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Journal articles on the topic 'Earth internal structure'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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1

Wood, Bernard, and George Helffrich. "Internal structure of the Earth." Nature 344, no. 6262 (1990): 106. http://dx.doi.org/10.1038/344106a0.

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2

Binzel, Richard P., and Wlodek Kofman. "Internal structure of Near-Earth Objects." Comptes Rendus Physique 6, no. 3 (2005): 321–26. http://dx.doi.org/10.1016/j.crhy.2005.01.001.

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3

NAKANISHI, Ichiro. "Recent Seismological Studies on Internal Structure of the Earth." Zisin (Journal of the Seismological Society of Japan. 2nd ser.) 41, no. 1 (1988): 133–44. http://dx.doi.org/10.4294/zisin1948.41.1_133.

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4

Liu, Shu Zhi. "Internal Force Analysis of Frame Structure Considering the Soil Constraint." Applied Mechanics and Materials 777 (July 2015): 38–41. http://dx.doi.org/10.4028/www.scientific.net/amm.777.38.

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Part of the bottom column in the frame structure is buried in the soil,sometimes it should be considered the affects from the body of the soil when calculating the ground floor of the frame structure. The Winkler assumes is quoted in this article, as considering the coefficient of the Soil-column interaction, the equivalent height calculating formula of the column restrained by the earth is deduced , this can change the frame structure that restrained by the earth into the commonly structure to calculate. It illustrates that the restrained load by the earth in the bottom of the structure has t

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5

Zhang, C. Z. "A comparison between two internal structure models of the Earth." Earth, Moon and Planets 54, no. 2 (1991): 129–43. http://dx.doi.org/10.1007/bf00057584.

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6

Gudkova, T. V., and V. N. Zharkov. "Models of the Internal Structure of the Earth-like Venus." Solar System Research 54, no. 1 (2020): 20–27. http://dx.doi.org/10.1134/s0038094620010049.

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7

Orozco, Miguel, Antonio M. Álvarez-Valero, Francisco M. Alonso-Chaves, and John P. Platt. "Internal structure of a collapsed terrain." Tectonophysics 385, no. 1-4 (2004): 85–104. http://dx.doi.org/10.1016/j.tecto.2004.04.025.

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8

Zhang, Keke, Dali Kong, and Gerald Schubert. "Shape, Internal Structure, Zonal Winds, and Gravitational Field of Rapidly Rotating Jupiter-Like Planets." Annual Review of Earth and Planetary Sciences 45, no. 1 (2017): 419–46. http://dx.doi.org/10.1146/annurev-earth-063016-020305.

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9

Nishimura, K., H. Narita, N. Maeno, and K. Kawada. "The Internal Structure of Powder-Snow Avalanches." Annals of Glaciology 13 (1989): 207–10. http://dx.doi.org/10.1017/s0260305500007904.

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The internal structure of powder-snow avalanches was investigated at Kurobe Canyon in the Shiai-dani area of Japan in 1988. Internal velocity was derived for avalanches of this kind by frequency analysis of impact-force data, and was found to undergo a remarkable change with time. The shear of the avalanche flow was estimated to range from 1 to 7 s−1. The front region of the avalanche wind was observed to precede the front of the avalanche by a distance of 17.3 m. The maximum wind velocity was comparable with the internal velocity of the front region of the avalanche.

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10

Nishimura, K., H. Narita, N. Maeno, and K. Kawada. "The Internal Structure of Powder-Snow Avalanches." Annals of Glaciology 13 (1989): 207–10. http://dx.doi.org/10.3189/s0260305500007904.

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The internal structure of powder-snow avalanches was investigated at Kurobe Canyon in the Shiai-dani area of Japan in 1988. Internal velocity was derived for avalanches of this kind by frequency analysis of impact-force data, and was found to undergo a remarkable change with time. The shear of the avalanche flow was estimated to range from 1 to 7 s−1. The front region of the avalanche wind was observed to precede the front of the avalanche by a distance of 17.3 m. The maximum wind velocity was comparable with the internal velocity of the front region of the avalanche.

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11

BUNGE, Hans‐Peter, Lorenzo COLLI, Siavash GHELICHKHAN, and Jens OESER. "Deep Time Reconstructions of Internal Earth Structure with the Adjoint Method." Acta Geologica Sinica - English Edition 93, S3 (2019): 3–4. http://dx.doi.org/10.1111/1755-6724.14226.

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12

Lupishko, Dmitrij, and Zhanna Pozhalova. "Near-Earth Objects 400 Years after Galileo: Physical Properties and Internal Structure." Proceedings of the International Astronomical Union 6, S269 (2010): 234–39. http://dx.doi.org/10.1017/s1743921310007477.

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AbstractThe review contains the most recent data on near-Earth objects such as their sizes and densities, rotation and shapes, taxonomy and mineralogy, optical properties and structure of their surfaces, binary systems among the NEOs and internal structure of asteroids and comets constituted the NEO population.

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13

Bradley, P. A. "The Internal Structure of White Dwarf Stars Using the Whole Earth Telescope." International Astronomical Union Colloquium 139 (1993): 117–19. http://dx.doi.org/10.1017/s0252921100117051.

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AbstractWhite dwarfs are the final end state for the majority of stars, and hold clues to help solve many current pressing astrophysical problems. We can perform asteroseismology on the pulsating white dwarfs to better understand their internal structure and input physics, paving the way to a better understanding of astrophysics, stellar evolution, and the history of our Galaxy. I describe briefly the potential of asteroseismology by using it to infer the internal structure of PG1159-035.

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14

Matoušek, Václav, Štĕpán Zrostlík, Luigi Fraccarollo, Anna Prati, and Michele Larcher. "Internal structure of intense collisional bedload transport." Earth Surface Processes and Landforms 44, no. 11 (2019): 2285–96. http://dx.doi.org/10.1002/esp.4641.

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15

Denis, C., M. Amalvict, Y. Rogister, and S. Tomecka-Suchoń. "Methods for computing internal flattening, with applications to the Earth's structure and geodynamics." Geophysical Journal International 132, no. 3 (1998): 603–42. http://dx.doi.org/10.1046/j.1365-246x.1998.00449.x.

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SUMMARY After general comments (Section 1) on using variational procedures to compute the oblateness of internal strata in the Earth and slowly rotating planets, we recall briefly some basic concepts about barotropic equilibrium figures (Section 2), and then proceed to discuss several accurate methods to derive the internal flattening. The algorithms given in Section 3 are based on the internal gravity field theory of Clairaut, Laplace and Lyapunov. They make explicit use of the concept of a level surface. The general formulation given here leads to a number of formulae which are of both theor

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16

Liu, Tai, Guangyu Fu, Yawen She, and Cuiping Zhao. "Co-seismic internal deformations in a spherical layered earth model." Geophysical Journal International 221, no. 3 (2020): 1515–31. http://dx.doi.org/10.1093/gji/ggaa086.

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SUMMARY Using a numerical integral method, we deduced a set of formulae for the co-seismic internal deformation in a spherically symmetric earth model, simultaneously taking self-gravitation, compressibility and realistically stratified structure of the Earth into account. Using these formulae, we can calculate the internal deformation at an arbitrary depth caused by an arbitrary seismic source. To demonstrate the correctness of our formulae, we compared our numerical solutions of radial functions with analytical solutions reported by Dong & Sun based on a homogeneous earth model; we found

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17

Stenberg, G., T. Oscarsson, M. André, et al. "Internal structure and spatial dimensions of whistler wave regions in the magnetopause boundary layer." Annales Geophysicae 25, no. 11 (2007): 2439–51. http://dx.doi.org/10.5194/angeo-25-2439-2007.

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Abstract. We use whistler waves observed close to the magnetopause as an instrument to investigate the internal structure of the magnetopause-magnetosheath boundary layer. We find that this region is characterized by tube-like structures with dimensions less than or comparable with an ion inertial length in the direction perpendicular to the ambient magnetic field. The tubes are revealed as they constitute regions where whistler waves are generated and propagate. We believe that the region containing tube-like structures extend several Earth radii along the magnetopause in the boundary layer.

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18

Otegi, J. F., C. Dorn, R. Helled, F. Bouchy, J. Haldemann, and Y. Alibert. "Impact of the measured parameters of exoplanets on the inferred internal structure." Astronomy & Astrophysics 640 (August 2020): A135. http://dx.doi.org/10.1051/0004-6361/202038006.

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Context. Exoplanet characterization is one of the main foci of current exoplanetary science. For super-Earths and sub-Neptunes, we mostly rely on mass and radius measurements, which allow us to derive the mean density of the body and give a rough estimate of the bulk composition of the planet. However, the determination of planetary interiors is a very challenging task. In addition to the uncertainty in the observed fundamental parameters, theoretical models are limited owing to the degeneracy in determining the planetary composition. Aims. We aim to study several aspects that affect the inter

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19

Kuznetsov, V. G. "Internal Structure of Carbonate Formations in Various Climate Regions." Doklady Earth Sciences 495, no. 1 (2020): 808–11. http://dx.doi.org/10.1134/s1028334x20110094.

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20

Nixon, Matthew C., and Nikku Madhusudhan. "How deep is the ocean? Exploring the phase structure of water-rich sub-Neptunes." Monthly Notices of the Royal Astronomical Society 505, no. 3 (2021): 3414–32. http://dx.doi.org/10.1093/mnras/stab1500.

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ABSTRACT Understanding the internal structures of planets with a large H2O component is important for the characterization of sub-Neptune planets. The finding that the mini-Neptune K2-18b could host a liquid water ocean beneath a mostly hydrogen envelope motivates a detailed examination of the phase structures of water-rich planets. To this end, we present new internal structure models for super-Earths and mini-Neptunes that enable detailed characterization of a planet’s water component. We use our models to explore the possible phase structures of water worlds and find that a diverse range of

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21

Pollard, W. H., and H. M. French. "The Internal Structure and Ice Crystallography of Seasonal Frost Mounds." Journal of Glaciology 31, no. 108 (1985): 157–62. http://dx.doi.org/10.1017/s0022143000006407.

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AbstractThe crystal character of the ice core within frost blisters supports the hypothesis that groundwater injection into residual zones of the active layer followed by rapid freezing is the primary growth mechanism for these features. The ice core is characterized by an upper zone of relatively small randomly arranged equigranular ice crystals which change with increasing depth to columnar anhedral crystals, commonly exceeding 200 mm in length, and with crystal diameters ranging between 25 and 35 mm. Petrofabric analyses show that thec-axis orientations are normal to crystal elongations, wi

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22

Hansen, A. C., and R. L. Brown. "The Granular Structure of Snow: An Internal-State Variable Approach." Journal of Glaciology 32, no. 112 (1986): 434–38. http://dx.doi.org/10.1017/s0022143000012144.

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AbstractA statistical model characterizing the granular structure of snow is developed using quantitative stereology. The model is based on specific parameters (e.g. bond radius, grain-size, etc.) which take the form of internal-state variables in a constitutive theory for high-rate deformation of snow. In addition to parameters developed by other authors in previous investigations, a new parameter characterizing the mean bond length is developed. More significantly, general relations are derived for the mean number of bonds per grain and mean number of grains per unit volume without making an

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23

Ross, N., C. Harris, P. J. Brabham, and T. H. Sheppard. "Internal Structure and Geological Context of Ramparted Depressions, Llanpumsaint, Wales." Permafrost and Periglacial Processes 22, no. 4 (2011): 291–305. http://dx.doi.org/10.1002/ppp.708.

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24

Weiss, J., M. Montagnat, B. Cinquin-Lapierre, et al. "Waterfall ice: mechanical stability of vertical structures." Journal of Glaciology 57, no. 203 (2011): 407–15. http://dx.doi.org/10.3189/002214311796905587.

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AbstractWe present a study of the mechanical (in)stability of the ephemeral waterfall ice structures that form from the freezing of liquid water seeping on steep rock. Three vertical structures were studied, two near Glacier d’Argentière, France, and one in the Valsavarenche valley, northern Italy. The generation of internal stresses in the ice structure in relation to air- and ice-temperature conditions is analyzed from pressure sensor records. Their role in the mechanical instability of the structures is discussed from a photographic survey of these structures. The main result is that dramat

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25

Xie, Quanyi, Jian Liu, Bo Han, Hongtao Li, Yuying Li, and Xuanzheng Li. "Critical Hydraulic Gradient of Internal Erosion at the Soil–Structure Interface." Processes 6, no. 7 (2018): 92. http://dx.doi.org/10.3390/pr6070092.

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Internal erosion at soil–structure interfaces is a dangerous failure pattern in earth-fill water-retaining structures. However, existing studies concentrate on the investigations of internal erosion by assuming homogeneous materials, while ignoring the vulnerable soil–structure-interface internal erosion in realistic cases. Therefore, orthogonal and single-factor tests are carried out with a newly designed apparatus to investigate the critical hydraulic gradient of internal erosion on soil–structure interfaces. The main conclusions can be draw as follows: (1) the impact order of the three fact

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26

Bublikova, T. M., V. S. Balitsky, D. A. Khanin, A. N. Nekrasov, and T. V. Setkova. "Features of the Internal Structure of a Synthetic Malachite." Moscow University Geology Bulletin 74, no. 1 (2019): 73–80. http://dx.doi.org/10.3103/s0145875219010034.

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27

Zumr, David, Václav David, Josef Krása, and Jiří Nedvěd. "Geophysical Evaluation of the Inner Structure of a Historical Earth-Filled Dam." Proceedings 2, no. 11 (2018): 664. http://dx.doi.org/10.3390/proceedings2110664.

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Small earth dams usually lack the detailed seepage monitoring system that would provide high resolution data on changes in seepage flow. Alternative solution is monitoring of the temperature and electrical resistivity in the body of the dams. Geophysical methods are useful techniques for a non-destructive exploration of the subsurface. We have utilized the combination of electrical resistivity tomography (ERT), ground penetrating radar (GPR) and multi-depth electromagnetical conductivity meter (CMD) techniques to observe the inner structure, especially internal failures, of the historical eart

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28

Florentine, Caitlyn, Mark Skidmore, Marvin Speece, Curtis Link, and Colin A. Shaw. "Geophysical analysis of transverse ridges and internal structure at Lone Peak Rock Glacier, Big Sky, Montana, USA." Journal of Glaciology 60, no. 221 (2014): 453–62. http://dx.doi.org/10.3189/2014jog13j160.

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AbstractRock glaciers are periglacial alpine landforms that are found in many locations worldwide. Whereas well-developed models of deformation are established for traditional alpine glaciers, rock glacier deformation is poorly understood. Geophysical data from Lone Peak Rock Glacier (LPRG), southwest Montana, USA, are paired with lidar bare-earth 1 m digital elevation model (DEM) analysis to explore potential genetic relationships between internal composition, structure and regularly spaced arcuate transverse ridges expressed at the rock glacier surface. The internal composition of LPRG is he

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29

Cuevas, Julia. "Internal structure of the Adra Nappe (Alpujarride Complex, Betics, Spain)." Tectonophysics 200, no. 1-3 (1991): 199–212. http://dx.doi.org/10.1016/0040-1951(91)90015-k.

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30

Zhou, Yao, Hao Pan, and Yuan Feng Wang. "Testing and Analysis on Subway Station Structure under Dynamic Vibration Loads." Advanced Materials Research 716 (July 2013): 648–52. http://dx.doi.org/10.4028/www.scientific.net/amr.716.648.

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Structure health monitoring system is used to monitor structural responses in real time. Dynamic performances of subway station structures are help to analyze seismic performances of the structures. Through structure health monitoring system of a subway station structure, dynamic responses of the subway station structure were tested under railway loads. The dynamic strain and internal forces of subway station structure are obtained. As restrained by earth, dynamic responses of the subway station structure is not significant change from most surface structures. Wavelet and multiscale analysis c

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31

BAUER, SIEGFRIED J. "Planet Earth – our oasis in space." European Review 12, no. 1 (2004): 111–19. http://dx.doi.org/10.1017/s1062798704000092.

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Planet Earth is unique in our solar system as an abode of life. In contrast to its planetary neighbours, the presence of liquid water, a benign atmospheric environment, a solid surface and an internal structure providing a protective magnetic field make it a suitable habitat for man. While natural forces have shaped the Earth over millennia, man through his technological prowess may become a threat to this oasis of life in the solar system.

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32

Petrov, Vladislav P., Vladimir A. Chernyshev, and Anatoly E. Nikiforov. "Structural and Vibrational Properties of Crystals with a Rare-Earth Sublattice: Ab Initio Calculations." Solid State Phenomena 271 (January 2018): 85–91. http://dx.doi.org/10.4028/www.scientific.net/ssp.271.85.

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We investigated the crystal structure, vibrational and elastic properties of crystals with a rare-earth sublattice related to different structural types at ab initio level of modeling: elpasolite Cs2NaRF6 −> pyrochlore R2Ti2O7 −> ferroborate RFe3(BO3)4, where R is a rare-earth ion or yttrium. The calculations were performed in the framework of a density functional theory using the hybrid functionals containing local and non-local contribution (i.e. Hartree-Fock exchange term) to the exchange energy. We used CRYSTAL program for simulating periodic structures in the MO LCAO approximation.

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33

Matonti, C., N. Attree, O. Groussin, et al. "Bilobate comet morphology and internal structure controlled by shear deformation." Nature Geoscience 12, no. 3 (2019): 157–62. http://dx.doi.org/10.1038/s41561-019-0307-9.

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34

Ring, Uwe, Lothar Ratschbacher, Wolfgang Frisch, Sören DÜrr, and Susanne Borchert. "The internal structure of the Arosa Zone (Swiss-Austrian Alps)." Geologische Rundschau 79, no. 3 (1990): 725–39. http://dx.doi.org/10.1007/bf01879211.

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35

Kaurova, I. A., D. M. Gorshkov, G. M. Kuz'micheva, and V. B. Rybakov. "COMPOSITION AND STRUCTURE OF THE HUNTITE-FAMILY COMPOUNDS." Fine Chemical Technologies 13, no. 6 (2018): 42–51. http://dx.doi.org/10.32362/2410-6593-2018-13-6-42-51.

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The literature data on the composition and structure of rare-earth borate compounds of the huntite family with the general composition LnM3(BO3)4, where Ln3+ = Y, La = Lu and M3+ = Al, Fe, Cr, Ga, Sc as well as a number of solid solutions with М3+ = Sc are systematized. The difference between the real compositions of crystals and the compositions of the initial mixture, the most characteristic of rare-earth scandium borates, is shown. The significant role of the composition in the manifestation of the compounds symmetry is established. The necessity of determining the crystals symmetry only on

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36

Némeni, T. M., V. V. Braitsev, and A. M. Krasil’nikov. "Use of the resistivity computer tomography method for determining the internal structure of earth dams." Hydrotechnical Construction 32, no. 4 (1998): 198–204. http://dx.doi.org/10.1007/bf02918726.

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37

KOBAYASHI, Takaaki, Shinji SASSA, Kojiro SUZUKI, et al. "PEFORMANCE OF GEOTECHNICAL FILTER ON MITIGATION OF GEOTEXTILE FAILURE AND INTERNAL EROSION IN EARTH STRUCTURE." Journal of Japan Society of Civil Engineers, Ser. B3 (Ocean Engineering) 73, no. 2 (2017): I_354—I_359. http://dx.doi.org/10.2208/jscejoe.73.i_354.

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38

Bartelt, Perry, Othmar Buser, and Martin Kern. "Dissipated work, stability and the internal flow structure of granular snow avalanches." Journal of Glaciology 51, no. 172 (2005): 125–38. http://dx.doi.org/10.3189/172756505781829638.

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AbstractWe derive work dissipation functionals for granular snow avalanches flowing in simple shear. Our intent is to apply constructive theorems of non-equilibrium thermodynamics to the snow avalanche problem. Snow chute experiments show that a bi-layer system consisting of a non-yielded flow plug overriding a sheared fluidized layer can be used to model avalanche flow. We show that for this type of constitutive behaviour the dissipation functionals are minimum at steady state with respect to variations in internal velocity; however, the functionals must be constrained by subsidiary mass- con

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39

?urawek, Roman. "Internal Structure of a relict rock glacier, ?l??a Massif, Southwest Poland." Permafrost and Periglacial Processes 13, no. 1 (2002): 29–42. http://dx.doi.org/10.1002/ppp.403.

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40

Sánchez-Núñez, J. M., J. L. Macías, Ricardo Saucedo, et al. "Geomorphology, internal structure and evolution of alluvial fans at Motozintla, Chiapas, Mexico." Geomorphology 230 (February 2015): 1–12. http://dx.doi.org/10.1016/j.geomorph.2014.10.003.

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41

Wang, Xin, Xie Hui Luo, Wan xue Long, and Bo Jiang. "Back analysis of pile and anchor retaining structure based on BOTDA distributed optical fiber sensing technology." E3S Web of Conferences 248 (2021): 01036. http://dx.doi.org/10.1051/e3sconf/202124801036.

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In order to understand the deformation law and internal force distribution characteristics of the pile-anchor retaining structure in deep foundation pit engineering, the stress of the pile-anchor retaining system in the process of foundation pit excavation was tested by using the distributed optical fiber sensing technology of BOTDA. It uses the supporting pile cloth to set up the strain cable to collect the strain from the excavation process to the stability of the foundation pit, which analyzes the stress and internal force distribution. The results show that the overall deformation of the f

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42

Barde-Cabusson, Stéphanie, Xavier Bolós, Dario Pedrazzi, et al. "Electrical resistivity tomography revealing the internal structure of monogenetic volcanoes." Geophysical Research Letters 40, no. 11 (2013): 2544–49. http://dx.doi.org/10.1002/grl.50538.

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43

Montagnat, M., J. Weiss, B. Cinquin-Lapierre, et al. "Waterfall ice: formation, structure and evolution." Journal of Glaciology 56, no. 196 (2010): 225–34. http://dx.doi.org/10.3189/002214310791968412.

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AbstractFor the first time, to our knowledge, a scientific study of the formation and evolution of waterfall ice, the ephemeral ice structures that form from the freezing of liquid water seeping on steep rock, was performed. We surveyed and analysed three waterfall ice structures near Glacier d’Argentière, Mont Blanc massif, France, between winter 2007 and spring 2009. We reconstruct the global evolution of two vertical ice structures using automatic digital cameras, while the internal ice microstructure was analysed using ice coring and sampling. Macro- and microstructural observations are co

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44

Zhang, C. Z., and K. Zhang. "On the internal structure and magnetic fields of." Earth, Moon, and Planets 69, no. 3 (1995): 237–47. http://dx.doi.org/10.1007/bf00643786.

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45

Tang, XueYuan, Bo Sun, ZhanHai Zhang, XiangPei Zhang, XiangBin Cui, and Xin Li. "Structure of the internal isochronous layers at Dome A, East Antarctica." Science China Earth Sciences 54, no. 3 (2010): 445–50. http://dx.doi.org/10.1007/s11430-010-4065-1.

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46

Jishi, Radi A., and Marcus A. Lucas. "ZnSnS3: Structure Prediction, Ferroelectricity, and Solar Cell Applications." International Journal of Photoenergy 2016 (2016): 1–9. http://dx.doi.org/10.1155/2016/6193502.

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The rapid growth of the solar energy industry is driving a strong demand for high performance, efficient photoelectric materials. In particular, ferroelectrics composed of earth-abundant elements may be useful in solar cell applications due to their large internal polarization. Unfortunately, wide band gaps prevent many such materials from absorbing light in the visible to mid-infrared range. Here, we address the band gap issue by investigating the effects of substituting sulfur for oxygen in the perovskite structure ZnSnO3. Using evolutionary methods, we identify the stable and metastable str

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47

Somoza, R., A. J. Tomlinson, C. B. Zaffarana, et al. "Tectonic rotations and internal structure of Eocene plutons in Chuquicamata, northern Chile." Tectonophysics 654 (July 2015): 113–30. http://dx.doi.org/10.1016/j.tecto.2015.05.005.

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48

Bayly, Brian. "The Vredefort structure: estimates of energy for some internal sources and processes." Tectonophysics 171, no. 1-4 (1990): 153–67. http://dx.doi.org/10.1016/0040-1951(90)90096-q.

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49

Leopold, M., M. W. Williams, N. Caine, J. Völkel, and D. Dethier. "Internal structure of the Green Lake 5 rock glacier, Colorado Front Range, USA." Permafrost and Periglacial Processes 22, no. 2 (2011): 107–19. http://dx.doi.org/10.1002/ppp.706.

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50

Machelski, Czesław. "Effects of Surrounding Earth on Shell During the Construction of Flexible Bridge Structures." Studia Geotechnica et Mechanica 41, no. 2 (2019): 67–73. http://dx.doi.org/10.2478/sgem-2019-0002.

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AbstractA characteristic feature of soil-steel structures is that, unlike in typical bridges, the backfill and the carriageway pavement with its foundation play a major role in bearing loads. In the soil-steel structure model, one can distinguish two structural subsystems: the shell made of corrugated plates and the backfill with the pavement layers. The interactions between the subsystems are modelled as interfacial interactions, that is, forces normal and tangent to the surface of the shell. This is a static condition of the consistency of mutual interactions between the surrounding earth an

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