Статті в журналах: "Solid Earth Sciences"

1

Sun, Weidong. "Challenges in Solid Earth Sciences." Solid Earth Sciences 1, no. 1 (June 2016): 1–4. http://dx.doi.org/10.1016/j.sesci.2016.06.001.

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2

Anonymous. "Committee on solid-earth sciences." Eos, Transactions American Geophysical Union 70, no. 12 (1989): 184. http://dx.doi.org/10.1029/89eo00096.

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3

Anonymous. "New report examines solid-Earth sciences." Eos, Transactions American Geophysical Union 74, no. 11 (March 16, 1993): 122. http://dx.doi.org/10.1029/93eo00352.

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4

Begaudeau, Karine, Yann Morizet, Pierre Florian, Michael Paris, and Jean-Claude Mercier. "Solid-state NMR analysis of Fe-bearing minerals: implications and applications for Earth sciences." European Journal of Mineralogy 24, no. 3 (May 21, 2012): 535–50. http://dx.doi.org/10.1127/0935-1221/2012/0024-2192.

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5

Stankus, Tony. "Sciences of the Solid Earth and Other Planets." Serials Librarian 27, no. 2-3 (April 8, 1996): 199–210. http://dx.doi.org/10.1300/j123v27n02_17.

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6

Eaton, Gordon. "Viewpoint on the solid Earth sciences and society." Eos, Transactions American Geophysical Union 74, no. 41 (1993): 466. http://dx.doi.org/10.1029/93eo00551.

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7

Willis, Pascal, Laurent Soudarin, Christian Jayles, and Lucie Rolland. "DORIS applications for solid earth and atmospheric sciences." Comptes Rendus Geoscience 339, no. 16 (December 2007): 949–59. http://dx.doi.org/10.1016/j.crte.2007.09.015.

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8

Oliver, J. "Solid earth science during the 21st century." Eos, Transactions American Geophysical Union 72, no. 11 (1991): 121. http://dx.doi.org/10.1029/90eo00099.

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9

Linn, Anne M. "Identifying grand research questions in the solid-earth sciences." Eos, Transactions American Geophysical Union 87, no. 9 (2006): 98. http://dx.doi.org/10.1029/2006eo090004.

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10

Thybo, Hans, Mike Sandiford, Tom Parsons, and Mian Liu. "Tectonophysics: The International Journal of Integrated Solid Earth Sciences." Tectonophysics 460, no. 1-4 (November 2008): v—vi. http://dx.doi.org/10.1016/s0040-1951(08)00518-0.

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11

Manea, Vlad Constantin, Marina Manea, Mihai Pomeran, Lucian Besutiu, and Luminita Zlagnean. "Computational Fluid Dynamics in Solid Earth Sciences–a HPC challenge." Acta Universitaria 22, no. 7 (November 15, 2012): 32–36. http://dx.doi.org/10.15174/au.2012.357.

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Presently, the Solid Earth Sciences started to move towards implementing High Performance Computational (HPC) research facilities. One of the key tenants of HPC is performance, which strongly depends on the interaction between software and hardware. In this paper, they are presented benchmark results from two HPC systems. Testing a Computational Fluid Dynamics (CFD) code specific for Solid Earth Sciences, the HPC system Horus, based on Gigabit Ethernet, performed reasonably well compared with its counterpart CyberDyn, based on Infiniband QDR fabric. However, the HPCC CyberDyn based on low-latency high-speed QDR network dedicated to MPI traffic outperformed the HPCC Horus. Due to the high-resolution simulations involved in geodynamic research studies, HPC facilities used in Earth Sciences should benefit from larger up-front investment in future systems that are based on high-speed interconnects.

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12

Watson, E. Bruce, and Ethan F. Baxter. "Diffusion in solid-Earth systems." Earth and Planetary Science Letters 253, no. 3-4 (January 2007): 307–27. http://dx.doi.org/10.1016/j.epsl.2006.11.015.

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13

Seber, Dogan, David Steer, Eric Sandvol, Christine Sandvol, Carrie Brindisi, and Muawia Barazangi. "Design and Development of Information Systems for the Geosciences: An Application to the Middle East." GeoArabia 5, no. 2 (April 1, 2000): 269–96. http://dx.doi.org/10.2113/geoarabia0502269.

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ABSTRACT As our understanding grows of how the Earth functions as a complex system of myriad interrelated mechanisms, it becomes clear that a revolutionary and novel approach is needed to study and understand it. In order to take advantage of an ever-growing number of observations and large data sets and to employ them efficiently in multidisciplinary studies aimed at solving earth system science problems, we are developing a comprehensive Solid Earth Information System (SEIS). The complex nature of the solid earth sciences raises serious challenges for geoscientists in their quest to understand the nature and the dynamic mechanisms at work in the planet. SEIS forms a first step in developing a broader and more comprehensive information system for earth system sciences designed for the needs of the geoscientists of the 21st century. In a way, SEIS is a step towards the Digital Earth. Application of SEIS to the complex tectonics of the Middle East shows that information systems are crucial in multidisciplinary research studies and open new avenues in research efforts. SEIS includes an Internet module that provides open access to anyone interested. Researchers as well as educators and students can access this knowledge and information system at http://atlas.geo.cornell.edu.

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14

Grant, Shermonta L. "Albarede to lead JGR-Solid Earth." Eos, Transactions American Geophysical Union 81, no. 43 (2000): 499. http://dx.doi.org/10.1029/00eo00360.

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15

Baltuck, Miriam. "Solid Earth Programs meet Coolfont Goals." Eos, Transactions American Geophysical Union 78, no. 47 (1997): 537. http://dx.doi.org/10.1029/97eo00321.

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16

Chousianitis, Konstantinos, Xanthos Papanikolaou, George Drakatos, and G. Akis Tselentis. "NOANET: A Continuously Operating GNSS Network for Solid-Earth Sciences in Greece." Seismological Research Letters 92, no. 3 (March 17, 2021): 2050–64. http://dx.doi.org/10.1785/0220200340.

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Abstract The NOANET network is a continuously operating high-rate Global Navigation Satellite System (GNSS) network in Greece whose primary role is to enhance and support geophysical research employing GNSS data. This network is operated by the Institute of Geodynamics of the National Observatory of Athens and currently (September 2020) consists of 26 stations, most of which are located close to major seismogenic structures of Greece to optimally measure tectonic and seismically induced motions. All NOANET receivers are configured to record and collect data with a sampling rate of 1 Hz, although some of them also collect data every 5 Hz on their ring buffer. The network is committed to free and open data sharing within the scientific community, and the collected data are made available via the NOANET data repository and distribution point for all interested parties with no limitations. Integrity, validity, and quality checks of the acquired data are performed using a variety of software tools along with in-house developed programs to supervise the network performance and detect ill-formed data and/or awkward station behavior. In addition, the conventional low-rate GNSS observation data of all NOANET stations are routinely processed on a daily basis to supervise their performance through their position time series. Since the beginning of its establishment, the NOANET network has recorded a variety of deformation signals, and a large number of published papers have used GNSS data from stations that are part of NOANET to constrain, model, and interpret the nature of the associated geophysical phenomena.

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17

Gray, Deborah. "JGR-Solid Earth moves toward electronic communication." Eos, Transactions American Geophysical Union 75, no. 6 (1994): 59. http://dx.doi.org/10.1029/94eo00775.

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18

Anonymous. "Hinze appointed editor of JGR-Solid Earth." Eos, Transactions American Geophysical Union 73, no. 2 (1992): 12. http://dx.doi.org/10.1029/91eo00015.

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19

Anonymous. "JGR-Solid Earth to commemorate AGU anniversary." Eos, Transactions American Geophysical Union 74, no. 4 (January 26, 1993): 42. http://dx.doi.org/10.1029/93eo00242.

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20

Anonymous. "Davis takes the reins of JGR—Solid Earth." Eos, Transactions American Geophysical Union 77, no. 48 (1996): 479. http://dx.doi.org/10.1029/96eo00319.

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21

Simons, Frederik J., Thorsten W. Becker, James B. Kellogg, Magali Billen, Jeanne Hardebeck, Cin-Ty A. Lee, Laurent G. J. Montési, Wendy Panero, and Shuie Zhong. "Young solid Earth researchers of the world unite!" Eos, Transactions American Geophysical Union 85, no. 16 (April 20, 2004): 160–61. http://dx.doi.org/10.1029/2004eo160011.

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22

Stein, C. A. "The solid Earth: An introduction to global geophysics." Eos, Transactions American Geophysical Union 72, no. 40 (1991): 427. http://dx.doi.org/10.1029/90eo00309.

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23

Hinze, William J. "Some first steps for JGR-Solid Earth." Journal of Geophysical Research: Solid Earth 99, B2 (February 10, 1994): 2587–88. http://dx.doi.org/10.1029/94jb00091.

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24

Wilson, Leonard. "Religious assumptions in Lord Kelvin's estimates of the Earth's age." Earth Sciences History 29, no. 2 (December 1, 2010): 187–212. http://dx.doi.org/10.17704/eshi.29.2.46678x0701k62j0j.

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Lord Kelvin's estimates of the Earth's age were not necessary consequences of his physics. Religion influenced his physics and his arguments for a limited age of the Earth. Kelvin's primary aim was to destroy Charles Darwin's theory of evolution by natural selection by attacking the uniformitarian geology on which Darwin's theory was founded. His calculations of the age of the Earth contained a fundamental contradiction. He assumed that the Earth began as a hot liquid sphere, but Fourier's mathematics, which he used to calculate the rate of cooling, applied only to heat conducted through a solid. Kelvin's assumption of an initially hot liquid Earth was a necessary consequence of his thermodynamics. Energy could neither be created nor destroyed. The heat within the Earth must, therefore, be derived from its first creation by God. Kelvin never admitted the contradiction between the original hot liquid Earth and his calculation of its cooling on the assumption that the Earth was solid throughout, but in 1897 his imagined account of the initial Earth was a search for a solid Earth amenable to his calculations. The heat flow through the solid crust was very small in proportion to the total internal heat of the Earth. If Kelvin had included the total internal heat in his calculations, he would have arrived at much higher figures for the age of the Earth.

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25

Lee, Hyongki, C. K. Shum, Chung-Yen Kuo, Yuchan Yi, and Alexander Braun. "Application of TOPEX Altimetry for Solid Earth Deformation Studies." Terrestrial, Atmospheric and Oceanic Sciences 19, no. 1-2 (2008): 37. http://dx.doi.org/10.3319/tao.2008.19.1-2.37(sa).

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26

Manea, Vlad Constantin, Marina Manea, Mihai Pomeran, Lucian Besutiu, and Luminita Zlagnean. "A parallelized particle tracing code for CFD simulations in Earth sciences." Acta Universitaria 22, no. 5 (August 15, 2012): 19–26. http://dx.doi.org/10.15174/au.2012.358.

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The problem of convective flows in a highly viscous fluid represents a common research direction in Earth sciences. For tracing the convective motion of the fluid material, a source passive particles (or tracers) that flow at a local convection velocity and do not affect the pattern of flow it is commonly used. Here we present a parallelized tracer code that uses passive and weightless particles with their position computed from their displacement during a small time interval at the velocity of flow previously calculated for a given point in space and time. The tracer code is integrated in the open source package CitcomS, which is widely used in the solid earth community (www.geodynamics.org). We benchmarked the tracer code on the state-of-the-art CyberDyn parallel machine, a High Performance Computing (HPC) Cluster with 1344 computing cores available at the Institute of Geodynamics of the Romanian Academy.

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27

Issaka, Yakubu, and Bernard Kumi-Boateng. "ARTIFICIAL INTELLIGENCE TECHNIQUES FOR PREDICTING TIDAL EFFECTS BASED ON GEOGRAPHIC LOCATIONS IN GHANA." Geodesy and cartography 46, no. 1 (April 3, 2020): 1–7. http://dx.doi.org/10.3846/gac.2020.7696.

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Tidal forces as a result of attraction of external bodies (Sun, Moon and Stars) through gravity and are a source of noise in many geoscientific field observations. The solid earth tides cause deformation. This deformation results in displacement in geographic positions on the surface of the earth. The displacement due to tidal effects can result in deformation of engineering structures, loss of lives, and economic cost. Tidal forces also help in detecting other environmental and tectonic signals. This study quantifies the effects of solid earth tides on stationary survey controls in five regions of Ghana. The study is in two stages: firstly, the solid earth tides were estimated for each control by a geometric approach (combining Navier’s equation of motion and Love theories). Secondly, estimation using two artificial intelligence methods (Multivariate Adaptive Regression Splines (MARS) and Backpropagation Artificial Neural Network (ANN)). Based on statistical indices of Mean Square Error (MSE) and Correlation Coefficient (R), BPANN, and MARS models can be used as a realistic alternative technique in quantifying solid earth tides for the study area. The MSE and R (MSE; BPANN = 1.3249 × 10–04 and MSE; MARS = 2.2052 × 10–06; R; BPANN = –0.6067 and R; MARS 0.6570) values indicate that MARS outperforms BPANN in quantifying solid earth tides in the study area. BPANN and MARS can be used as an efficient tool for quantifying tidal values based on geographic positions for geodetic deformation studies within the study area.

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28

Simons, Frederik J., Thorsten W. Becker, James B. Kellogg, Magali Billen, Cin-Ty A. Lee, Laurent G. J. Montèsi, Wendy Panero, and Shijie Zhong. "MYRES: A program to unite young solid earth researchers." Eos, Transactions American Geophysical Union 86, no. 5 (2005): 48. http://dx.doi.org/10.1029/2005eo050005.

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29

Pasteris, Jill D., and Olivier Beyssac. "Welcome to Raman Spectroscopy: Successes, Challenges, and Pitfalls." Elements 16, no. 2 (April 1, 2020): 87–92. http://dx.doi.org/10.2138/gselements.16.2.87.

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Geoscientists quickly recognized the broad applicability of Raman micro-probe spectroscopy to the Earth and planetary sciences, especially after commercially built microprobe instruments became available in the early 1980s. Raman spectra are sensitive to even minor (chemical or structural) perturbations within chemical bonds in (even amorphous) solids, liquids, and gases and can, thus, help identify, characterize, and differentiate between individual minerals, fluid inclusions, glasses, carbonaceous materials, solid solution phases, strain in minerals, and dissolved species in multi-component solutions. The articles in this issue explore how Raman spectroscopy has deepened and broadened our understanding of geological and extraterrestrial materials and processes.

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30

Métivier, Laurent, Olivier de Viron, Clinton P. Conrad, Stéphane Renault, Michel Diament, and Geneviève Patau. "Evidence of earthquake triggering by the solid earth tides." Earth and Planetary Science Letters 278, no. 3-4 (February 2009): 370–75. http://dx.doi.org/10.1016/j.epsl.2008.12.024.

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31

Zhang, Shuai, and Lei Chen. "Melting Temperature of MgO under Pressure." Applied Mechanics and Materials 319 (May 2013): 19–22. http://dx.doi.org/10.4028/www.scientific.net/amm.319.19.

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The melting temperature-pressure phase diagram [Tm(P)-P] for magnesium oxide (MgO) is predicted through the Clapeyron equation where the pressure-dependent volume difference is modeled by introducing the effect of surface stress induced pressure. MgO is a material of key importance to earth sciences and solid-state physics: it is one of the most abundant minerals in the Earth and a prototype material for a large group of ionic oxides.

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32

Fujii, Naoyuki, Valeri Korneev, Junzo Kasahara, Hiromichi Higashihara, Sergey Goldin, Innokentty Chichinin, Rudolf Unger, Michael Zhdanov, Viktor Seleznev, and Viktor Seleznev. "First International Workshop on Active Monitoring in Solid Earth Geophysics." Eos, Transactions American Geophysical Union 86, no. 9 (2005): 92. http://dx.doi.org/10.1029/2005eo090006.

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33

de Grosbois, Anne. "Fowler CMR: The Solid Earth: An Introduction to Global Geophysics." Environmental Geology 48, no. 7 (October 2005): 968. http://dx.doi.org/10.1007/s00254-005-0038-7.

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34

Hinze, William J. "A new type of article for JGR-Solid Earth." Journal of Geophysical Research: Solid Earth 99, B2 (February 10, 1994): 2589–90. http://dx.doi.org/10.1029/94jb00092.

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35

Young, Alexander, Nicolas Flament, Simon E. Williams, Andrew Merdith, Xianzhi Cao, and R. Dietmar Müller. "Long-term Phanerozoic sea level change from solid Earth processes." Earth and Planetary Science Letters 584 (April 2022): 117451. http://dx.doi.org/10.1016/j.epsl.2022.117451.

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36

Sun, Linlin, Ziming Wang, Chengyu Li, Wei Tang, and Zhonglin Wang. "Probing Contact Electrification between Gas and Solid Surface." Nanoenergy Advances 3, no. 1 (January 2, 2023): 1–11. http://dx.doi.org/10.3390/nanoenergyadv3010001.

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Contact electrification exists everywhere and between every phase of matter. However, its mechanism still remains to be studied. The recent triboelectric nanogenerator serves as a probe and provides some new clues about the mechanism present in solid–solid, solid–liquid, and liquid–liquid contact electrification. The gas–solid model still remains to be exploited. Here, we investigated the contact electrification between gases and solids based on the single-electrode triboelectric nanogenerator. Our work shows that the amount of transferred charges between gas and solid particles increases with surface area, movement distance, and initial charges of particle increase. Furthermore, we find that the initial charges on the particle surface can attract more polar molecules and enhance gas collisions. Since ions in gas–solid contact are rare, we speculate that gas–solid contact electrification is mainly based on electron transfer. Further, we propose a theoretical model of gas–solid contact electrification involving the gas collision model and initial charges of the particle. Our study may have great significance to the gas–solid interface chemistry.

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37

Simonetti, Cristián. "The Petrified Anthropocene." Theory, Culture & Society 36, no. 7-8 (September 11, 2019): 45–66. http://dx.doi.org/10.1177/0263276419872814.

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The Anthropocene is seen by many scholars across the sciences and the humanities as a tool for political action. Yet the validation process for this term appears to be extremely conservative. According to geologists’ leading efforts to formalize the term, signals need to petrify in stratigraphic sequences in order to become candidates to mark the start of the Anthropocene. I argue that this emphasis results from a fossilized view of becoming, where time is seen as a punctuated accumulation of solid surfaces that are accessible only in retrospect. I show that this petrified view of change relates to a tendency to divorce earth and sky, which currently divides the practices of humanities scholars and geologists, as well as those of earth system scientists and stratigraphers collaborating on the formalization of the Anthropocene. Challenging this tendency, I conclude, requires opening up earth’s history to the more-than-solid flows of environmental change.

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38

Wu, Kai, Ce Ji, Lei Luo, and Xinyuan Wang. "Simulation Study of Moon-Based InSAR Observation for Solid Earth Tides." Remote Sensing 12, no. 1 (January 1, 2020): 123. http://dx.doi.org/10.3390/rs12010123.

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The observation of solid earth tides (SET) provides an important basis for understanding the structure of the earth’s interior, and has long been the focus of research in geoscience. However, actually, there still exist some limitations in capturing its global-scale information only with ground stations. Remote sensing technology can realize large-scale deformation monitoring of high point density constantly. However, it is still difficult for the artificial satellite system to meet the requirements of SET monitoring in terms of field of view and temporal resolution now. In this work, the moon is hypothesized as a new platform for SET observation combined with interferometric synthetic aperture radar (InSAR) technology. Based on the tidal model and lunar ephemeris, the spatial and temporal characteristics of the SET from the lunar view were analyzed. Furthermore, the calculations demonstrate that more abundant SET information can be observed in this view. After comparing various observation modes, the single-station with repeat-pass differential InSAR was selected for this simulation. We mainly considered the restriction of observation geometry on moon-based InSAR under three signal bandwidths, thereby providing a reference for the sensor design. The results demonstrate that the moon-based platform offers the potential to become an optimal SET observation method.

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39

Dickey, J., C. Bentley, R. Bilham, J. Carton, R. Eanes, T. Herring, W. Kaula, and G. S. E. Lagerloef. "Satellite gravity: insights into the solid Earth and its fluid envelope." Eos, Transactions American Geophysical Union 79, no. 20 (1998): 237. http://dx.doi.org/10.1029/98eo00171.

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40

Cui, Xiaona, Erlong Yang, Kaoping Song, and Yuming Wang. "The Seepage Model Considering Liquid/Solid Interaction in Confined Nanoscale Pores." Geofluids 2018 (August 19, 2018): 1–14. http://dx.doi.org/10.1155/2018/8302782.

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Different from conventional reservoirs, nanoscale pores and fractures are dominant in tight or shale reservoirs. The flow behaviors of hydrocarbons in nanopores (called “confined space”) are more complex than that of bulk spaces. The interaction between liquid hydrocarbons and solid pore wall cannot be neglected. The viscosity formula which is varied with the pore diameter and interaction coefficient of liquids and solids in confined nanopores has been introduced in this paper to describe the interaction effects of hydrocarbons and pore walls. Based on the Navier-Stokes equation, the governing equation considered liquid/solid effect in two dimensions has been established, and approximate theoretical solutions to the governing equations have been achieved after mathematic simplification. By introducing the vortex equation, the complex numerical seepage model has been discretized and solved. Numerical results show that the radial velocity distribution near the solid wall has an obvious change when considering the liquid/solid interaction. The results consist well with that approximate mathematical solution. And when the capillary radius is smaller, the liquid and solid interaction coefficient n is greater. The liquid and solid interaction obviously cannot be neglected in the seepage model if the capillary radius is small than 50 nm when n>0.1. The numerical model has also been further validated by two types of nanopore flow tests: from pore to throat and inversely from throat to pore. There is no big difference in flow regularity of throat to pore model considering when liquid/solid interaction or not, whereas the liquid/solid interaction of pore to throat model totally cannot be overlooked.

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41

TAKEDA, Hiroshi. "A view for the promotion of solid earth and planetary sciences and the related mineralogical research subjets." Journal of the Mineralogical Society of Japan 19, no. 5 (1990): 273–79. http://dx.doi.org/10.2465/gkk1952.19.273.

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42

Wessels, Richard, Geertje ter Maat, Elisabetta Del Bello, Lucia Cacciola, Fabio Corbi, Gaetano Festa, Francesca Funiciello, et al. "Transnational Access to Research Facilities: an EPOS service to promote multi‑domain Solid Earth Sciences in Europe." Annals of Geophysics 65, no. 2 (April 29, 2022): DM214. http://dx.doi.org/10.4401/ag-8768.

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Transnational access (TNA) allows cross-border, short-term and frequently free-of-charge access to world-class research facilities, to foster collaborations and exchanges of experience. Specifically, TNA aims to encourage open science and innovation and to increase the efficient and effective use of scientific infrastructure. Within EPOS, the European Plate Observing System, the Volcano Observatories and Multi-scale Laboratories communities have offered TNA to their high-quality research facilities through national and European funding. This experience has allowed the definition, design, and testing of procedures and activities needed to provide transnational access inn the EPOS context. In this paper, the EPOS community describes the main objectives for the provision of transnational access in the EPOS framework, based on previous experiences. It includes practical procedures for managing transnational access from a legal, governance, and financial perspective, and proposes logistical and technical solutions to effectively execute transnational access activities. In addition, it provides an outlook on the inclusion of new thematic communities within the TNA framework, and addresses the challenges of providing market-driven access to industry.

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43

M, Kumar. "Plasma Technology: An Ultimate Solution for Solid Waste Management." Open Access Journal of Waste Management & Xenobiotics 4, no. 2 (2021): 1–6. http://dx.doi.org/10.23880/oajwx-16000159.

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The growth of the population is related to urbanization, development, and industrialization. There found a strong correlation between population, industrialization, and waste production. The famous thermodynamics laws offer insights into the technological/marketing impact on waste production and energy conversion processes. The conventional methods such as land filling, combustion, gasification, incineration, etc. not enough to manage such a huge volume of waste. The non-segregation tendency, consumerism nature makes this waste management work problematic. The paper studies the natural efficiency in the waste management system and also the inability of traditional technology's to handle rapidly increasing waste volume. The plasma-based waste technology is similar to the natural waste management cycle, but with high volume capacity in a short duration. This also has a scope of waste to energy (WtE) conversion. Though plasma has high installation and maintenance costs, revenue generation from byproducts like syngas and slag will create it financially viable.

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44

Solomon, Sean C., Victor R. Baker, Jeremy Bloxham, Jeffrey Booth, Andrea Donnellan, Charles Elachi, Diane Evans, et al. "Plan for living on a restless planet sets NASA's solid Earth agenda." Eos, Transactions American Geophysical Union 84, no. 45 (2003): 485. http://dx.doi.org/10.1029/2003eo450001.

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45

Di Salvo, Sara, Eleonora Braschi, Martina Casalini, Sara Marchionni, Teresa Adani, Maurizio Ulivi, Andrea Orlando, et al. "High-Precision In Situ 87Sr/86Sr Analyses through Microsampling on Solid Samples: Applications to Earth and Life Sciences." Journal of Analytical Methods in Chemistry 2018 (2018): 1–20. http://dx.doi.org/10.1155/2018/1292954.

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An analytical protocol for high-precision, in situ microscale isotopic investigations is presented here, which combines the use of a high-performing mechanical microsampling device and high-precision TIMS measurements on micro-Sr samples, allowing for excellent results both in accuracy and precision. The present paper is a detailed methodological description of the whole analytical procedure from sampling to elemental purification and Sr-isotope measurements. The method offers the potential to attain isotope data at the microscale on a wide range of solid materials with the use of minimally invasive sampling. In addition, we present three significant case studies for geological and life sciences, as examples of the various applications of microscale 87Sr/86Sr isotope ratios, concerning (i) the pre-eruptive mechanisms triggering recent eruptions at Nisyros volcano (Greece), (ii) the dynamics involved with the initial magma ascent during Eyjafjallajökull volcano’s (Iceland) 2010 eruption, which are usually related to the precursory signals of the eruption, and (iii) the environmental context of a MIS 3 cave bear, Ursus spelaeus. The studied cases show the robustness of the methods, which can be also be applied in other areas, such as cultural heritage, archaeology, petrology, and forensic sciences.

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46

孟, 圆. "Research Progress of Self-Healing Solid-Solid Phase Change Materials." Hans Journal of Nanotechnology 12, no. 04 (2022): 311–29. http://dx.doi.org/10.12677/nat.2022.124032.

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47

Shiraki, Susumu, Tetsuroh Shirasawa, and Taro Hitosugi. "Study of Solid-Solid Interface in All-Solid-State Batteries: Atomic Structures and Ion Conductivities at Interfaces." Journal of Surface Analysis 27, no. 3 (2021): 156–60. http://dx.doi.org/10.1384/jsa.27.156.

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48

Chen, L., J. G. Chen, and Q. H. Xu. "Correlations between solid tides and worldwide earthquakes <i>M</i><sub>S</sub> ≥ 7.0 since 1900." Natural Hazards and Earth System Sciences 12, no. 3 (March 6, 2012): 587–90. http://dx.doi.org/10.5194/nhess-12-587-2012.

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Abstract. Most studies on the correlations between earthquakes and solid tides mainly concluded the syzygies (i.e. new or full moons) of each lunar cycle have more earthquakes than other days in the month. We show a correlation between the aftershock sequence of the ML = 6.3 Christchurch, New Zealand, earthquake and the diurnal solid tide. Ms ≥ 7 earthquakes worldwide since 1900 are more likely to occur during the 0°, 90°, 180° or 270° phases (i.e. earthquake-prone phases) of the semidiurnal solid earth tidal curve (M2). Thus, the semidiurnal solid tides triggers earthquakes. However, the long-term triggering effect of the lunar periodicity is uncertain. This proposal is helpful in defining possible origin times of aftershocks several days after a mainshock and can be used for warning of subsequent larger shocks.

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49

Fischer, Cornelius, and Andreas Luttge. "Pulsating dissolution of crystalline matter." Proceedings of the National Academy of Sciences 115, no. 5 (January 16, 2018): 897–902. http://dx.doi.org/10.1073/pnas.1711254115.

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Fluid–solid reactions result in material flux from or to the solid surface. The prediction of the flux, its variations, and changes with time are of interest to a wide array of disciplines, ranging from the material and earth sciences to pharmaceutical sciences. Reaction rate maps that are derived from sequences of topography maps illustrate the spatial distribution of reaction rates across the crystal surface. Here, we present highly spatially resolved rate maps that reveal the existence of rhythmic pulses of the material flux from the crystal surface. This observation leads to a change in our understanding of the way crystalline matter dissolves. Rhythmic fluctuations of the reactive surface site density and potentially concomitant oscillations in the fluid saturation imply spatial and temporal variability in surface reaction rates. Knowledge of such variability could aid attempts to upscale microscopic rates and predict reactive transport through changing porous media.

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50

Mitrovica, J. X., J. Austermann, S. Coulson, J. R. Creveling, M. J. Hoggard, G. T. Jarvis, and F. D. Richards. "Dynamic Topography and Ice Age Paleoclimate." Annual Review of Earth and Planetary Sciences 48, no. 1 (May 30, 2020): 585–621. http://dx.doi.org/10.1146/annurev-earth-082517-010225.

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The connection between the geological record and dynamic topography driven by mantle convective flow has been established over widely varying temporal and spatial scales. As observations of the process have increased and numerical modeling of thermochemical convection has improved, a burgeoning direction of research targeting outstanding issues in ice age paleoclimate has emerged. This review focuses on studies of the Plio-Pleistocene ice age, including investigations of the stability of ice sheets during ice age warm periods and the inception of Northern Hemisphere glaciation. However, studies that have revealed nuanced connections of dynamic topography to biodiversity, ecology, ocean chemistry, and circulation since the start of the current ice-house world are also considered. In some cases, a recognition of the importance of dynamic topography resolves enigmatic events and in others it confounds already complex, unanswered questions. All such studies highlight the role of solid Earth geophysics in paleoclimate research and undermine a common assumption, beyond the field of glacial isostatic adjustment, that the solid Earth remains a rigid, passive substrate during the evolution of the ice age climate system. ▪ Dynamic topography is the large-scale, vertical deflection of Earth's crust driven by mantle convective flow. ▪ This review highlights recent research exploring the implications of the process on key issues in ice age paleoclimate. ▪ This research includes studies of ice sheet stability and inception as well as inferences of peak sea levels during periods of relative ice age warmth. ▪ This review also includes studies on longer timescales, continental-scale ecology and biodiversity, the long-term carbon cycle, and water flux across oceanic gateways.

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