientations. London: Chapman & Hall, 1993.
1964-, Bons Paul Dirk, Koehn Daniel, and Jessell Mark W, eds. Microdynamics simulation. Berlin: Springer, 2008.
1964-, Bons Paul Dirk, Koehn Daniel, and Jessell Mark W, eds. Microdynamics simulation. Berlin: Springer, 2008.
1964-, Bons Paul Dirk, Koehn Daniel, and Jessell Mark W, eds. Microdynamics simulation. Berlin: Springer, 2008.
Частини книг з теми "Microstructure des roches":
Nagel, Thomas, Tuanny Cajuhi, Ralf-Michael Günther, Jobst Maßmann, Frank Wuttke, Keita Yoshioka, and Olaf Kolditz. "Introduction to GeomInt2." In SpringerBriefs in Earth System Sciences, 1–6. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-26493-1_1.
Barber, David J. "Régimes of plastic deformation — processes and microstructures: an overview." In Deformation Processes in Minerals, Ceramics and Rocks, 138–78. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-6827-4_7.
Ague, Daria M., Hans-Rudolf Wenk, and Eduard Wenk. "Deformation microstructures and lattice orientations of plagioclase in Gabbros from central Australia." In The Brittle‐Ductile Transition in Rocks, 173–86. Washington, D. C.: American Geophysical Union, 1990. http://dx.doi.org/10.1029/gm056p0173.
Tullis, Jan. "Experimental studies of deformation mechanisms and microstructures in quartzo-feldspathic rocks." In Deformation Processes in Minerals, Ceramics and Rocks, 190–227. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-6827-4_9.
Chester, F. M., and J. M. Logan. "Frictional faulting in polycrystalline halite: Correlation of microstructure, mechanisms of slip, and constitutive behavior." In The Brittle‐Ductile Transition in Rocks, 49–65. Washington, D. C.: American Geophysical Union, 1990. http://dx.doi.org/10.1029/gm056p0049.
Knipe, Robert J. "Microstructural analysis and tectonic evolution in thrust systems: examples from the Assynt region of the Moine Thrust Zone, Scotland." In Deformation Processes in Minerals, Ceramics and Rocks, 228–61. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-6827-4_10.
Miura, K., and K. Maeda. "Non-linear deformation behavior of granular materials by Elliptic Microstructure Model." In Deformation Characteristics of Geomaterials / Comportement Des Sols Et Des Roches Tendres. Taylor & Francis, 2003. http://dx.doi.org/10.1201/noe9058096043.ch148.
Tanaka, H., F. Rito, M. Tanaka, and N. Ohmukai. "Change in microstructure of Pleistocene clays due to one-dimensional consolidation." In Deformation Characteristics of Geomaterials / Comportement Des Sols Et Des Roches Tendres. Taylor & Francis, 2003. http://dx.doi.org/10.1201/noe9058096043.ch25.
Silvestroni, Laura, and Diletta Sciti. "Effect of Transition Metal Silicides on Microstructure and Mechanical Properties of Ultra-High Temperature Ceramics." In MAX Phases and Ultra-High Temperature Ceramics for Extreme Environments, 125–79. IGI Global, 2013. http://dx.doi.org/10.4018/978-1-4666-4066-5.ch005.
"83. Deformation Microstructure of Natural Plagioclase." In Fault-related Rocks, 276–77. Princeton University Press, 1998. http://dx.doi.org/10.1515/9781400864935.276.
Тези доповідей конференцій з теми "Microstructure des roches":
Meredith, Philip, and John Browning. "MICROSTRUCTURAL CONTROLS ON THERMAL CRACKING IN IGNEOUS ROCKS." In PRF2022—Progressive Failure of Brittle Rocks. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022pr-376046.
Koo, Joseph, Holly Stretz, Jon Weispfenning, Zhiping Luo, and W. Wootan. "Nanocomposite Rocket Ablative Materials: Processing, Microstructure, and Performance." In 45th AIAA/ASME/ASCE/AHS/ASC Structures, Structural Dynamics & Materials Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2004. http://dx.doi.org/10.2514/6.2004-1996.
Roberts, A. P., Dale P. Bentz, and Mark A. Knackstedt. "Correlating Microstructure to the Petrophysical Properties of Porous Rocks." In SPE Asia Pacific Oil and Gas Conference. Society of Petroleum Engineers, 1996. http://dx.doi.org/10.2118/37024-ms.
Saveliev, D. E., D. K. Makatov, and S. N. Sergeev. "MICROSTRUCTURAL FEATURES OF CHROMITITE AND ULTRAMAFIC ROCKS OF ALMAZ-ZHEMCHUZHINA DEPOSIT (KEMPIRSAY MASSIF, KAZAKHSTAN)." In Проблемы минералогии, петрографии и металлогении. Научные чтения памяти П. Н. Чирвинского. Perm State University, 2023. http://dx.doi.org/10.17072/chirvinsky.2023.230.
North, L. J., C. Couves, A. I. Best, and J. Sothcott. "Relationships Between Resistivity Anisotropy and Microstructure of Volcanic Reservoir Rocks." In 76th EAGE Conference and Exhibition 2014. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20141353.
Prasad”, Manika, and Murli H. Manghnani. "Velocity and impedance microstructural anisotropy in reservoir rocks." In SEG Technical Program Expanded Abstracts 1996. Society of Exploration Geophysicists, 1996. http://dx.doi.org/10.1190/1.1826500.
Xu, Tao, Shengqi Yang, Mike Heap, Chongfeng Chen, and Tianhong Yang. "Microstructural Damage-Induced Localized Fracturing of Brittle Rocks." In Fourth Geo-China International Conference. Reston, VA: American Society of Civil Engineers, 2016. http://dx.doi.org/10.1061/9780784480007.007.
Siciliano, Fulvio, Douglas G. Stalheim, and J. Malcolm Gray. "Modern High Strength Steels for Oil and Gas Transmission Pipelines." In 2008 7th International Pipeline Conference. ASMEDC, 2008. http://dx.doi.org/10.1115/ipc2008-64292.
Pineda, J. A., E. Romero, D. Tarragò, E. Tauler, and E. E. Alonso. "Microstructural Evaluation of the Water Sensitivity of Clayey Rocks." In Fifth Biot Conference on Poromechanics. Reston, VA: American Society of Civil Engineers, 2013. http://dx.doi.org/10.1061/9780784412992.173.
Kayser, A., S. Warner, and R. Gras. "Using Virtual Reality to Visualize the Internal Microstructure of Rocks in 3D." In 66th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.3.d023.
Звіти організацій з теми "Microstructure des roches":
Schlueter, E. M. Predicting the permeability of sedimentary rocks from microstructure. Office of Scientific and Technical Information (OSTI), January 1995. http://dx.doi.org/10.2172/70737.
Schlueter, Erika M. Predicting the transport properties of sedimentary rocks from microstructure. Office of Scientific and Technical Information (OSTI), January 1995. http://dx.doi.org/10.2172/79095.
Le Pape, Yann, and Mohammed Alnaggar. Microstructural Simulation of Ion-Irradiated Natural Rocks and Minerals. Office of Scientific and Technical Information (OSTI), March 2023. http://dx.doi.org/10.2172/1994706.
Zhang, Yida, Pania Newell, Yunping Xi, Andrea Tyrrell, Mitul Sisodiya, Xiang Zhou, Yao Wang, Yanbo Wang, and Bozo Vazic. Time-dependent THMC properties and microstructural evolution of damaged rocks in excavation damage zone. Office of Scientific and Technical Information (OSTI), November 2022. http://dx.doi.org/10.2172/1897054.